4.5 Article

Seasonal divergence in the sensitivity of evapotranspiration to climate and vegetation growth in the Yellow River Basin, China

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
Volume 122, Issue 1, Pages 103-118

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2016JG003648

Keywords

evapotranspiration; seasonal divergence; climate change; vegetation growth; interannual sensitivity; Yellow River Basin

Funding

  1. National Natural Science Foundation of China [41390462, 41130640, 41571038]
  2. PCSIRT [IRT_15R06]
  3. state Key Laboratory of Earth Surface Processes and Resource Ecology

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Seasonal variations in terrestrial evapotranspiration (ET) in the Yellow River Basin (YRB) have crucial impacts on the seasonal trajectories of the regional water cycle, vegetation growth, and local climate feedback. However, the possibly divergent roles of climate and vegetation growth variations in controlling seasonal ET patterns remain poorly quantified. This study therefore quantifies the interannual sensitivity and attribution of ET to climate and vegetation growth variations in different seasons and different biomes in the YRB in China between 1982 and 2011, using the satellite-derived normalized difference vegetation index (NDVI), FLUXNET-based upscaled ET, and concurrent climate data. The results reveal a clear seasonal divergence in the interannual sensitivity of ET to climate and vegetation growth variations in the YRB. Interannual precipitation and NDVI variations play a dominant role in controlling seasonal ET variations in the YRB, with temperature having a marginal effect. Interannual ET sensitivity to precipitation weakens with an increasing mean annual precipitation gradient in almost all seasons, especially in summer and autumn. More importantly, a seasonally varying role of vegetation growth in mediating seasonal ET was discovered, and a crucial role of late-growing-season vegetation growth in controlling the seasonal trajectory of regional ET was explicitly identified. These results suggest that ongoing intensive vegetation restoration has crucial impacts on seasonal water-cycle patterns and consequent terrestrial-atmospheric biogeochemical feedback in the YRB.

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