UBC Undergraduate Research

Climate change effects on eruptive forest insects : a review and synthesis of empirical evidence Marciniak, Amberly 2012

Your browser doesn't seem to have a PDF viewer, please download the PDF to view this item.

Item Metadata


52966-Marciniak_Amberly_FRST_498_Graduating_Thesis_2012.pdf [ 554kB ]
JSON: 52966-1.0075624.json
JSON-LD: 52966-1.0075624-ld.json
RDF/XML (Pretty): 52966-1.0075624-rdf.xml
RDF/JSON: 52966-1.0075624-rdf.json
Turtle: 52966-1.0075624-turtle.txt
N-Triples: 52966-1.0075624-rdf-ntriples.txt
Original Record: 52966-1.0075624-source.json
Full Text

Full Text

    CLIMATE CHANGE EFFECTS ON ERUPTIVE FOREST INSECTS: A REVIEW AND SYNTHESIS OF EMPIRICAL EVIDENCE     FRST 498 AMBERLY MARCINIAK 2  ABSTRACT Global climate change is affecting ecosystems through warming temperatures, changing precipitation, and increasing climatic variability. One of the major impacts is the alteration of forest disturbance regimes, including forest insect outbreaks that cause landscape-scale tree mortality and significantly affect the composition, function, and socioeconomic value of forests. Many studies have been conducted and models created to predict how future climate change may affect forest insects, but it may also be useful to determine how insects have already responded in order to detect where knowledge may be lacking and which species may be of most concern in future forest management. For this thesis, research papers providing empirical evidence to show a definitive climate change effect on an eruptive forest insect were identified and reviewed. The selected papers were then synthesized into a predictive framework for the likely responses of specific forest insect groups or species to changes in temperature or precipitation. Bark beetles and defoliators were the two functional groups for which evidence was found. All evidence pointed to bark beetle species responding positively to warming temperatures and decreasing precipitation through range expansion and increases in outbreak extent and severity. Evidence was less straightforward for defoliators, as some species, but not all, showed a negative response to warmer temperatures due to increasing asynchrony between insect emergence and host tree budburst on which they depend for food and survival. KEYWORDS Bark beetles, climate change, defoliators, forest insect disturbance, forest management   3  CONTENTS ABSTRACT………………………………………………………………………………………………………………………………….2 KEYWORDS………………………………………………………………………………………………………………………………..2 INDEX OF TABLES……………………………………………………………………………………………………………………....4 INDEX OF FIGURES……………………………………………………………………………………………………………………..4 INTRODUCTION………………………………………………………………………………………………………………………….5  OBJECTIVES…………………………………………………………………………………………………………………….7 METHODS………………………………………………………………………………………………………………………………….8 RESULTS AND DISCUSSION…………………………………………………………………………………………………………9  BARK BEETLES………………………………………………………………………………………………………………13  DEFOLIATORS……………………………………………………………………………………………………………….17  PREDICTIVE FRAMEWORK…………………………………………………………………………………………….22  IMPLICATIONS FOR FOREST MANAGEMENT…………………………………………………………………26 CONCLUSION……………………………………………………………………………………………………………………………28 REFERENCES…………………………………………………………………………………………………………………………….30   4  INDEX OF TABLES Table 1: Summary of studies that give empirical evidence for climate change effects on eruptive forest insects ......................................................................................................................................................... 10  INDEX OF FIGURES Figure 1: Flowchart summary of probably forest insect responses to climate change given the results in Table 1. The + and – symbols refer to positive and negative response to climate change effects respectively. ................................................................................................................................................ 22  5  INTRODUCTION Over the past century and a half, the world has experienced climate change through a significant warming trend and an increase in climatic variability (IPCC 2007, Peterson and Baringer 2009). Record high temperatures have been occurring since the 1970s (IPCC 2007), especially at the higher latitudes in the northern hemisphere, such as the Arctic and boreal regions (IPCC 2007, Soja et al. 2007). Climate change has also been connected to rising seas levels (Church and White 2006, IPCC 2007), rapidly melting glaciers and ice caps (IPCC 2007, Kwok and Rothrock 2009), and more frequent extreme weather events (IPCC 2007). There has been an increase in heavy precipitation events, the frequency of heat waves and hot days and nights, and intense tropical cyclone activity in some regions. It is expected that in the 21 st  century there will be an increase in the mean annual global temperature of between 1.8°C to 4.0°C (IPCC 2007). Temperatures and temperature and precipitation extremes will continue to rise in the future, especially in Northern Eurasia, Alaska, and Canada (Soja et al. 2007, Safranyik et al. 2010). Summer warming in Northern Eurasia is predicted to be greater by almost half of the global mean, and boreal regions of Europe and Canada will also experience summer warming estimated to exceed the global mean (Soja et al. 2007). Most evidence points to human-induced reasons for climate change, as human activities have caused increased emissions of greenhouse gases into the atmosphere from factory waste, vehicles, deforestation, agriculture and other sources, and concentrations of these greenhouse gases have significantly increased globally since the late 1700s (Hegerl et al.1996, Santer et al. 1996, Santer et al. 2003, IPCC 2007). Climate change is a concern for forest management because shifts in temperature, precipitation, and atmospheric greenhouse gas concentrations are likely to have significant effects on trees and forest ecosystems (Bentz et al. 2010). By the end of the century, climate profiles that are completely different from current coniferous vegetation are predicted to affect much of the landscape. Furthermore, natural forest disturbances are predicted to be greatly impacted by climate change. Natural forest disturbances include pathogens, such as fungal root rot, rusts, dwarf mistletoe, and white pine blister (Ayres and Lombardero 2000); insect disturbances, like spruce budworm (Choristoneura fumiferana [Clemens]) and spruce beetle (Dendroctonus rufipennis Kirby) infestations that have had great impacts in boreal forests; overabundances of browsing herbivores, such as deer, moose, elk, and hares; and abiotic disturbances, such as fire, 6  drought, windstorms, ice storms, and landslides (Dale et al. 2001). Climate change impacts forests by creating changes in local, regional, and global temperature and precipitation that affect the occurrence, frequency, duration, extent, and intensity of disturbances (IPCC 2007, Dale et al.2001). In other words, forest disturbance regimes may be completely altered. For example, there have been recent increases in fires, droughts, insect and pathogen outbreaks, introduced species, and extreme weather events, all of which can be linked to climate change (IPCC 2007, Dale et al. 2001, Wotton et al. 2010, Soja et al. 2007). The effects of these changes often have great impacts on forest ecosystems, and even alter them in unexpected and often undesirable ways (Dale et al. 2001). The social and economic effects that arise from these changes make it crucial to carefully manage forests with future climate change impacts in mind (Ayres and Lombardero 2000, Dale et al. 2001), especially as losses of valuable forests to large-scale disturbances can equal millions of dollars lost (Dale et al. 2001). The most costly of forest disturbances are insects and pathogens, to which over $2 billion and 20.4 million hectares of trees are lost in the U.S. every year (Dale et al. 2001). Insect herbivores, those that eat plant tissues, are a natural and important part of forests, but can significantly affect forest composition, ecosystem function, and socioeconomic value in ways that humans consider negative (Ayres and Lombardero 2000). Every major forest type has experienced strong impacts by insect disturbances; for example, bark beetles in the family Curculionidae (sub family: Scolytinae) have created some of the largest natural disturbances in pine forests (Ayres and Lombardero 2000). Loss of trees to forest insect disturbances not only creates economic losses, but also can result in negative impacts on other animal, plant, or insect species that live in forests (Ayres and Lombardero 2000, Conner et al. 1998), such as by removing important habitat like mature trees that cavity nesting birds rely on, or fragmenting forest stands by killing large groups of trees, thereby reducing the ability of certain animal populations to disperse (Ayres and Lombardero 2000). Landscape-scale tree mortality from insect herbivores also releases large amounts of carbon to the atmosphere, which can exacerbate climate change (Kurz et al. 2008). Climate change appears to have been strongly and directly affecting insect herbivores, and warming conditions will likely increase insect outbreaks in the future (Ayres and Lombardero 2000, Soja et al. 2007, Bentz et al. 2010). The rate of development and reproductive potential of many insects will likely be increased by summer temperatures in temperate and boreal forests 7  (Ayres and Lombardero 2000, Soja et al. 2007), while warmer winter temperatures may reduce winter mortality of insects that are susceptible to cold weather, such as the southern pine beetle that experiences nearly 100% mortality when air temperatures fall below -16°C (Ayres and Lombardero 2000). Climate change may also indirectly affect insect herbivores; for example, excessive heat or drought create stress on trees and lower their defences, making them less resistant to insect attacks (Ayres 1993, Croise and Lieutier 1993). It has only been recently, however, that a connection has been established between insect infestations and changes in temperature in regions such as Alaska, where correlations have been shown between insect outbreaks, tree ring evidence and recorded air temperature (Soja et al.2007). While experts generally agree that there has been increased forest mortality as a result of insect outbreaks responding to climate change, there is still a lack in complete documentation for some insect disturbance responses to warming temperatures (Soja et al.2007). This makes it more difficult to predict how insects will respond with further climate change in the future, which is essential for effective management of forests that will inevitably face such disturbances. OBJECTIVE Many models have been created to attempt to project how insect herbivores might respond to future climate change (e.g., Robinet et al. 2007, Jonsson et al. 2009, Safranyik et al. 2010). A combination of climate models and quantitative models based on a mechanistic understanding of biological responses to temperature can give results to provide insight into ecosystem responses to climate change (Bentz et al. 2010, Seidl et al. 2011). While models may be useful for creating predictions that can be utilized by forest managers to help mitigate future disturbances, many uncertainties arise when using them, including uncertainties associated with climate model data choices (Jonsson et al. 2009, IPCC 2007), and the ability of the model to make good predictions more than a year or two in advance. For example, a model that was created to predict mountain pine beetle (Dendroctonus ponderosae Hopkins) outbreaks, when tested against past outbreaks, showed an 80% predictive capacity for one year, but its capacity to make a 2-year and 3-year forecast was reduced to 69% and 30% respectively (Aukema et al. 2008). It may be beneficial, therefore, to use current evidence of insect herbivore responses to establish a real and practical indication of how warming temperatures and changing climatic variability have affected insect disturbances. If patterns are found in their recent responses, then perhaps they may be applied to predictions of future insect disturbances. 8  The objective of this paper is to conduct a literature review that presents empirical evidence in scientific literature of climate change impacts on forest disturbances caused by outbreaking insect herbivores, as well as to synthesize the evidence into a possible framework for predicting the general trend of disturbances by certain insect groups or species in the future. METHODS To create a predictive framework, peer-reviewed scientific papers were selected based on their claimed strength of empirical evidence for climate change impacts on forest insect populations. A general search was conducted first for papers that were focused on potentially eruptive insect species found in forest ecosystems and reliant on trees for food and reproduction, such as bark beetles, that have displayed some relatively recent change in life history characteristics, range, or outbreak dynamics. The search was constrained to select for evidence of definite change in approximately the last century, and to exclude studies that focused on making predictions for the future state, such as through the use of models. Next, the results were narrowed further by selecting for only those that linked the change in a forest insect to some impact of climate change. Studies providing evidence that an insect species population had responded positively or negatively to climate change effects, such as increased temperatures or variations in precipitation, were chosen as good candidate papers for the final selection. For a paper to be selected for the synthesis, it had to be accepted as definitively showing a climate change effect on an eruptive forest insect, which it only did if it met the following criteria: (1) empirical evidence was provided for a change in the insect outbreak frequency, intensity and/or range; (2) there was explicit evidence given that an effect of climate change had occurred at the same time, such as measurable increases or decreases in temperature, precipitation, or extreme weather events; (3) a strong link was made between the climate change effect and the response of the insect. Papers were excluded if they showed evidence for the response of a forest insect to a certain climatic variable, such as temperature or precipitation, but did not state or provide adequate support for the connection to recent climate change altering both the climatic variable and the insect response in a certain region. Data on the forest insect species that responded to climate change impacts were extracted from the final selection of papers, including which functional group the species belonged to (e.g., bark 9  beetles), the host tree species and geographic location of the species in each study, the study methods used, the climate change effects on insect herbivory response (i.e., positive or negative), the mechanism of the effects, and how the responses were linked to climate change. To synthesize the data into a useful predictive framework, reoccurring patterns were looked for in the data. Within each functional group of insects, similarities in herbivory responses to climate change effects were noted; for example, the species that responded positively and the ones that showed a negative response were identified. The mechanisms of the climate change effects on the responses, such as range expansion or altered outbreak dynamics, were also compared, along with the specific effects that the responses were linked to (e.g., warmer winters and/or summers, or reduced precipitation). Different functional groups were then compared and contrasted for the climate change effects on the responses of forest insect species. Based on the analysis of similarities and differences in the responses within and between insect functional groups, a possible framework was created to attempt to predict how similar insect species within each group may respond to climate change in the future. RESULTS AND DISCUSSION In total, twelve papers were found to provide adequate evidence for climate change impacts on six outbreak forest insect species (Table 1). All studies linked changes in temperature and/or precipitation to positive or negative changes in the species’ range expansion or frequency and intensity of outbreaks. Only two major functional groups of insects were addressed in the studies – bark beetles and defoliators. Bark beetles were found to respond positively to warmer summers and winters, increased average temperatures, and/or decreased precipitation. One species, the mountain pine beetle, expanded its range as a result of warming temperatures outside the limits of its range that allowed it to successfully attack hosts and reproduce in regions that were historically unsuitable for it. Another bark beetle, the spruce beetle, erupted in areas that previously had no records of outbreaks, as well as increased spatio-temporal synchrony of outbreaks. This was mainly due to increased temperatures and shorter extreme cold periods causing changes in the population dynamics. On the other hand, while defoliators were shown to generally respond positively for similar reasons as bark beetles, some studies produced conflicting results that indicated that the effects of climate change may have partially or wholly negative impacts on certain defoliators, such as the winter moth (Operophtera brumata Bkh.) 10  Table 1: Summary of studies that give empirical evidence for climate change effects on eruptive forest insects Insect characteristics  Study Insect functional group Insect species Host species Location Methods Climate change effects on herbivory Mechanism of the effect Link to climate change Reference Bark Beetles Mountain pine beetle Pines; primarily lodgepole pine British Columbia Climatic suitability model Positive  Range expansion:  increased climatic suitability  Warmer winters and summers Carroll et al. (2004)   Whitebark pine Idaho, USA Process-based model Positive  Altitudinal range expansion:  increased climatic suitability  Warmer average temperature than historically Logan and Powell (2001)  Spruce beetle Spruce  Alaska  Yukon Field measurements (dendrochronology), simulation modelling Positive Outbreaks in new areas of range:  altered population dynamics  increased rates of reproduction  Warmer summers (for 5- 6 year periods)  Shorter and fewer extreme cold periods in winter Berg et al. (2006)   Spruce Alaska Field measurements (dendrochronology) Positive  Increased spatio- temporal synchrony of outbreaks:  altered population dynamics  earlier emergence and dispersal  Decreased winter precipitation  Warmer winter and summer temperatures Sherriff et al. (2011) Defoliators Winter moth Birch Norway Quantile regression modelling; spatial mapping Positive  Expansion of core outbreak area:  increased climatic suitability  Warmer mean annual and minimum winter temperatures Jepsen et al. (2008) 11  Insect characteristics  Study Insect functional group Insect species Host species Location Methods Climate change effects on herbivory Mechanism of the effect Link to climate change Reference   Oak Netherlands Modelling of egg hatch timing; field measurements of oak budburst Negative  Asynchrony of larvae emergence and host budburst:  disrupted relationship  maladaptive behaviour  Increased mean daily warmth with no change in number of frost days from 1 Dec – 1 Mar Visser and Holleman (2001)  Pine processionary moth Pine Spain Field measurements Positive  Increased defoliation:  increased larval survival in winter  Warmer winter temperatures Hodar and Zamora (2004)   Pine (Pinus sylvestris and Pinus nigra)  France  Italy Field measurements Positive  Range expansion:  increased climatic suitability  Warmer average winter temperatures Battisti et al. (2005)   Pine (Pinus nigra) Italy Field measurements, lab experiment Positive  Altitudinal range expansion:  increased climatic suitability  Warmer average winter temperatures, temperature variability Hoch et al. (2009)  Larch budmoth Subalpine larch Switzerland Field measurements (dendrochronology) Negative  Outbreak absence:  altered population dynamics  increased egg and larval mortality  asynchrony of emergence with host budburst  Extreme regional warmth outside of historical climatic envelope  Warmer winters Esper et al. (2007) 12  Insect characteristics  Study Insect functional group Insect species Host species Location Methods Climate change effects on herbivory Mechanism of the effect Link to climate change Reference   Subalpine larch Switzerland Lab experiment Negative  Outbreak absence:  altered population dynamics  increased egg and larval mortality  asynchrony of emergence with host budburst  Warmer spring temperatures than average for 3 consecutive years Baltensweiler (1993)  Birch budmoth Birch (Betula pubescens L.) Norway Calculations of monthly air temperature averages, statistical analysis: ANOVA, Tukey’s HSD Positive  New outbreak:  altered population dynamics  increased larval survival  Warmer winter temperatures and shorter extreme cold periods Tenow et al. (1999)  13  and larch budmoth (Zeiraphera diniana Gn.). It was shown that asynchrony between larvae emergence and host budburst may be occurring because of the insect and trees responding differently to warmer winter and spring temperatures, which leads the larvae that depend on new foliage for food to starve or attempt to disperse in search of a new host. These findings and the strengths and weaknesses of the evidence that each study provided is discussed in the following review of the literature, after which is an attempt to synthesize the results into a framework for predicting forest insect response to climate change. BARK BEETLES The range and outbreak area of the mountain pine beetle has expanded from central BC in the 1990’s to more northern and eastern localities and higher elevations post-2000, including into regions of the province of Alberta (Bentz et al. 2010, Safranyik et al. 2010). Several observations and models in the past have attempted to predict the large-scale outbreaks of mountain pine beetle in naïve areas in relation to climate change effects (e.g., Aukema et al. 2008, Bentz et al. 2010, Safranyik et al. 2010); however, Logan and Powell (2001) and Carroll et al. (2004) were the first studies to provide direct evidence for the changes that have occurred due to climate change. They demonstrated that the mountain pine beetle has been able to move into and maintain self-sustaining populations at higher latitudes and elevations that previously did not have the right climatic conditions for it to survive or successfully outbreak. Carroll et al. (2004) used a model of climatic suitability that incorporated the direct and indirect effects of temperature and precipitation on habitat suitability to mountain pine beetle. They used that model, along with Environment Canada weather data, to produce maps of the distribution of the climatically suitable habitats in the past. Then they compared the distribution of infestations through time to the distribution of climatically suitable habitats in the past to show that mountain pine beetle populations had moved at an increasing rate over time into the areas that were historically unsuitable. There has been an apparent shift in climatically suitable habitats over the past three decades, which beetle populations have followed: prior to 1968, there were no infestations in areas with historically very low to low climatic suitability, but the increasing number of infestations at an increasing rate in those higher latitude/elevation areas points to a sufficient change in the climatic conditions that has allowed mountain pine beetles to now establish and persist. Similarly, Logan and Powell (2001) showed that the beetle has been able to 14  persist in pine stands at higher elevations than it could historically due to a change in climatic suitability. A process-based model was used to demonstrate that a previous outbreak during the 1930’s in high elevation whitebark pines in the White Cloud Mountains of central Idaho was caused by beetles that were able to maintain a self-sustaining population as a result of the higher than normal temperatures. The evidence presented by Carroll et al. (2004) and Logan and Powell (2001) for mountain pine beetle range expansion in response to climate change is strongly supported by the facts that only climate could have limited the boundaries of their range in the past (Carroll et al. 2004, Safranyik and Carroll 2006, Safranyik et al. 2010), and temperature has the biggest effect on the ability of mountain pine beetles to successfully establish, persist, and reach outbreaking populations (Safranyik and Carroll 2006, Raffa et al 2008, Bentz et al. 2010). Lodgepole pine, ponderosa pine, and western white pine, the beetle’s preferred hosts (Safranyik and Carroll 2006), grow throughout BC, and therefore could not have contributed to restricting the mountain pine beetle range within central BC in the early 1900s. Furthermore, the mountain pine beetle has been shown to successfully attack and reproduce in other species of pine, including whitebark pine that grows at high elevations in BC (Logan and Powell 2001), and jack pine, a species that is abundant in Alberta and other provinces outside BC (Safranyik et al. 2010). Thus, the beetle has plenty of acceptable hosts not only in BC, but throughout the country, and yet its occurrence had never been recorded in those areas at higher latitudes and elevations or east of the Rocky Mountains until the habitats warmed due to climate change in the recent time period (Logan and Powell 2001, Carroll et al. 2004, Safranyik et al. 2010). In terms of climatic suitability of an environment, temperature plays a crucial role in the survival of the mountain pine beetle (Safranyik and Carroll 2006, Raffa et al. 2008). The overwintering larvae may not survive extremely cold temperatures, and the lethal temperature of -40°C will cause 100% mortality (Safranyik and Carroll 2006). Regions at higher latitudes and altitudes in BC were often free of beetle infestation because the lethal temperature was frequently met in winter, but climate change has led to warmer winters in which the beetle is better able to survive and emerge synchronously the following spring (Logan and Powell 2001, Carroll et al. 2004, Aukema et al. 2008). Increased temperatures also increase the developmental time of the mountain pine beetle so that it may complete its lifecycle in one year rather than two (Logan and 15  Powell 2001). Logan and Powell (2001) demonstrated that a semivoltine population can shift into a synchronous univoltine population with only about a 2°C increase in the average annual temperature. This shift allows the population to increase in size at a faster rate and attack larger, healthier trees with better success (Logan and Powell 2001, Safranyik and Carroll 2006), both of which allow for exceeding the threshold from endemic to epidemic, self-amplifying populations (Raffa et al. 2008, Boone et al. 2011). Finally, temperature indirectly influences the success of attacks on the host by affecting the resistance of trees (Raffa et al. 2008, Bentz et al. 2010). Trees under attack by bark beetles will generally defend with a combination of constitutive and inducible resins; however, high temperatures (as well as drought conditions) can stress and weaken trees to the point where they lack the resources to produce resin defences. Warmer temperatures may also aid blue-stain fungus carried by the mountain pine beetle in germinating and growing more quickly within the tree, where it desiccates the phloem and xylem, disrupting transpiration and bringing resin production by the tree to a halt (Safranyik and Carroll 2006). Climate change has led to warmer summer and winter temperatures at higher latitudes and elevations, directly aiding the survival of mountain pine beetle and indirectly increasing its ability to attack its hosts in previously uninfested habitats, and has resulted in the range expansion of the beetle. The spruce beetle is the second bark beetle species which has evidence for responding to climate change. Berg et al. (2006) demonstrated that, because of increasing climatic suitability, new outbreaks have occurred in areas that previously did not experience them. Historically, periodic outbreak occurred in maritime regions of Alaska when forests matured and disturbances such as windthrow or fire favoured beetle reproduction (Berg et al. 2006); however, more recent outbreaks have occurred in interior regions where they were previously rare, without any clearly identifiable disturbance, and possibly outside the normal historical range of outbreak sizes. Berg et al. (2006) found that there were large, outbreaks of spruce beetle in the 1990s within Kluane National Park, Yukon, an interior region without previous records of outbreaks, that were likely initiated and sustained by 5-6 year periods of abnormally warm summer temperatures. Recent winters in the interior, although not significantly warmer, have also experienced shorter and fewer periods of extreme cold which has increased the survivability of the overwintering larvae. Sherriff et al. (2011) provided further evidence for an increase in spatio-temporal synchrony of outbreaks within the historic geographic range in Alaska due to warmer winters and summers, 16  and a decrease in winter precipitation, which has led to stressed trees that cannot defend well against attacks. It is suggested that outbreaks are increasingly having similar timings across not only Alaska, but in the Southern Rocky Mountains and Central BC as well, likely as a result of climate change creating similar patterns of synchrony in environmental variables such as temperature across many regions (Sherriff et al. 2011). The results shown in the two studies can be explained in part by the way in which the life histories of the spruce beetle are tightly controlled by summer temperatures (Berg et al. 2006, Raffa et al. 2008, Sherriff et al.  2011). Warmer summer temperatures brought on by climate change increases the rate at which the beetle develops, allowing for earlier adult emergence, dispersal, attack, and breeding (Werner and Holsten 1985, Berg et al. 2006, Sherriff et al. 2011). This results in eggs being laid earlier and provides larvae with a longer growing season. Warmer air temperatures also increase the temperature of the tree phloem, which can lead larvae to develop in only one year instead of two, changing it to a univoltine life-cycle that promotes larger population sizes and outbreaks. Finally, larval development and subsequent adult emergence may be synchronized by higher temperatures, which allows for more successful mass attacks on trees. Historically, spruce beetles were limited to outbreaking in maritime regions because of the climate, but as the interior climate has warmed, summer and winter temperatures have risen, and the beetle has been able to successfully erupt in areas previously too cool (Berg et al. 2006, Sherriff et al. 2011). The four papers that link climate change to increases in bark beetle range expansion and outbreaks correspond with other studies that have looked at the effect of temperature and other climatic variables on bark beetles. The methods also use empirical evidence to support their results, strengthening their conclusions. Carroll et al. (2004) and Logan and Powell (2001) took actual records of historical mountain pine beetle range and analyzed it with climate data records. Berg et al. (2006) and Sherriff et al. (2011) used dendrochronology techniques to determine spruce beetle outbreak occurrences and annual climate reconstruction records. They took spruce cores and analyzed the tree rings for growth releases that indicated spruce beetle outbreaks had occurred. This technique has been used in the past to analyze spruce beetle outbreaks (Veblen et al. 1991), and it is useful as a detection tool because aside from occasional fires, the only other large-scale disturbance in the northern region where the studies occurred is tree mortality by 17  spruce beetle outbreaks (Berg et al. 2006, Sherriff et al. 2011); therefore, identification of years where outbreaks created gaps and allowed neighbouring trees to be released should be fairly accurate. It should be noted, however, that the bark beetle studies were all located in North America, a continent that has been colonized for a much shorter time period than Europe, and historical records for climate data and forest insect disturbances only go back for a relatively short period compared to those that can be found in Europe (Quinlan et al. 1987, Mbogga et al. 2009). It is therefore more difficult to differentiate normal variability in insect disturbances in relation to climate. Dendrochronology has allowed these studies to examine disturbance regimes in the last 200 to 400 years, yet the lack of first-hand records during those years makes the interpretation of apparent disturbances somewhat less confident. DEFOLIATORS Evidence for climate change effects on forest insect disturbances was provided for four defoliating forest insect species, compared to only two bark beetles (Table 1); however, there was less consensus between the studies on how defoliating species were responding to a warming climate. The species that was most strongly linked to a positive response with climate change was the pine processionary moth (Thaumetopoea pityocampa [Denis & Schiffermuller]). Three studies provided evidence that the pine processionary moth has expanded its outbreak area range in latitude and/or elevation due to warmer than average winter temperatures in southern Europe (Hoch et al. 2009, Battisti et al. 2005, Hodar and Zamora 2004). This species has minimum winter threshold temperatures that must be met in order for the larvae to feed (Battisti et al. 2005), which has historically limited its range to warmer, more southern regions where winter temperatures rise above the threshold often enough for the moth to successfully develop and complete its lifecycle. Winter temperatures have been increasing outside of the moth’s previous range, such as at more northerly latitudes and higher altitudes around central France and northern Italy (Hodar and Zamora 2004, Battisti et al. 2005, Robinet et al. 2007, Hoch et al. 2009), which has allowed the insect to expand further into those regions. Hodar and Zamora (2004) directly linked climate experienced by the pine processionary moth and the defoliation incidence in the following winter, showing an increased intensity of defoliation as the temperature in the previous winter increased. Battisti et al. (2005) provided substantial evidence that the pine processionary moth range has shifted in latitude in central France and in elevation in northern Italy, and that the expansion has accelerated in the past 10 years in response to warmer 18  temperatures at the limits of their range. Hoch et al. (2009) supported this with further results showing a range expansion in elevation in Italy. Even at the very limits of its range, the moth is able to cope with highly variable temperatures because of its moderate freeze tolerance (Hoch et al. 2009), the ability of the pupae to remain in the soil for up to 7 years (Battisti et al. 2005), and its tolerance for long periods of starvation in the larval stage. The moth is able to rapidly move into regions near the boundaries of its range that have begun to warm, even if there are still periods of variable, cold weather. The combination of warmer winters and the widespread, often homogeneous structured ranges of its host trees make it likely that this species will continue to move further north in Europe and into higher elevations. Contradictory to the pine processionary moth, the response of larch budmoth, another defoliating species, to climate change was negative according to two studies (Table 1). Analysis of tree ring density profiles using dendrochronology techniques revealed that the larch budmoth in the subalpine larch forests of the European Alps has maintained highly regular outbreaks that have recurred every 8 to 9 years for over a millennium (Weber 1997, Esper et al. 2007). The extensive periodicity provides strong evidence for the predictability of outbreaks, and therefore the absence of any significant outbreaks since the 1980s, an unprecedented length in regards to the last 1173 years (Esper et al. 2007), indicates that the population dynamics of the larch budmoth has been disrupted. Esper et al. (2007) linked the absence of outbreaks since the late 20 th  Century to the period of extreme regional warmth outside of the climatic envelope of the past 1200 years, suggesting that a temperature variation threshold has recently been passed. Baltensweiler (1993), who examined the reasons for the collapse of the 1990 outbreak, agreed that consecutively warmer winters and springs affected the ability of the moth to outbreak. Both studies suggested that the increased winter and spring temperatures affected the overwintering eggs by inducing early development and egg hatch, leading to increased mortality of eggs when colder weather hit again or increased 1 st  instar larvae starvation and mortality when they hatched before budburst in their host. Hatching in synchrony with the host’s budburst and new flush of the leaves is crucial for the survival of the vast majority of Lepidopteran defoliating insects (Feeny 1970, Bale et al. 2002). The 1 st  instar larvae generally require the very soft leaves that first emerge from buds to be able to tear into them with their tiny mandibles (Feeny 1970). Furthermore, leaves very quickly lose 19  much of their nutritional quality as they age (Feeny 1970, Schultz et al. 1982), so that larvae that can eat older foliage will develop more slowly, gain less mass, and have a higher chance of dying from lack of necessary amounts of nutrients (Feeny 1970, Schweitzer 1979, Larsson and Ohmart 1988, Dongen 1997, Bylund 1999). There is only a very small window after budburst before foliage becomes less edible and nutrient-poor (Feeny 1970), and therefore the species that rely on it must hatch before that opportunity is lost. It is also important that the larvae do not emerge much earlier than budburst, otherwise they will have nothing to feed on and are likely to starve before the new leaves come out (Visser and Holleman 2001). Climate change, however, may be disrupting the synchrony by speeding up the development rate of eggs so that they have an increased probability of hatching before budburst (Bale et al. 2002, Visser and Holleman 2001). This is due to the insect responding more quickly than the trees to increased temperatures as a cue for development (Bylund 1999). Early egg hatch will result in increasing mortality rates and outbreak collapses among various species (Bylund 1999, Visser and Holleman 2001). Asynchrony due to climate change is likely a significant factor in the absence of outbreaks by the larch budmoth, as the species must hatch simultaneously with the flushing of the larch in the spring or otherwise experience high rates of mortality (Baltensweiler 1993). The pine processionary moth, however, is one of the exceptions to the need for synchrony. Rather than overwintering as eggs and hatching with the new spring flush, pine processionary moth larvae emerge in the late summer or early fall and remain active throughout the winter (Battisti et al. 2005, Aimi et al. 2008). They live gregariously in silk nests and feed whenever the temperature thresholds are met. By the time spring comes around, the larvae will have finished feeding and entered the soil to pupate, so that they are not dependent on new foliage for their development. This difference between the pine processionary moth and defoliators like the larch budmoth is likely an important factor in the difference between their responses to climate change, since a mistiming between egg hatching and budburst is not an issue for species that actively feed in the winter (Bale et al. 2002). The winter moth is another example of a defoliating species that requires synchrony of egg hatching and budburst (Feeny 1970, Watt and McFarlane 1991, Dongen et al. 1997, Visser and Holleman 2001). The evidence for the response of this moth to climate change was less clear-cut than the other species, as one study provided results for a positive response, while the other 20  suggested that it is more likely to be negative (Table 1). Jepsen et al. (2008) demonstrated a strong northward and eastward core outbreak area expansion of the winter moth in Norway by comparing historical outbreak records dating back to 1862 and the recent change in the boundaries of the moth’s range to the warming that has occurred at its range’s limits. The winter moth was historically restricted in its range by cold winter temperatures because it suffers substantial egg mortality at temperatures below -35°C, but the recent increase in mean annual and minimum winter temperatures has allowed the moth to expand its core outbreak area further north and east. It is clear from this study that there has been an expansion of range by the winter moth over the last few decades and that this expansion is linked to climate change because the moth, which is polyphagous mainly on birch and oak, has not been limited by its host range (Bylund 1999, Jepsen et al. 2008, Visser and Holleman 2001); however, what Jepsen et al. (2008) failed to take into account was that the fitness of the caterpillar is reliant on emerging from the egg in synchrony with budburst, and that warming temperatures within the historic range of the moth may be negatively affecting that synchrony (Bylund 1999, Visser and Holleman 2001). Visser and Holleman (2001) used measurements of oak budburst and egg hatch timing within the moth’s historic range in the Netherlands to show that climate change is likely having a negative effect on winter moth herbivory. Like the larch budmoth, the winter moth has strongly selected for close synchrony between hatching and budburst because of the risk of starvation if it hatches too early, or having to settle for less digestible leaves and a longer larval period that would increase its exposure to predators and parasites if it hatches too late (Feeny 1970, Bylund 1999, Visser and Holleman 2001). Because bud burst has no direct effect on hatching, the eggs must use an environmental cue to time hatching synchrony with budburst, and most likely uses temperature as its cue (Visser and Holleman 2001). According to Visser and Holleman (2001), the timing difference between the date of egg hatching and the date of bud burst has become more and more negative over the past 25 years. As a result, there has been an increase in mistiming of egg hatching recently, which leads to both higher mortality and dispersal of small larvae, likely causing severe effects on population dynamics (Bylund 1999, Visser and Holleman 2001). The study was able to link the mistiming to climate change by correlating the increasing ratio of warmer winter and early spring temperatures to the number of frost days with the stronger negative egg hatch timing difference. The conclusion was that extreme temperature 21  patterns brought on by climate change is likely increasing the asynchrony of winter moth hatching and oak bud burst, and therefore we should expect to see fewer outbreaks and less defoliation overall by this species as the temperatures continue to warm. Visser and Holleman (2001)’s and Jepsen et al. (2008)’s studies taken together indicate that it may be less clear how the winter moth may respond in the future with climate change, except that it may continue to expand its range at the northeast limits while possibly retracting its historical range where asynchrony between egg hatching and budburst is experienced. Birch budmoth (Argyresthia retinella Zell.) may also be outbreaking more frequently, according to one study by Tenow et al. (1999). The outbreak that that was studied started in the late 1980s in birch forests in Norway and went into the mid-1990s before crashing. Although it is unlikely that birch budmoth attacks are a new phenomenon in the region (Tenow 1996), the only other birch budmoth outbreak in recorded history that the area likely experienced was in the 1940s, and Tenow et al. (1999) claimed that both outbreaks took place during much higher than average temperatures. According to the authors, it is likely that increased temperatures may promote outbreaks for this species, especially since the restriction of its outbreak area to maritime climate indicates that the population is limited by cold temperatures at the boundaries (Tenow et al. 1999), similar to the other defoliator species mentioned previously. Tenow et al. (1999) suggested that increased winter temperatures caused by climate change may increase the survival of overwintering eggs and could be a releasing factor of outbreaks, initially making outbreaks more frequent and severe and possibly shifting area. Unfortunately, this study only examined a single recent outbreak period and only had one other unconfirmed historical outbreak to compare it to, which reduces the confidence with which the 1990s outbreak can be attributed to climate change effects. Furthermore, it was not clear whether the birch budmoth in Norway, which displays similar characteristics to the winter moth, such as similar egg diapause and cold hardiness (Elverum et al. 2003), may be affected by budburst timing. Elverum et al. (2003) reported larvae appearing in birch buds 9 days before the leaves began to unfold, so synchrony may or may not be as important for this species as with other defoliators. How the fitness of the larvae will be affected by positive or negative differences between hatching and budburst as temperatures continue to increase is not yet known.  22   PREDICTIVE FRAMEWORK The evidence in Table 1 suggests the following framework (Figure 1) for predicting the responses of bark beetles and insect defoliators to climate change:  Figure 1: Flowchart summary of probably forest insect responses to climate change given the results in Table 1. The + and – symbols refer to positive and negative response to climate change effects respectively. The four studies that examined bark beetles provided strong evidence for positive responses to climate change (Table 1), and it is likely that other bark beetles with similar biology and current climate restrictions in their range will respond positively as well (Figure 1). Various other bark beetle species have been observed to increase in frequency and intensity of outbreaks during periods of exceptionally warm and dry weather, especially other Dendroctonus species, such as the southern pine beetle (Dendroctonus frontalis) (Gan 2004) and Douglas-fir beetle (Dendroctonus pseudotsugae) (Schmitz and Gibson 1996). Landscape-scale mortality by these types of insects is expected in Canada and the United States if they respond the same way to climate change as the mountain pine beetle and spruce beetle have (Bentz et al. 2010). Ips species, such as Ips confusus and Ips typographus, have also been known to have severe outbreaks during higher temperatures or drought-like conditions, even though under normal conditions they are generally not as destructive or aggressive as the Dendroctonus species (Wermelinger 2004, Breshears et al. 2005, Jonsson et al. 2009, Santos and Whitham 2010). Ips species are generally considered to be secondary bark beetles because they normally do not seek out or kill live, healthy trees, but infest those that are stressed, weakened, damaged or downed 23  (Bentz et al. 2010, Santos and Whitham 2010).  While secondary bark beetles are not generally a concern as forest pests, they do have the ability to outbreak and cause high amounts of tree mortality under certain climatic conditions (Wermelinger 2004, Jonsson et al. 2009, Santos and Whitham 2010). Two examples of Ips species that have become major pests with outbreaks that may be linked to climate change are pinyon ips (Ips confusus) and the European spruce bark beetle (I. typographus [L.]) (Wermelinger 2004, Jonsson et al. 2009, Santos and Whitham 2010). I. confusus is a major bark beetle in southwestern U.S.A, and in 1996 a large-scale infestation occurred that caused an estimated 70% mortality of local stands of pinyon pine trees (Santos and Whitham 2010). This outbreak was associated with a major drought event that happened at the same time. A second drought occurred in 2002, the most severe on record, and instigated another devastating pinyon ips outbreak. The droughts likely increased the stress on trees and weakened them against bark beetle attack, thereby allowing pinyon ips to infest more quickly and efficiently than before, leading to faster increases in the populations (Bentz et al. 2010, Santos and Whitham 2010). Although, unlike mountain pine beetle and spruce beetle, pinyon ips have not yet been shown to generate enough positive feedback in their outbreaks to become self- amplifying and continue to outbreak after the drought is over (Raffa et al. 2008), climate change may increase the frequency and severity of droughts (IPCC 2007), and cause an increase in pinyon ips outbreak events. The European spruce bark beetle is another Ips species that has caused a lot of destruction in mature spruce forests in central and northern Europe (Wermelinger 2004, Jonsson et al. 2009). Spruce tree mortality caused by the periodic large-scale outbreaks has been in the millions, and the damage has increased considerably in the last 15 years (Jonsson et al. 2009). Increased storm felling events and favourable climatic conditions have been suggested as the reasons for the increased outbreaks, and it is likely that they will continue to expand their outbreak area as temperatures continue to rise. These examples indicate that the evidence presented in Table 1 for mountain pine beetle and spruce beetle responses to climate change may be applied to many potential pest bark beetles, including both primary Dendroctonus and secondary Ips species, and species ranging within either North America or Europe. There appears to be less certainty in regards to using the current evidence to predict the response of defoliators to climate change (Table 1, Figure 1); however, examining the life histories of the 24  species in question may help to make some tentative predictions (Bale et al. 2002). The pine processionary moth example suggests that species that have active overwintering stages in their life cycle will be more apt to benefit in their survival from warmer winters (Bale et al. 2002, Battisti et al. 2005, Battisti 2008), as that would reduce the periods of cold temperatures that prevent feeding (Battisti et al. 2005). This type of life history also does not depend on hatching and feeding in synchrony with budburst, and therefore will not be affected in that sense (Bale et al. 2002). Therefore, increased defoliation and range expansion into more northern latitudes and higher elevations is expected of species similar to the pine processionary moth. There are not, however, as many species that overwinter with active stages as there are those that wait until the spring to feed (Feeny 1970, Battisti et al. 2005, Battisti 2008). Two possible examples given by Battisti et al. (2005) of active winter feeding butterfly species that may expand in range are the North African Colotis evagore, which is likely to establish further in southern Spain once it is less limited by the winter temperature, and Eucheria socialis, a montane pierid that is like the pine processionary moth in that it has gregarious larvae that only feed when temperatures are above 0°C in the winter. The pine processionary moth appears to be somewhat of an exception among forest defoliators in that climate change effects will almost certainly be positive for it and it will likely continue to expand its range as long as temperatures are rising and at least one of its many hosts is available. Warmer winters may also be better for frost-sensitive species that do not actively feed in the winter by reducing mortality caused by extremely cold periods on the overwintering stage (Bale et al. 2002). Furthermore, warmer summers may speed up development of the growth phase (Bale et al. 2002, Netherer and Schopf 2010). This leads to less time spent in egg, larval and pupal stages, which are the periods that are normally most exposed to predators and parasites (Netherer and Schopf 2010). Increased temperatures can also allow many insects to fly and immigrate earlier by advancing the time of year at which the threshold temperature for flight is first met (Bale et al. 2002, Netherer and Schopf 2010). Therefore, most defoliators will likely benefit from the direct effects of climate change to some extent and period of time, but their exact responses will vary from species to species (Bale et al. 2002), and the possible negative effects on species that rely on synchrony with budburst of their host or require certain low temperatures to be reached in order to complete diapause may make their responses more difficult to predict. Climate change was shown to cause mistiming between egg hatching and 25  budburst in the winter moth, resulting in higher mortality and dispersal of the larvae, and making it much less likely for outbreaks to occur (Bylund 1999, Visser and Holleman 2001). Other species that rely on synchrony will most likely be adversely affected by increasing temperatures. Alternatively, they may experience increased synchrony at the northern and higher edges of their current range boundaries as climatic conditions become more suitable (Jepsen et al. 2008), reducing mortality of larvae and increasing the population size so that increased defoliation and range expansion could occur. It is difficult to predict, based on current evidence, whether climate change will cause the range of these species to contract due to increased asynchrony, expand if they are able to adapt and become synchronous again, or merely shift as the southern range boundary contracts and the northern expands. Another characteristic of many defoliating insects that makes responses more uncertain, and was not addressed in the studies in Table 1, is diapause. Diapause is very common among temperate species which experience reduced metabolic rates as inactive egg, pupa, larva or adult stages to increase cold hardiness (Bale et al. 2002, Netherer and Schopf 2010). It is an important process that promotes seasonal synchrony and helps to buffer the effects of varying temperatures so that some species may not be so restricted in their geographical range. Diapause is obligatory in many univoltine species and requires specific low temperature thresholds before the insect becomes active again when the growing season begins. Because completion of winter diapause requires lower temperatures than those that favour growth, warming winters may exceed the threshold at the southern range edges, creating a shift north in the distribution of a particular insect species (Bale et al. 2002). On the other hand, diapause may help to counteract the asynchrony effect of climate change. Higher temperatures have been promoting earlier larval emergence for many species, but because photoperiod, not temperature, controls diapause completion, diapause may prevent early emergence and help maintain synchrony with budburst. Some previous studies have shown this to possibly occur in the winter moth, in which higher temperatures prolong its autumn diapause so that even though development happens more quickly under warmer springs, the life cycle as a whole is not shortened (Bale et al. 2002, Buse and Good 1996). The added variable of diapause means that there will be even less consensus between species responses.  26   IMPLICATIONS FOR FOREST MANAGEMENT The current studies that provide empirical evidence for climate change effects on eruptive forest insects suggest that bark beetles are likely to be more strongly impacted than insect defoliators because of the lack of need for emerging in synchrony with budburst of their hosts and their rapid response to stress in their host trees. Bark beetles that have the potential to outbreak are very likely to show range expansion and increased frequency and intensity of outbreaks as conditions become more suitable with climate change. Future forest management research should focus strongly on determining which bark beetle species are likely to be of most concern to forestry goals and how landscape-level tree mortality might be mitigated. Further studies should also be conducted on lesser known bark beetle species that are found farther south, such as those indigenous to the southwestern U.S. and Mexico, because of their potential to move northward as temperatures increase (Gan 2004, Bentz et al. 2010). Similar to the northern species, such as the mountain pine beetle, southern beetles – for example the roundheaded pine beetle (Dendroctonus adjunctus) that colonizes pines in southern Utah and Colorado down into Guatemala – are currently limited to their range by climate and not by the availability of their hosts. This indicates that as climate becomes more suitable at the northern limits of their range, these beetles may move up into currently uninfested hosts or adapt to novel hosts; however, unlike the spruce beetle and mountain pine beetle that have been studied extensively in the north, there is as of yet very little information on the temperature-dependent physiological aspects of the southern beetles’ life histories (Bentz et al. 2010). While managers should expect increases in range expansion, and possibly new species from the south to shift up into new habitats, it is important to gather more information and evidence on other species aside from the two in Table 1, including more concrete links between climate change and bark beetle species that are secondary pests or from lesser known southern populations. Defoliators may be more negatively affected by climate change compared to bark beetles; however, the impacts and responses will likely vary more from species to species. Species that feed during the winter, do not require newly flushed foliage to survive, and are currently limited by cold temperatures at their range limits are likely to benefit from climate change by being able to expand their range. Other species, such as those that depend on close synchrony of emergence and budburst, but are also limited in their range by climate, may experience both positive and 27  negative effects from climate change, and predicting the final outcomes of their responses is not feasible without further, longer term studies. The evidence is currently lacking for making general assumptions about forest insect defoliators, and so proper management for future responses to climate change requires more studies on the different types of life histories of the species and which will be most affected by changes in temperature and precipitation. Other considerations that should be a focus in future studies are other variables that may increase the strength of insect pest responses to climate change. The rate of growth of population size may be impacted by increasing temperatures and climatic variability that could help insects escape the pressure of their natural enemies (Stireman et al. 2005). For example, an extensive data analysis conducted by Stireman et al. (2005) found that the frequency of parasitism in caterpillars declines with increasing climatic variability. Increased temperatures and drought- conditions also often lead to outbreaks of mountain pine beetle where the population size grows to the point where natural enemies have no affect on it and cannot control it (Safranyik and Carroll 2006). By escaping the pressure of natural enemies, bark beetles and defoliators may respond to climate change even more rapidly than expected (Stireman et al. 2005). Another concern is the connectivity of host trees that may encourage the spread of insect pests (Safranyik et al. 2010). In Europe, forests have been managed in a way that has created extensively homogeneous landscapes of pine, the pine processionary moth’s preferred host (Felton et al. 2010). With few non-hosts in the way, it is easy for the moth to locate suitable trees by dispersing even a short distance, even if it locates hosts randomly (Dulaurent et al. 2012). In Canada as well, homogeneous forests of lodgepole pine throughout BC have aided the mountain pine beetle in quickly locating hosts and expanding its range (Safranyik et al. 2010). Similar forests of Jack pine across the prairie provinces will also likely increase the rate at which the beetles are able to spread eastward. While current evidence as shown in Table 1 provides an idea of whether insect pests will respond positively or negatively to climate change, more information is required to extend predictions to response strength as climatic conditions change in the future. Finally, it is important to realize that this analysis of the literature is applicable only to the short term because it assumes that the forests as we know them will largely be intact and in the same place in the future. The effects of climate change on forest insect responses have been considered only in the context of the current forest structure, species composition, and range; however, 28  forest communities and tree species will be impacted by climate change, as shown by climate- based species distribution models and ecosystem-based climate envelope modeling (Hamann and Wang 2006, Aitken et al. 2008). As warming occurs, potential habitat is predicted to open up for tree species that are limited by cold temperatures at their northern range limits, while other species, such as some of BC’s most important conifer species, will lose a lot of their suitable habitat in their historical range (Hamann 2006). The robust capacity of tree species to shift range has already been demonstrated by fossil pollen records and genetic data that indicate the occurrence of past glacial and postglacial migrations (Davis and Shaw 2001, Hamrick 2004, Aitken et al. 2008). Current evidence also suggests that recent climate change is already affecting forests; for example, research by Breshears et al. (2005) showed that drought was the main cause of regional-scale vegetation die-off occurring across southwestern North American woodlands in the early 2000s, and that the warming and vegetation die-off was more extensive than a previous recorded drought in the 1950s. They suggest that future drought conditions due warming temperatures from global climate change will likely lead to severe and extensive death of woody plants in the overstory. When range shifts and die-offs of tree species are taken into account, it is impossible to predict the responses of eruptive forest insects given the current evidence of climate change effects. There are too many uncertainties regarding whether specific insect species will shift with their host species, expand or contract their range, adapt to novel host species that come into their historic range, or respond in other unexpected ways. Therefore, further research could be conducted to try to predict what will happen in the longer term with forest insects when climate change begins to render areas unsuitable for the tree species that used to grow there. CONCLUSION Climate change has been occurring for over 100 years and already there has been evidence that forest insect pests have been responding to the changes in temperature, precipitation, and climatic variability. Most of the focus has been on bark beetles and insect defoliators that have been known to outbreak in North American and European temperate and boreal regions. All selected studies showed that bark beetles have responded positively to climate change, and the majority of bark beetles that are of concern to management of forests will likely respond in similar ways. It was less simple, however, to generalize the responses of defoliators as increased 29  temperatures benefited some species, while negatively affecting others. While models can help us to predict future responses of insects, it could be useful to conduct more studies similar to those in Table 1 that focus on gathering current evidence on how climate change as affected various insect groups and species up to now. It may aid in determining the processes that are driving temperature-based responses in insects, and provide a concrete foundation upon which models could be built and predictions made. 30  REFERENCES Aimi, A., Larsson, S., Ronnas, C., Frazao, J., and Battisti, A. 2008. Growth and survival of larvae of Thaumetopoea pinivora inside and outside a local outbreak area. Agricultural and Forest Entomology 10: 225-232. Aitken, S.N., Yeaman, S., Holliday, J.A., Wang, T., and Curtis-McLane, S. 2008. Adaptation, migration or extirpation: climate change outcomes for tree populations. Evolutionary Applications 1: 95-111. Aukema, B.H., Carroll, A.L., Zheng, Y., Zhu, J., Raffa, K.F., Moore, R.D., Stahl, K., and Taylor, S.W. 2008. Movement of outbreak populations of mountain pine beetle: influences of spatiotemporal patterns and climate. Ecography 31: 348-358. Ayres, M.P. 1993. Global change, plant defense, and herbivory. In Biotic Interactions and Global Changes (Kareiva, P.M.,  J.G. Kingsolver, and R.B. Huey, eds.). Sinauer Associates, Sunderland, MA, pp. 75-94. Ayres, M.P., and Lombardero, M.J. 2000. Assessing the consequences of global change for forest disturbance from herbivores and pathogens. The Science of the Total Environment 262: 263-286. Bale, J.S., Masters, G.J., Hodkinson, I.D., Awmack, C., Bezemer, T.M., Brown, V.K., Butterfield, J., Buse, A., Coulson, J.C., Farrar, J., Good, J.G., Harrington, R., Hartley, S., Jones, T.H., Lindroth, R.L., Press, M.C., Symrnioudis, I., Watt, A.D., and Wittaker, J.B. 2002. Herbivory in global climate change research: direct effects of rising temperature on insect herbivores. Global Change Biology 8: 1-16. Baltensweiler, W. 1993. Why the larch bud-moth cycle collapsed in the subalpine larch-cembran pine forests in the year 1990 for the first time since 1850. Oecologia 94: 62-66. Battisti, A. 2008. Forest and climate change – lessons from insects. iForest 1: 1-5 [online: Feb 28, 2008] URL: http://www.sisef.it/iforest/ Battisti, A., Stastney, M., Netherer, S., Robinet, C., Schopf, A., Roques, A., Larsson, S. 2005. Expansion of geographic range in the pine processionary moth caused by increased winter temperatures. Ecological Applications 15: 2084-2096. Bentz, B.J., Regniere, J., Fettig, C.J., Hansen, E.M., Hayes, J.L., Hicke, J.A., Kelsey, R.G., Negron, J.F., and Seybold, S.J. 2010. Climate change and bark beetles of the western United States and Canada: direct and indirect effects. BioScience 60: 602-613. Berg, E.E., Henry, J.D., Fastie, C.L., De Volder, A.D., and Matsuoka, S.M. 2006. Spruce beetle outbreaks on the Kenai Peninsula, Alaska, and Kluane National Park and Reserve, Yukon Territory: relationship to summer temperatures and regional differences in disturbance regimes. Forest Ecology and Management 227: 219-232. Boone, C.K., Aukema, B.H., Bohlmann, J., Carroll, A.L., and Raffa, K.F. 2011. Efficacy of tree defense physiology varies with bark beetle population density: a basis for positive feedback in eruptive species. Canadian Journal of Forest Research 41: 1174-1188. 31  Breshears, D.D., Cobb, N.S., Rich, P.M., Price, K.P., Allen, C.D., Balice, R.G., Romme, W.H., Kastens, J.H., Floyd, M.L., Belnap, J., Anderson, J.J., Myers, O.B., and Meyer, C.W. 2005. Regional vegetation die-off in response to global-change-type drought. PNAS102: 15144-15148. Buse, A., and Good, J.E. 1996. Synchronization of larval emergence in winter moth (Operophtera brumata L.) and budburst in pedunculate oak (Quercus robur L.) under simulated climate change. Ecological Entomology 21: 335-343. Bylund, H. 1999. Climate and the population dynamics of two insect outbreak species in the north. Ecological Bulletins 47: 54-62. Carroll, A.L., Taylor, S.W., Regniere, J., and Safranyik, L. 2004. Effects of climate and climate change on the mountain pine beetle. In Challenges and Solutions: Proceedings of the Mountain Pine Beetle Symposium, Kelowna, British Columbia, 30 and 31 October 2003. Edited by T.L. Shore, J.E. Brooks, and J.E. Stone. Information Report BC-X-399, Pacific Forestry Centre, Canadian Forest Service, Natural Resources Canada, Victoria, British Columbia, pp. 221-230. Church, J.A., and White, N.J. 2006. A 20 th  century acceleration in global sea level rise. Geophysical Research Letters 33: L01602. Conner, R.N., Saenz, D., Rudolph, D.C., and Coulson, R.N. 1998. Southern pine beetle-induced mortality of pines with natural and artificial red-cockaded woodpecker cavities in Texas. Wilson Bulletin 110: 100-109. Croise, L., and Lieutier, F. 1993. Effects of drought on the induced defence reaction of Scots pine to bark beetle-associated fungi. Annals of Forest Science 50: 91-97 Dale, V.H., Joyce, L.A., McNulty, S., Neilson, R.P., Ayres, M.P., Flannigan, M.D., Hanson, P.J., Irland, L.C., Lugo, A.E., Peterson, C.J., Simberloff, D., Swanson, F.J., Stocks, B.J., and Wotton, B.M. 2001. Climate change and forest disturbances. BioScience 51: 723-734. Davis, M.B., and Shaw, R.G. 2001. Range shifts and adaptive responses to Quaternary climate change. Science 292: 673-679. Dongen, S.V., Backeljau, T., Matthysen, E., and Dhondt, A.A. 1997. Synchronization of hatching date with budburst of individual host tress (Quercus robur) in the winter moth (Operophtera brumata) and its fitness consequences. Journal of Animal Ecology 66: 113-121. Dulaurent, A.M., Porte, A.J., van Halder, I., Vetillard, F., Menassieu, P., Jactel, H. 2012. Hide and seek in forests: colonization by the pine processionary moth is impeded by the presence of nonhost trees. Agricultural and Forest Entomology 14: 19-27. Elverum, F., Johansen, T.J., and Nilssen, A.C. 2003. Life history, egg cold hardiness and diapause of Argyresthia retinella (Lepidoptera: Yponomeutidae). Norwegian Journal of Entomology 50: 43-53. Esper, J., Buntgen, U., Frank, D.C., Nievergelt, D., and Leibhold, A. 2007. 1200 years of regular outbreaks in alpine insects. Proc. R. Soc. B. 274: 671-679. 32  Feeny, P. 1970. Seasonal changes in oak leaf tannins and nutrients as a cause of spring feeding by winter moth caterpillars. Ecology 51: 565-581. Felton, A., Lindbladh, M., Brunet, J., Fritz, O. 2010. Replacing coniferous monocultures with mixed- species production stands: an assessment of the potential benefits for forest biodiversity in northern Europe. Forest Ecology and Management 260: 939-947. Gan, J. 2004. Risk and damage of southern pine beetle outbreaks under global climate change. Forest Ecology and Management 191: 61-71. Hamann, A., and Wang, T. 2006. Potential effects of climate change on ecosystem and tree species distribution in British Columbia. Ecology 87: 2773-2786. Hamrick, J.L. 2004. Response of forest trees to global environmental changes. Forest Ecology and Management 197: 323-335. Hegerl, G.C., von Storch, H., Hasselmann, K., Santer, B.D., Cubasch, U., and Jones, P.D. 1996. Detecting greenhouse-gas-induced climate change with an optimal fingerprint method. American Meteorological Society 9: 2281-2306. Hoch, G., Toffolo, E.P., Netherer, S., Battisti, A., and Schopf, A. 2009. Survival at low temperature of larvae of the pine processionary moth Thaumetopoea pityocampa from an area of range expansion. Agricultural and Forest Entomology 11: 313-320. Hodar, J.A., and Zamora, R. 2004. Herbivory and climatic warming: a Mediterranean outbreaking caterpillar attacks a relict, boreal pine species. Biodiversity and Conservation 13: 493-500. [IPCC] Intergovernmental Panel on Climate Change. 2007. Climate change 2007: the scientific basis. Cambridge University Press. Jepsen, J.U., Hagen, S.B., Ims, R.A., and Yoccoz, N.G. 2008. Climate change and outbreaks of the geometrids Operophtera brumata and Epirrita autumnata in subarctic birch forest: evidence of a recent outbreak range expansion. Journal of Animal Ecology 77: 257-264. Jonsson, A.M., Appelberg, G., Harding, S., and Barring, L. 2009. Spatio-temporal impact of climate change on the activity and voltinism of the spruce bark beetle, Ips typographus. Global Change Biology 15: 486-499. Kurz, W.A., Stinson, G., Rampley, G.J., Dymond, C.C., and Neilson, E.T. 2008. Risk of natural disturbances makes future contribution of Canada’s forests to the global carbon cycle highly uncertain. PNAS 105: 1551-1555. Kwok, R., and Rothrock, D.A. 2009. Decline in Arctic sea ice thickness from submarine and ICESAT records: 1958-2008. Geophysical Research Letters 36: L15501. Larsson, S., and Ohmart, C.P. 1988. Leaf age and larval performance of the leaf beetle Paropsis atomaria. Ecological Entomology, 13: 19-24. 33  Logan, J.A., and Powell, J.A. 2001. Ghost forests, global warming, and the mountain pine beetle (Coleoptera: Scolytidae). American Entomologist 47: 160-173 Mbogga, M.S., Hamann, A., and Wang, T. 2009. Historical and projected climate data for natural resource management in western Canada. Agricultural and Forest Meteorology 149: 881-890. Netherer, S., and Schopf, A. 2010. Potential effects of climate change on insect herbivores in European forests – general aspects and the pine processionary moth as specific example. Forest Ecology and Management 259: 831-838. Peterson, T.C., and Baringer, H.O. 2009. State of the climate in 2008. Special supplement to the bulletin of the American Meteorological Society. 90: S17-S18. Quinlan, F.T., Karl, T.R., and Williams, C.N., Jr. 1987. United States Historical Climatology Network (HCN) serial temperature and precipitation data. NDP-019. Carbon Dioxide Information Analysis Center. Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tennessee. Raffa, K.F., Aukema, B.H., Bentz, B.J., Carroll, A.L., Hicke, J.A., Turner, M.G., and Romme, W.H. 2008. Cross-scale drivers of natural disturbances prone to anthropogenic amplification: the dynamics of bark beetle eruptions. BioScience 58: 501-517. Robinet, C.R., Baier, P., Pennerstorfer, J., Schopf, A., and Roques, A. 2007. Modelling the effects of climate change on the potential feeding activity of Thaumetopoea pityocampa (Den. & Schiff.) (Lep., Notodontidae) in France. Global Ecol. Biogeogr. 16: 460-471. Safranyik, L., and Carroll, A.L. 2006. The biology and epidemiology of the mountain pine beetle in lodgepole pine forests. In The mountain pine beetle: a synthesis of its biology, management and impacts on lodgepole pine. Edited by L. Safranyik and B. Wilson. Pacific Forestry Centre, Canadian Forest Service, Natural Resources Canada, Victoria, British Columbia, pp. 3-66. Safranyik, L., Carroll, A.L., Regniere, J., Langor, D.W., Riel, W.G., Shore, T.L., Peter, B., Cooke, B.J., Nealis, V.G., and Taylor, S.W. 2010. Potential for range expansion of the mountain pine beetle into the boreal forest of North America. Can. Entomol. 142: 415-442. Santer, B.D., Taylor, K.E., Wigley, T.M.L., Johns, T.C., Jones, P.D., Karoly, D.J., Mitchell, J.F.B., Oort, A.H., Penner, J.E., Ramaswamy, V., Schwarzkopf, M.D., Stouffer, R.J., and Tett, S. 1996. A search for human influences on the thermal structure of the atmosphere. Nature 382: 39-46. Santer, B.D., Wehner, M.F., Wigley, T.M.L., Sausen, R., Meehl, G.A., Taylor, K.E., Ammann, C., Arblaster, J., Washington, W.M., Boyle, J.S., and Bruggemann, W. 2003. Contributions of anthropogenic and natural forcing to recent tropopause height changes. Science 301: 469-470. Santos, M.J., and Whitham, T.G. 2010. Predictors of Ips confusus outbreaks during a record drought in southwestern USA: implications for monitoring and management. Environmental Management45: 239-249. Schmitz, R.F., and Gibson, K.E. 1996. Douglas-fir beetle. USDA Forest Service, Forest Insect and Disease Leaflet 5. 34  Schultz, J.C., Nothnagle, P.J., Baldwin, I.T. 1982. Seasonal and individual variation in leaf quality of two northern hardwoods tree species. American Journal of Botany. 69: 753-759. Schweitzer, D.F. 1979. Effects of foliage age on body weight and survival in larvae of the tribe Lithophanini (Lepidoptera: Noctuidae). Oikos 32: 403-408. Seidl, R., Fernandes, P.M., Fonseca, T.F., Gillet, F., Jonsson, A.M., Merganicova, K., Netherer, S., Arpaci, A., Bontemps, J.-D., Bugmann, H., Gonzalez-Olabarria, J.R., Lasch, P., Meredieu, C., Moreira, F., Schelhaas, M.-J., and Mohren, F. 2011. Modelling natural disturbances in forest ecosystems: a review. Ecological Modelling 222: 903-924. Sherriff, R.L., Berg, E.E., and Miller, A.E. 2011. Climate variability and spruce beetle (Dendroctonus rufipennis) outbreaks in south-central and southwest Alaska. Ecology 92: 1459-1470. Soja, A.J., Tchebakova, N.M., French, N.H.F., Flannigan, M.D., Shugart, H.H., Stocks, B.J., Sukhinin, A.I., Parfenova, E.I., Chapin, F.S.III, and Stackhouse, P.W.Jr. 2007. Climate-induced boreal forest change: predictions versus current observations. Global and Planetary Change 56: 274-296. Stireman, III, J.O., Dyer, L.A., Janzen, D.H., Singer, M.S., Lill, J.T., Marquis, R.J., Ricklefs, R.E., Gentry, G.L., Hallwachs, W., Coley, P.D., Barone, J.A., Greeney, H.F., Connahs, H., Barbosa, P., Morais, H.C., and Diniz, I.R. 2005. Climatic unpredictability and parasitism of caterpillars: implications of global warming. PNAS 102: 17384-17387. Tenow, O. 1996. Hazards to a mountain birch forest – Abisko in perspective. Ecological Bulletins 45: 104-114. Tenow, O., Nilssen, A.C., Holmgren, B., and Elverum, F. 1999. An insect (Argyresthia retinella, Lep., Yponomeutidae) outbreak in northern birch forests, released by climatic changes? Journal of Applied Ecology 36: 111-122. Veblen, T.T., Hadley, K.S., Reid, M.S., Rebertus, A.J. 1991. Methods of detecting past spruce beetle outbreaks in Rocky Mountain subalpine forests. Canadian Journal of Forest Research 21: 242-254. Visser, M.E., and Holleman, L.J.M. 2001. Warmer springs disrupt the synchrony of oak and winter moth phenology. Proc R Soc Lond Ser B Biol Sci 268: 289-294. Watt, A.D., and MacFarlane, A.M. 1991. Winter moth on Sitka spruce: synchrony of egg hatch and budburst, and its effect on larval survival. Ecological Entomology 16: 387-390. Weber, U. 1997. Dendrochronological reconstruction and interpretation of larch budmoth (Zeiraphera diniana) outbreaks in two central alpine valleys of Switzerland from 1470-1990. Trees 11: 277-290. Wermelinger, B. 2004. Ecology and management of the spruce bark beetle Ips typographus – a review of recent research. Forest Ecology and Management 202: 67-82. Werner, R.A., and Holsten, E.H. 1985. Factors influencing generation times of spruce beetles in Alaska. Canadian Journal of Forest Research 15: 438-443. 35  Wotton, B.M., Nock, C.A., and Flannigan, M.D. 2010. Forest fire occurrence and climate change in Canada. International Journal of Wildland Fire 19: 253-271.


Citation Scheme:


Citations by CSL (citeproc-js)

Usage Statistics



Customize your widget with the following options, then copy and paste the code below into the HTML of your page to embed this item in your website.
                            <div id="ubcOpenCollectionsWidgetDisplay">
                            <script id="ubcOpenCollectionsWidget"
                            async >
IIIF logo Our image viewer uses the IIIF 2.0 standard. To load this item in other compatible viewers, use this url:


Related Items