气候变化领域集成服务门户(CCPortal): Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013)

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DOI	10.5194/tc-9-1229-2015
	Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013)
	Salerno, F.; Guyennon, N.; Thakuri, S.; Viviano, G.; Romano, E.; Vuillermoz, E.; Cristofanelli, P.; Stocchi, P.; Agrillo, G.; Ma, Y.; Tartari, G.
通讯作者	Salerno, F (通讯作者)
发表日期	2015
ISSN	1994-0416
EISSN	1994-0424
起始页码	1229
结束页码	1247
卷号	9 期号:3
英文摘要	Studies on recent climate trends from the Himalayan range are limited, and even completely absent at high elevation (> 5000ma.s.l.). This study specifically explores the southern slopes of Mt. Everest, analyzing the time series of temperature and precipitation reconstructed from seven stations located between 2660 and 5600ma.s.l. during 1994-2013, complemented with the data from all existing ground weather stations located on both sides of the mountain range (Koshi Basin) over the same period. Overall we find that the main and most significant increase in temperature is concentrated outside of the monsoon period. Above 5000ma.s.l. the increasing trend in the time series of minimum temperature (+ 0.072 degrees C yr(-1)) is much stronger than of maximum temperature (+ 0.009 degrees C yr(-1)), while the mean temperature increased by + 0.044 degrees C yr(-1). Moreover, we note a substantial liquid precipitation weakening (9.3mmyr(-1)) during the monsoon season. The annual rate of decrease in precipitation at higher elevations is similar to the one at lower elevations on the southern side of the Koshi Basin, but the drier conditions of this remote environment make the fractional loss much more consistent (47% during the monsoon period). Our results challenge the assumptions on whether temperature or precipitation is the main driver of recent glacier mass changes in the region. The main implications are the following: (1) the negative mass balances of glaciers observed in this region can be more ascribed to a decrease in accumulation (snowfall) than to an increase in surface melting; (2) the melting has only been favoured during winter and spring months and close to the glaciers terminus; (3) a decrease in the probability of snowfall (10 %) has made a significant impact only at glacier ablation zone, but the magnitude of this decrease is distinctly lower than the observed decrease in precipitation; (4) the decrease in accumulation could have caused the observed decrease in glacier flow velocity and the current stagnation of glacier termini, which in turn could have produced more melting under the debris glacier cover, leading to the formation of numerous supraglacial and proglacial lakes that have characterized the region in the last decades.
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000360659200015
来源期刊	CRYOSPHERE
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/258524
推荐引用方式 GB/T 7714	Salerno, F.,Guyennon, N.,Thakuri, S.,et al. Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013)[J]. 中国科学院青藏高原研究所,2015,9(3).
APA	Salerno, F..,Guyennon, N..,Thakuri, S..,Viviano, G..,Romano, E..,...&Tartari, G..(2015).Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013).CRYOSPHERE,9(3).
MLA	Salerno, F.,et al."Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013)".CRYOSPHERE 9.3(2015).