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人为变暖导致北半球积雪减少 快报文章
气候变化快报,2024年第3期
作者:  董利苹
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:539/0  |  提交时间:2024/02/05
Human Influence  Northern Hemisphere  Snow Loss  Evidence  
美研究指出气候变暖增加极端降水风险 快报文章
气候变化快报,2023年第14期
作者:  刘莉娜
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:580/0  |  提交时间:2023/07/19
Warming  Rainfall Extremes  Snow  
海藻的大量繁殖使太平洋西北地区的融雪量增加了20% 快报文章
资源环境快报,2023年第13期
作者:  李恒吉
Microsoft Word(17Kb)  |  收藏  |  浏览/下载:514/0  |  提交时间:2023/07/15
Snow algae  NSF  Climate change  Snow melt  
气候变暖导致以雪为主导的生态系统功能普遍发生变化 快报文章
气候变化快报,2022年第15期
作者:  刘燕飞
Microsoft Word(17Kb)  |  收藏  |  浏览/下载:621/0  |  提交时间:2022/08/05
Ecosystem Function  Snow  Warming  
全球变化背景下水资源变得难以预测 快报文章
资源环境快报,2022年第14期
作者:  吴秀平
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:638/1  |  提交时间:2022/07/31
snow-dominated ecosystem  climate change  
NOAA报告显示2021年是有记录以来的第六热年份 快报文章
气候变化快报,2022年第03期
作者:  董利苹
Microsoft Word(17Kb)  |  收藏  |  浏览/下载:751/0  |  提交时间:2022/02/06
Global Climate  global surface temperature  Ocean Heat Content  Snow  Sea Ice  Tropical Cyclones  
全球雪旱分布的热点地区及特征分析 快报文章
资源环境快报,2020年第16期
作者:  王立伟,宋晓谕
Microsoft Word(16Kb)  |  收藏  |  浏览/下载:428/0  |  提交时间:2020/08/29
Global snow drought  hot spots  characteristics  
北半球第一个积雪的可靠估计量面世 快报文章
气候变化快报,2020年第12期
作者:  董利苹
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:411/0  |  提交时间:2020/06/19
Northern Hemisphere  snow mass  
Assimilating multi-satellite snow data in ungauged Eurasia improves the simulation accuracy of Asian monsoon seasonal anomalies 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (6)
作者:  Lin, Peirong;  Yang, Zong-Liang;  Wei, Jiangfeng;  Dickinson, Robert E.;  Zhang, Yongfei;  Zhao, Long
收藏  |  浏览/下载:9/0  |  提交时间:2020/08/18
Asian monsoon  dynamical seasonal forecast  multi-satellite snow data assimilation  GRACE  MODIS  
Patterns and trends of Northern Hemisphere snow mass from 1980 to 2018 期刊论文
NATURE, 2020, 581 (7808) : 294-+
作者:  Ibrahim, Nizar;  Maganuco, Simone;  Dal Sasso, Cristiano;  Fabbri, Matteo;  Auditore, Marco;  Bindellini, Gabriele;  Martill, David M.;  Zouhri, Samir;  Mattarelli, Diego A.;  Unwin, David M.;  Wiemann, Jasmina;  Bonadonna, Davide;  Amane, Ayoub;  Jakubczak, Juliana;  Joger, Ulrich;  Lauder, George V.;  Pierce, Stephanie E.
收藏  |  浏览/下载:16/0  |  提交时间:2020/05/25

Warming surface temperatures have driven a substantial reduction in the extent and duration of Northern Hemisphere snow cover(1-3). These changes in snow cover affect Earth'  s climate system via the surface energy budget, and influence freshwater resources across a large proportion of the Northern Hemisphere(4-6). In contrast to snow extent, reliable quantitative knowledge on seasonal snow mass and its trend is lacking(7-9). Here we use the new GlobSnow 3.0 dataset to show that the 1980-2018 annual maximum snow mass in the Northern Hemisphere was, on average, 3,062 +/- 35 billion tonnes (gigatonnes). Our quantification is for March (the month that most closely corresponds to peak snow mass), covers non-alpine regions above 40 degrees N and, crucially, includes a bias correction based on in-field snow observations. We compare our GlobSnow 3.0 estimates with three independent estimates of snow mass, each with and without the bias correction. Across the four datasets, the bias correction decreased the range from 2,433-3,380 gigatonnes (mean 2,867) to 2,846-3,062 gigatonnes (mean 2,938)-a reduction in uncertainty from 33% to 7.4%. On the basis of our bias-corrected GlobSnow 3.0 estimates, we find different continental trends over the 39-year satellite record. For example, snow mass decreased by 46 gigatonnes per decade across North America but had a negligible trend across Eurasia  both continents exhibit high regional variability. Our results enable a better estimation of the role of seasonal snow mass in Earth'  s energy, water and carbon budgets.


Applying a bias correction to a state-of-the-art dataset covering non-alpine regions of the Northern Hemisphere and to three other datasets yields a more constrained quantification of snow mass in March from 1980 to 2018.