Soil moisture drought in China, 1950-2006
Soil moisture drought in China, 1950-2006
Four physically based land surface hydrology models driven by a common observation-based 3-hourly meteorological dataset were used to simulate soil moisture over China for the period 1950-2006. Monthly values of total column soil moisture from the simulations were converted to percentiles and an ensemble method was applied to combine all model simulations into a multimodel ensemble from which agricultural drought severities and durations were estimated. A cluster analysis method and severity-area-duration (SAD) algorithm were applied to the soil moisture data to characterize drought spatial and temporal variability. For drought areas greater than 150 000 km2 and durations longer than 3 months, a total of 76 droughts were identified during the 1950-2006 period. The duration of 50 of these droughts was less than 6 months. The five most prominent droughts, in terms of spatial extent and then duration, were identified. Of these, the drought of 1997-2003 was the most severe, accounting for the majority of the severity-area-duration envelope of events with areas smaller than 5 million km2. The 1997-2003 drought was also pervasive in terms of both severity and spatial extent. It was also found that soil moisture in north central and northeastern China had significant downward trends, whereas most of Xinjiang, the Tibetan Plateau, and small areas of Yunnan province had significant upward trends. Regions with downward trends were larger than those with upward trends (37% versus 26% of the land area), implying that over the period of analysis, the country has become slightly drier in terms of soil moisture. Trends in drought severity, duration, and frequency suggest that soil moisture droughts have become more severe, prolonged, and frequent during the past 57 yr, especially for northeastern and central China, suggesting an increasing susceptibility to agricultural drought.
Drought, Ensembles, Hydrology, Land surface model, Soil moisture
3257-3271
Wang, Aihui
ebd4d701-e96c-497f-9402-38b56fb76d3c
Lettenmaier, Dennis P.
c3ae7db6-9f48-4875-8052-9e16fd099c09
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
1 July 2011
Wang, Aihui
ebd4d701-e96c-497f-9402-38b56fb76d3c
Lettenmaier, Dennis P.
c3ae7db6-9f48-4875-8052-9e16fd099c09
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wang, Aihui, Lettenmaier, Dennis P. and Sheffield, Justin
(2011)
Soil moisture drought in China, 1950-2006.
Journal of Climate, 24 (13), .
(doi:10.1175/2011JCLI3733.1).
Abstract
Four physically based land surface hydrology models driven by a common observation-based 3-hourly meteorological dataset were used to simulate soil moisture over China for the period 1950-2006. Monthly values of total column soil moisture from the simulations were converted to percentiles and an ensemble method was applied to combine all model simulations into a multimodel ensemble from which agricultural drought severities and durations were estimated. A cluster analysis method and severity-area-duration (SAD) algorithm were applied to the soil moisture data to characterize drought spatial and temporal variability. For drought areas greater than 150 000 km2 and durations longer than 3 months, a total of 76 droughts were identified during the 1950-2006 period. The duration of 50 of these droughts was less than 6 months. The five most prominent droughts, in terms of spatial extent and then duration, were identified. Of these, the drought of 1997-2003 was the most severe, accounting for the majority of the severity-area-duration envelope of events with areas smaller than 5 million km2. The 1997-2003 drought was also pervasive in terms of both severity and spatial extent. It was also found that soil moisture in north central and northeastern China had significant downward trends, whereas most of Xinjiang, the Tibetan Plateau, and small areas of Yunnan province had significant upward trends. Regions with downward trends were larger than those with upward trends (37% versus 26% of the land area), implying that over the period of analysis, the country has become slightly drier in terms of soil moisture. Trends in drought severity, duration, and frequency suggest that soil moisture droughts have become more severe, prolonged, and frequent during the past 57 yr, especially for northeastern and central China, suggesting an increasing susceptibility to agricultural drought.
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Published date: 1 July 2011
Keywords:
Drought, Ensembles, Hydrology, Land surface model, Soil moisture
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Local EPrints ID: 480870
URI: http://eprints.soton.ac.uk/id/eprint/480870
ISSN: 0894-8755
PURE UUID: 5352b1e5-be48-4b8b-b92c-3fda625ed3e9
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Date deposited: 10 Aug 2023 16:40
Last modified: 17 Mar 2024 03:40
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Author:
Aihui Wang
Author:
Dennis P. Lettenmaier
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