Glacially mediated impacts of climate warming on alpine lakes of the Canadian Rocky Mountains

R. Vinebrooke, Patrick L. Thompson, W. Hobbs, B. Luckman, M. Graham, A. P. Wolfe
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引用次数: 21

Abstract

Climate warming is having a more pronounced impact ontemperature change in alpine and polar regions than on aglobal scale (Beniston 2006, Lemke et al. 2007). For theCordillera region of North America, climate models predictthat warming will increase with elevation, reaching its maxi-mum at mid-northern latitudes (Bradley et al. 2004). Den-drochronological models have already shown that summertemperatures in the Canadian Rockies were anomalouslywarm during the 20
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冰川介导的气候变暖对加拿大落基山脉高山湖泊的影响
气候变暖对高寒地区和极地地区的温度变化的影响比对全球范围的影响更为明显(Beniston 2006, Lemke et al. 2007)。对于北美的科迪勒拉地区,气候模式预测变暖将随着海拔的升高而增加,在中北纬度地区达到最大值(Bradley et al. 2004)。dendro年代学模型已经显示,加拿大落基山脉的夏季温度在20世纪20年代异常温暖
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