Changing temperature and precipitation extremes in the Hindu Kush-Himalayan region: an analysis of CMIP3 and CMIP5 simulations and projections

被引:76
作者
Panday, Prajjwal K. [1 ]
Thibeault, Jeanne [2 ]
Frey, Karen E. [3 ]
机构
[1] Woods Hole Res Ctr, Falmouth, MA 02540 USA
[2] Univ Connecticut, Dept Geog, Storrs, CT USA
[3] Clark Univ, Grad Sch Geog, Worcester, MA 01610 USA
基金
美国国家科学基金会;
关键词
CMIP5; CMIP3; climate change; climate extremes; Hindu Kush-Himalaya; climate model; ensemble; ASIAN SUMMER MONSOON; CLIMATE-CHANGE; ENSEMBLE; INDEXES; SCENARIOS; GLACIER; WEATHER; EVENTS; WATER;
D O I
10.1002/joc.4192
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Hindu Kush-Himalayan (HKH) region epitomizes a geographic region where cryospheric processes coupled with hydrological regimes are under threat owing to a warming climate and shifts in climate extremes. In this study, we analyse global climate models in the Coupled Model Intercomparison Project phase 3 (CMIP3) and phase 5 (CMIP5) archives to investigate the qualitative aspects of change and trends in temperature and precipitation indices. Specifically, we examine and evaluate multi-model, multi-scenario climate change projections and seven extreme temperature and precipitation indices over the eastern Himalaya (EH) and western Himalaya-Karakoram (WH) regions for the 21st century. Density distribution plots of observed climate indices for meteorological stations and gridded indices are also analysed, which indicate significant negative trends in the annual number of frost days and significant increasing trends in warm nights in the EH region over the 1960-2000 period. Multi-model average (MMA) projections additionally indicate continued trends towards more extreme conditions consistent with a warmer, wetter climate. Precipitation projections indicate increased mean precipitation with more frequent extreme rainfall during monsoon season in the EH region, and a wetter cold season in the WH region. Time series of all MMA precipitation indices exhibit significant increasing trends over the 1901-2099 period. By comparison, time series of temperature indices show decreases in the intra-annual extreme temperature range and total number of frost days, as well as increases in warm nights. In general, these future projections point towards increases in summertime temperatures and modifications in precipitation across both regions.
引用
收藏
页码:3058 / 3077
页数:20
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