在亚洲高山地区,平均和极端降雪的趋势正在下降
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Updated: Jul 2, 2025

08:20
In Situ Soil Moisture Sensors in Undisturbed Soils
Published on: November 18, 2022
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Fan Sun1, Yaning Chen2, Yupeng Li3
1State Key Laboratory of Desert and Oasis Ecology, Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, China; University of the Chinese Academy of Sciences, Beijing 10049, China.
The Science of the total environment
|February 26, 2024
概括
高山亚洲正在经历降雪的显著减少,极端降雪事件正在减少,并在特定的温度和湿度条件下发生. 像AMO和SOI这样的气候振荡会影响降雪变化,影响区域风险管理.
科学领域:
- 气候学 气候学 气候学
- 气象学 天气学
- 水文学的水文学
背景情况:
- 高山亚洲 (HMA) 地区的强烈变暖改变了降水量,但降雪极端情况仍未得到充分研究.
- 了解降雪变化对于水资源管理和HMA的防灾准备至关重要.
研究的目的:
- 调查HMA (1979-2020) 中非极端和极端降雪的空间和时间变化.
- 在极端和非极端降雪事件期间比较天气系统.
- 确定影响降雪波动的循环因素.
主要方法:
- 利用多个来源的气象数据进行降雪分析.
- 在极端和非极端事件期间对天气系统进行了综合分析.
- 采用逐步回归来将降雪与气候振荡联系起来.
主要成果:
- 总体降雪量,天数,分数和季节长度的显著下降.
- 极端降雪指标,如连续几天的最大降雪量,重度降雪和极度重度降雪日均出现显著下降.
- 极端降雪事件与-5°C至3°C之间的温度,更高的湿度和降水有关.
结论:
- 气候变化正在减少HMA的降雪量,极端降雪事件显著减少.
- 大西洋多季度振荡影响年平均降雪量,而南方振荡指数主要影响极端降雪变化.
- 研究结果为区域气候变化影响评估,风险管理和灾害适应提供了关键的见解.
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