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首页> 外文期刊>Science in China. Series D, Earth sciences >Global glacial fluctuations in response to climatic change in the past 40 a
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Global glacial fluctuations in response to climatic change in the past 40 a

机译:过去40 a来因应气候变化的全球冰川波动

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Analyses on glacier fluctuations for the past 40 a show that glacial fluctuations were obviously regional over the world. Amplitudes of glacier fluctuations were smaller in northern Europe and high Asia (H Asia) regions than in northern America and the Alps regions. Retreating glaciers were dominant in northern European and high Asia regions, while remarkable glacial advance emerged in different periods in northern America and the Alps regions. Sensitivity of glaciers in the varying scales to climatic change was different. Time lag for reactions to climatic change between larger glaciers (length > 5 km) and smaller glaciers (length ≤ 5 km) has been found. In the globe, glacial fluctuations well correspond to climatic change. Fluctuation lags behind climatic change were about 8 a for larger glaciers and about 2 a for smaller glaciers.
机译:对过去40 a的冰川波动进行的分析表明,冰川波动显然是全球性的区域性变化。北欧和高亚洲(H Asia)地区的冰川波动幅度小于北美和阿尔卑斯山地区。在北欧和高亚洲地区,后退冰川占主导地位,而北美和阿尔卑斯山地区则在不同时期出现了明显的冰川发展。不同尺度的冰川对气候变化的敏感性不同。已发现较大冰川(长度> 5 km)和较小冰川(长度≤5 km)之间对气候变化的反应存在时滞。在全球范围内,冰川波动很好地与气候变化相对应。气候变化后的波动滞后对于较大的冰川大约为8 a,对于较小的冰川大约为2 a。

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