干旱
灌溉
季风
气候学
湿度
显热
相对湿度
环境科学
地质学
大气科学
气象学
地理
农学
生物
古生物学
作者
Vimal Mishra,Anukesh Krishnankutty Ambika,Akarsh Asoka,Saran Aadhar,Jonathan Buzan,Rohini Kumar,Matthew Huber
出处
期刊:Nature Geoscience
[Nature Portfolio]
日期:2020-10-26
卷期号:13 (11): 722-728
被引量:186
标识
DOI:10.1038/s41561-020-00650-8
摘要
Intensive irrigation in India has been demonstrated to decrease surface temperature, but the influence of irrigation on humidity and extreme moist heat stress is not well understood. Here we analysed a combination of in situ and satellite-based datasets and conducted meteorological model simulations to show that irrigation modulates extreme moist heat. We found that intensive irrigation in the region cools the land surface by 1 °C and the air by 0.5 °C. However, the decreased sensible heat flux due to irrigation reduces the planetary boundary layer height, which increases low-level moist enthalpy. Thus, irrigation increases the specific and relative humidity, which raises the moist heat stress metrics. Intense irrigation over the region results in increased moist heat stress in India, Pakistan, and parts of Afghanistan—affecting about 37–46 million people in South Asia—despite a cooler land surface. We suggest that heat stress projections in India and other regions dominated by semi-arid and monsoon climates that do not include the role of irrigation overestimate the benefits of irrigation on dry heat stress and underestimate the risks. Intensive irrigation in India cools the land surface, but increases the moist heat stress in South Asia, according to an analysis of observational datasets and meteorological models.
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