Spruce BudwormWeather is a critical factor in determining spruce budworm distribution. Sudden upsurges in budworm numbers generally follow drought and the visible effects of these outbreaks begin after hot, dry summers. Drought stresses the trees, reducing their resistance, and elevated summer temperatures increase budworm reproduction. For example, female budworms lay 50% more eggs at 25˚C than at 15˚C. Also, higher temperatures and drought can shift the timing of budworm reproduction such that their natural predators are no longer effective in limiting budworm numbers. Conversely, cold weather can stop a budworm outbreak. Budworms starve if a late spring frost kills the new shoot growth of the trees on which the larvae feed. Thus it is to be expected that climate warming would result in the northward movement of the spruce budworm and this has already occurred. Before 1990, spruce budworm had not appeared able to reproduce in the boreal forest of central Alaska. Then, in 1990, after a series of warm summers, a sudden and major upsurge in spruce budworm numbers occurred and visible damage to the forest canopy spread over several tens of thousands of hectares of white spruce forest. Populations of spruce budworm have since persisted in this area near the Arctic Circle. The entire range of white spruce forests in North America is considered vulnerable to outbreaks of spruce budworm under projected climate change. In the Northwest Territories of Canada, for example, the northern limit of current spruce budworm outbreaks is approximately 400 kilometers south of the northern limit of its host, the white spruce. Therefore, there is potential for a northward expansion of spruce budworm to take over this remaining 400 kilometer-wide band of currently unaffected white spruce forest. Source & © ACIA Impacts of a Warming Arctic: Arctic Climate Impact Assessment Related publication:
Other Figures & Tables on this publication: Observed Arctic Temperature, 1900 to Present Observed sea ice September 1979 and September 2003 Projected Vegetation, 2090-2100 Arctic Thermohaline Circulation Projected Arctic Surface Air Temperatures Projected opening of northern navigation routes Factors influencing UV at the surface 1000 years of changes in carbon emissions Projected Surface Air Temperature change 1990-2090 Melt of the Greenland Ice Sheet The Gwich’in and the Porcupine Caribou Herd Seals Become Elusive for Inuit in Nunavut Observed Climate Change Impacts in Sachs Harbour, Canada Indigenous knowledge and observations of current trends Case study of interacting changes: Saami reindeer herders Indigenous knowledge and observations of current trends Indigenous knowledge and observations of current trends |