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| Type: | Resource | |
| Storage: | The size of this resource is 3.3 MB | |
| Created: | Dec 25, 2020 at 12:20 p.m. (UTC) | |
| Last updated: | Dec 25, 2020 at 1:05 p.m. (UTC) (Metadata update) | |
| Published date: | Dec 25, 2020 at 1:05 p.m. (UTC) | |
| DOI: | 10.4211/hs.48b3fba7ff3f4e379b7fe9a2dfd2cf55 | |
| Citation: | See how to cite this resource | |
| Content types: | Multidimensional Content |
| Sharing Status: | Published |
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| Views: | 2488 |
| Downloads: | 174 |
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Abstract
Using a weakly coupled data assimilation (WCDA) system to constrain the soil moisture and soil temperature in a coupled climate model with a global land data assimilation product, this study demonstrates significant improvements in simulating the interannual variations of EASM rainfall, capturing the notable shift to a "wetter-South-drier-North" rainfall pattern in China in the early 1990s.
Improvements in predicting the EASM rainfall are attributed to the strong land-atmosphere coupling in large areas over China, which allows improved predictions of soil moisture to influence precipitation through soil moisture-precipitation feedback, and the effects of land anomalies on the EASM circulation. This study highlights the significant contribution of land to the interannual predictability of EASM rainfall, with a great potential to advance skillful interannual predictions of benefit to the large populations influenced by the annual whiplash of the summer monsoon rain.
Subject Keywords
Coverage
Spatial
Temporal
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Content
Data Services
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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