Vegetation Greening and Climate Change Promote Multidecadal Rises of Global Land Evapotranspiration

被引:331
|
作者
Zhang, Ke [1 ,2 ,3 ,4 ]
Kimball, John S. [5 ]
Nemani, Ramakrishna R. [6 ]
Running, Steven W. [5 ]
Hong, Yang [2 ,3 ,8 ]
Gourley, Jonathan J. [7 ]
Yu, Zhongbo [4 ]
机构
[1] Univ Oklahoma, Cooperat Inst Mesosacle Meteorol Studies, Norman, OK 73072 USA
[2] Univ Oklahoma, Hydrometeorol & Remote Sensing HyDROS Lab, Norman, OK 73072 USA
[3] Univ Oklahoma, Sch Civil Engn & Environm Sci, Norman, OK 73072 USA
[4] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[5] Univ Montana, Numer Terradynam Simulat Grp, Missoula, MT 59812 USA
[6] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[7] NOAA, Natl Severe Storms Lab, Norman, OK 73072 USA
[8] Tsinghua Univ, Dept Hydraul Engn, Beijing 100084, Peoples R China
来源
SCIENTIFIC REPORTS | 2015年 / 5卷
关键词
INCREASE; CARBON; PRECIPITATION; TEMPERATURE; SIMULATION; DROUGHT; DATASET; TRENDS; IMPACT; CO2;
D O I
10.1038/srep15956
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Recent studies showed that anomalous dry conditions and limited moisture supply roughly between 1998 and 2008, especially in the Southern Hemisphere, led to reduced vegetation productivity and ceased growth in land evapotranspiration (ET). However, natural variability of Earth's climate system can degrade capabilities for identifying climate trends. Here we produced a long-term (1982-2013) remote sensing based land ET record and investigated multidecadal changes in global ET and underlying causes. The ET record shows a significant upward global trend of 0.88 mm yr(-2) (P < 0.001) over the 32-year period, mainly driven by vegetation greening (0.018% per year; P < 0.001) and rising atmosphere moisture demand (0.75 mm yr(-2); P = 0.016). Our results indicate that reduced ET growth between 1998 and 2008 was an episodic phenomenon, with subsequent recovery of the ET growth rate after 2008. Terrestrial precipitation also shows a positive trend of 0.66 mm yr(-2) (P = 0.08) over the same period consistent with expected water cycle intensification, but this trend is lower than coincident increases in evaporative demand and ET, implying a possibility of cumulative water supply constraint to ET. Continuation of these trends will likely exacerbate regional drought-induced disturbances, especially during regional dry climate phases associated with strong El Nino events.
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页数:9
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