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Canadian snow and sea ice: historical trends and projections

机译:加拿大的雪和海冰:历史趋势和预测

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The Canadian Sea Ice and Snow Evolution (CanSISE) Network is a climate research network focused on developing and applying state of the art observational data to advance dynamical prediction, projections, and understanding of seasonal snow cover and sea ice in Canada and the circumpolar Arctic. Here, we present an assessment from the CanSISE Network on trends in the historical record of snow cover (fraction, water equivalent) and sea ice (area, concentration, type, and thickness) across Canada. We also assess projected changes in snow cover and sea ice likely to occur by mid-century, as simulated by the Coupled Model Intercomparison Project Phase 5 (CMIP5) suite of Earth system models. The historical datasets show that the fraction of Canadian land and marine areas covered by snow and ice is decreasing over time, with seasonal and regional variability in the trends consistent with regional differences in surface temperature trends. In particular, summer sea ice cover has decreased significantly across nearly all Canadian marine regions, and the rate of multi-year ice loss in the Beaufort Sea and Canadian Arctic Archipelago has nearly doubled over the last 8 years. The multi-model consensus over the 2020–2050 period shows reductions in fall and spring snow cover fraction and sea ice concentration of 5–10?% per decade (or 15–30?% in total), with similar reductions in winter sea ice concentration in both Hudson Bay and eastern Canadian waters. Peak pre-melt terrestrial snow water equivalent reductions of up to 10?% per decade (30?% in total) are projected across southern Canada.
机译:加拿大海冰与积雪演变(CanSISE)网络是一个气候研究网络,致力于开发和应用最先进的观测数据,以推动动力学预测,预测以及对加拿大和极地北极季节性积雪和海冰的了解。在这里,我们提供了CanSISE网络对加拿大全雪覆盖(分数,水当量)和海冰(面积,浓度,类型和厚度)历史记录趋势的评估。我们还评估了地球系统模型的耦合模型比较项目第5阶段(CMIP5)模型所模拟的,预计到本世纪中叶可能发生的积雪和海冰变化。历史数据表明,加拿大陆地和海洋地区被冰雪覆盖的比例随着时间的推移而下降,趋势的季节和区域变化与地表温度趋势的区域差异一致。特别是,几乎加拿大所有海洋地区的夏季海冰覆盖量都已大大减少,过去八年来,波弗特海和加拿大北极群岛的多年冰损失率几乎翻了一番。 2020年至2050年期间的多模型共识显示,秋季和春季积雪覆盖率减少,海冰浓度每十年降低5-10%(或总计15-30%),而冬季海冰也有类似的减少集中在哈德逊湾和加拿大东部水域。预计加拿大南部地区最高的融化前陆地雪水当量峰值每十年减少10%(总计30%)。

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