Soil-vegetation moisture capacitor maintains dry season vegetation productivity over India

被引:10
|
作者
Sebastian, Dawn E. E. [1 ,2 ]
Murtugudde, Raghu [3 ,4 ]
Ghosh, Subimal [1 ,4 ]
机构
[1] Indian Inst Technol, Dept Civil Engn, Mumbai 400076, India
[2] Ctr Water Resources Dev & Management, Kozhikode 673571, Kerala, India
[3] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr ESSIC DOAS, College Pk, MD USA
[4] Indian Inst Technol, Interdisciplinary Program Climate Studies, Mumbai 400076, India
关键词
EARTH SYSTEM MODELS; CLIMATE-CHANGE; INTERANNUAL VARIABILITY; PLANT-RESPONSES; SUMMER MONSOON; INCREASING CO2; LAND; ATMOSPHERE; WATER; RAINFALL;
D O I
10.1038/s41598-022-27277-6
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
India receives more than 70% of its annual rainfall in the summer monsoon from June to September. The rainfall is scanty and scattered for the rest of the year. Combining satellite data and model simulations, we show that the soil-vegetation continuum works as a natural capacitor of water, storing the monsoon pulse and releasing the moisture to the atmosphere through evapotranspiration over approximately 135 days when the moisture supply from precipitation is less than the evapotranspiration losses. The total Gross Primary Productivity of vegetation in India during the capacitor period accounts for almost 35% of the total annual GPP value. It primarily depends on the soil moisture at the beginning of the period, a measure of moisture capacitance of soil, with a correlation of 0.6. Given that India is the second largest contributor to recent global greening, its soil-vegetation water capacitance plays a significant role in the global carbon balance.
引用
收藏
页数:10
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