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首页> 外文期刊>The Cryosphere >Anthropogenic climate change versus internal climate variability: impacts on snow cover in the Swiss Alps
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Anthropogenic climate change versus internal climate variability: impacts on snow cover in the Swiss Alps

机译:人为气候变化与内部气候变化:瑞士阿尔卑斯山区对雪覆盖的影响

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摘要

Snow is a sensitive component of the climate system. In many parts of the world, water stored as snow is a vital resource for agriculture, tourism and the energy sector. As uncertainties in climate change assessments are still relatively large, it is important to investigate the interdependencies between internal climate variability and anthropogenic climate change and their impacts on snow cover. We use regional climate model data from a new single-model large ensemble with 50?members (ClimEX LE) as a driver for the physically based snow model SNOWPACK at eight locations across the Swiss Alps. We estimate the contribution of internal climate variability to uncertainties in future snow trends by applying a Mann–Kendall test for consecutive future periods of different lengths (between 30 and 100?years) until the end of the 21st century. Under RCP8.5, we find probabilities between 10 % and 60 % that there will be no significant negative trend in future mean snow depths over a period of 50?years. While it is important to understand the contribution of internal climate variability to uncertainties in future snow trends, it is likely that the variability of snow depth itself changes with anthropogenic forcing. We find that relative to the mean, interannual variability of snow increases in the future. A decrease in future mean snow depths, superimposed by increases in interannual variability, will exacerbate the already existing uncertainties that snow-dependent economies will have to face in the future.
机译:雪是气候系统的敏感成分。在世界的许多地方,作为雪的水是农业,旅游和能源部门的重要资源。由于气候变化评估的不确定性仍然相对较大,重要的是要调查内部气候变异性和人为气候变化的相互依赖性及其对雪覆盖的影响。我们将区域气候模型数据从新的单型大型集合中使用50?成员(Climex Le)作为瑞士阿尔卑斯山的八个地点的物理基础的雪地模型积雪的司机。我们估计内部气候变化对未来雪趋势的不确定性的贡献,通过在21世纪结束至21世纪结束之前应用了Mann-Kendall测试,以便连续未来的不同长度(在30到100岁之间)。根据RCP8.5,我们发现10%至60%之间的概率在未来的平均雪深度在50岁的时候没有显着的负面趋势。虽然重要的是要了解内部气候变化对未来雪趋势的不确定性的贡献,但很可能随着人为强制而变化的雪深度本身变化。我们发现,相对于未来雪的平均际变化增加。未来平均雪深度的减少,依然变化的增加叠加,将加剧已经存在雪依赖经济将来会面临的现有的不确定性。

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