Projections of the Advance in the Start of the Growing Season during the 21st Century Based on CMIP5 Simulations

被引:0
|
作者
XIA Jiangjiang [1 ]
YAN Zhongwei [1 ]
JIA Gensuo [1 ]
ZENG Heqing [2 ]
Philip Douglas JONES [3 ,4 ]
ZHOU Wen [5 ]
ZHANG Anzhi [1 ]
机构
[1] Key Laboratory of Regional Climate-Environment for East Asia, Institute of Atmospheric Physics,Chinese Academy of Sciences
[2] Ministry of Environmental Protection of Jiuzhaigou Country  3. Climatic Research Unit, University of East Anglia
[3] Guy Carpenter Asia-Pacific Climate Impact Centre, School of Energy and Environment,City University of Hong Kong
[4] Center of Excellence for Climate Change Research and Department of Meteorology,King Abdulaziz University
基金
中国国家自然科学基金;
关键词
start of growing season(SOS); normalized difference vegetation index(NDVI); temperature sensitivity; Repre-sentative Concentration;
D O I
暂无
中图分类号
P467 [气候变化、历史气候];
学科分类号
0706 ; 070601 ;
摘要
It is well-known that global warming due to anthropogenic atmospheric greenhouse effects advanced the start of the vegetation growing season(SOS) across the globe during the 20 th century. Projections of further changes in the SOS for the 21 st century under certain emissions scenarios(Representative Concentration Pathways, RCPs) are useful for improving understanding of the consequences of global warming. In this study, we first evaluate a linear relationship between the SOS(defined using the normalized difference vegetation index) and the April temperature for most land areas of the Northern Hemisphere for 1982–2008. Based on this relationship and the ensemble projection of April temperature under RCPs from the latest state-of-the-art global coupled climate models, we show the possible changes in the SOS for most of the land areas of the Northern Hemisphere during the 21 st century. By around 2040–59, the SOS will have advanced by-4.7 days under RCP2.6,-8.4 days under RCP4.5, and-10.1 days under RCP8.5, relative to 1985–2004. By 2080–99, it will have advanced by-4.3 days under RCP2.6,-11.3 days under RCP4.5, and-21.6 days under RCP8.5. The geographic pattern of SOS advance is considerably dependent on that of the temperature sensitivity of the SOS. The larger the temperature sensitivity,the larger the date-shift-rate of the SOS.
引用
收藏
页码:831 / 838
页数:8
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