4.2 Article

Risk assessment of agricultural drought using the CERES-Wheat model: a case study of Henan Plain, China

Journal

CLIMATE RESEARCH
Volume 50, Issue 2-3, Pages 247-256

Publisher

INTER-RESEARCH
DOI: 10.3354/cr01060

Keywords

Crop model; Yield potential; Water-limited yield potential; Thresholds; Drought frequency

Funding

  1. National Key Technology Research and Development Program [2007BAC29B02]
  2. Special Fund for Public Welfare Industry [GYHY200906019]

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Droughts caused by a lack of precipitation are one of the major factors limiting agricultural crop production. It is thus important to assess the risk of such droughts in order to reduce their effect on agriculture. In the present study, the drought risk for crop production was assessed through an integrated approach that analyzed the relationship between crop yield and drought on the Henan Plain, China. We used the calibrated CERES-Wheat model to simulate 2 levels of wheat yield, the yield potential and the water-limited yield potential, at 66 weather stations. The yield gap between the yield potential and the water-limited yield potential was used as an indicator of the effects of a precipitation deficit on crop production under rain-fed conditions. A strong linear relationship between the yield gap and the amount of precipitation in the growing season was observed for each station during the period 1962-2009. A uniform criterion for drought severity thresholds for the entire Henan Plain was constructed based on the yield gap. For each station, the growing-season precipitation thresholds associated with different drought severities were then calculated based on the linear relationship between the yield gap and the amount of precipitation in the growing season. Drought frequencies derived from changes in the amount of precipitation during the growing season were also examined for all stations and spatially interpolated over the plain. The results showed diverse spatial patterns of frequency with respect to different drought types. Light droughts often occurred in the southern region, and moderate droughts occurred more frequently in the western and eastern regions. Severe drought displayed a generally decreasing trend from north to south.

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