4.7 Article

Identifying spatiotemporal propagation of droughts in the agro-pastoral ecotone of northern China with long-term WRF simulations

Journal

AGRICULTURAL AND FOREST METEOROLOGY
Volume 336, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.agrformet.2023.109474

Keywords

Drought propagation; Spatiotemporal continuity; Clustering algorithm; Agro-pastoral ecotone of northern; WRF

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Understanding the spatiotemporal evolution of droughts is crucial for food security and water allocation. This study proposes an approach to explore the simultaneous spatiotemporal evolution of droughts by constructing the linkage of propagation from meteorological drought to agricultural drought. The results show that 53.75% of meteorological drought events progress further to agricultural droughts, and agricultural droughts have a longer duration than meteorological droughts.
Understanding the spatiotemporal evolution of droughts is critical for food security and water allocation. In this study, we propose an approach to construct the linkage of the propagation from meteorological drought to agricultural drought to explore the simultaneous spatiotemporal evolution of droughts based on a 3-dimensional clustering algorithm. We first evaluate the improvement of the downscaled high-resolution outputs from the Weather Research and Forecasting (WRF) model to reanalysis data in detecting wet-dry variations in the agro-pastoral ecotone of northern China (APENC). The WRF simulation results well characterize the evolution of droughts with a high correlation coefficient of 0.82 (p<0.05), which implies that the WRF downscaling model provides reliable hydrometeorological results for assessing and analyzing long-term wet-dry variations. Subse-quently, we identify and track the spatiotemporal evolution of each individual drought event in the APENC for the first time. Based on the standardized precipitation index calculated from the WRF outputs, a total of 185 drought clusters were identified during 2000-2017, with 28 drought events lasting at least 3 months duration occurring in the APENC. The characteristics of the different drought events vary considerably. Droughts in the APENC have a larger percentage of propagation to the northeast and northwest and migrated hundreds of ki-lometers from the source sites. The results of the propagation of meteorological droughts to agricultural droughts indicate that 53.75% of the meteorological drought events progressed further to agricultural droughts. Agri-cultural droughts exhibit spatial variations consistent with meteorological droughts. Agricultural droughts have 1.69 months onset lag time, 2.12 months termination lag time, and overall longer duration than meteorological droughts in the APENC. Our findings provide valuable information for the mechanism and prediction of drought propagation.

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