Monitoring Daily All-Sky Evapotranspiration Over the East Asian Continent Using Multi-Channel Passive Microwave Measurements From Fengyun-3B Satellite of China

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Yipu Wang, Jiheng Hu, Rui Li, Peng Zhang, Binbin Song, Qingyang Liu
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Abstract

Terrestrial evapotranspiration (ET) modulates energy and water cycles of land-atmosphere continuum. Satellite daily ET estimation under all sky (both clear and cloudy sky) remains challenging due to the difficulty in detecting vegetation dynamics under cloud cover. In this study, we utilized the microwave land surface Emissivity Difference Vegetation Index (EDVI) at X- and K-bands, which was retrieved from Chinese Fengyun-3B satellite Microwave Radiation Imager (MWRI) measurements under all sky conditions, to derive daily ET (ETFYEDVI) over East Asia (80–145°E, 10–55°N) from 2016 to 2018, in combination with multi-source satellite all-sky radiation and ERA5 climatic data. The Fengyun-3B EDVI was used to represent the key vegetation characteristic for allocating total available energy and constraining canopy conductance. ETFYEDVI was validated at multiple spatiotemporal scales, against daily in situ measurements from eight flux sites and annual water balance method at nine river basins. Site-scale validations showed that ETFYEDVI generated overall good accuracy (R2 = 0.78, bias of −0.1 mm day−1) across forest, grass, crop, and desert sites. Basin-scale evaluations further demonstrated the stable and small bias (R2 of 0.96, bias of −22.2 mm year−1) in annual ETFYEDVI from southern humid to arid inland basins. This accuracy was comparable or better than those of four global satellite ET products. More importantly, ETFYEDVI produced low and stable accumulative bias under increasing cloud conditions, and characterized the spatiotemporal variability in continental ET even under heavy cloud cover (>90%) conditions. This study marks the first attempt to use Fengyun-3 satellite passive microwave measurements to produce continental-scale ET, showing great potential for mapping spatiotemporally continuous global daily ET.

利用中国风云3b卫星多通道无源微波监测东亚大陆全天蒸散量
陆地蒸散发调节着陆地-大气连续体的能量和水循环。全天(晴空和多云)下的卫星日蒸散发估算仍然具有挑战性,因为很难探测云层下的植被动态。本研究利用中国风云三号乙卫星微波辐射成像仪(MWRI)在所有天空条件下的X波段和k波段微波地表发射率差异植被指数(EDVI),结合多源卫星全天辐射和ERA5气候数据,反演了2016 - 2018年东亚地区(80-145°E, 10-55°N)的日ET (ETFYEDVI)。利用风云三号乙EDVI代表了分配总有效能和约束冠层电导的关键植被特征。ETFYEDVI在多个时空尺度上进行了验证,对比了8个通量站点的每日现场测量数据和9个流域的年水平衡方法。站点尺度验证表明,ETFYEDVI在森林、草地、作物和沙漠站点上产生了良好的总体精度(R2 = 0.78,偏差为- 0.1 mm day - 1)。流域尺度评价进一步表明,南方湿润内陆盆地对干旱内陆盆地的ETFYEDVI的年偏差稳定且较小(R2为0.96,偏差为- 22.2 mm /年- 1)。这一精度与四种全球卫星ET产品相当或更好。更重要的是,ETFYEDVI在云量增加的条件下产生了低而稳定的累积偏置,即使在重云量(>90%)条件下,也表现出大陆ET的时空变异特征。该研究标志着首次尝试利用风云三号卫星无源微波测量产生大陆尺度ET,显示出绘制时空连续全球日ET的巨大潜力。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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