New downscaling prediction models for spring drought in China
Abstract Accurate prediction of spring drought in China is helpful toward reducing associated agricultural losses. In this study, spring drought is defined as the three‐month Standardized Precipitation Evapotranspiration Index (SPEI) ending in May. Based on the year‐to‐year increment and downscaling...
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crwiley:10.1002/joc.7623 2024-06-23T07:51:39+00:00 New downscaling prediction models for spring drought in China Tian, Baoqiang Fan, Ke National Natural Science Foundation of China National Key Research and Development Program of China 2022 http://dx.doi.org/10.1002/joc.7623 https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7623 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7623 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7623 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 42, issue 13, page 6960-6975 ISSN 0899-8418 1097-0088 journal-article 2022 crwiley https://doi.org/10.1002/joc.7623 2024-06-06T04:21:00Z Abstract Accurate prediction of spring drought in China is helpful toward reducing associated agricultural losses. In this study, spring drought is defined as the three‐month Standardized Precipitation Evapotranspiration Index (SPEI) ending in May. Based on the year‐to‐year increment and downscaling method, three single‐predictor prediction models (P1 model, P2 model, and P3 model) and two multi‐predictor models for spring drought at 677 stations in China are developed for the period 1983–2020. As physical processes affecting spring drought in the China region, the tropical Pacific–Indian Ocean sea surface temperature (SST) in winter, the Davis Strait–Barents sea‐ice concentration (SIC) in winter, and the 500‐hPa spring vertical velocity, predicted by the Climate Forecast System, version 2 (CFSv2), are considered in the prediction models. The prediction skill of the downscaling models for the spring SPEI is measured by cross‐validation for the period 1983–2020. The CFSv2 model only shows convincing prediction skill for the spring SPEI at 35 of 677 stations. However, among the 677 stations, the temporal correlation coefficient between the observed and predicted spring SPEI at 621 stations for P1 model, 598 stations for P2 model, 545 stations for P3 model, 674 stations for the statistical downscaling model (SD model), and 675 stations for the hybrid downscaling dynamical–statistical prediction model (HD model) exceeds the 95% confidence level. Therefore, compared to the CFSv2 model, the prediction skill for spring drought is improved by the single‐predictor and multi‐predictor models. The prediction skill of HD model for spring drought, which combines preceding observational predictors and the simultaneous predictor of the CFSv2 model, is higher than that of SD model. In addition, the severe drought that occurred in Northeast and North China in spring 2017 can be successfully predicted by HD model. Article in Journal/Newspaper Barents Sea Davis Strait Sea ice Wiley Online Library Barents Sea Indian Pacific International Journal of Climatology 42 13 6960 6975 |
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Wiley Online Library |
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crwiley |
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English |
description |
Abstract Accurate prediction of spring drought in China is helpful toward reducing associated agricultural losses. In this study, spring drought is defined as the three‐month Standardized Precipitation Evapotranspiration Index (SPEI) ending in May. Based on the year‐to‐year increment and downscaling method, three single‐predictor prediction models (P1 model, P2 model, and P3 model) and two multi‐predictor models for spring drought at 677 stations in China are developed for the period 1983–2020. As physical processes affecting spring drought in the China region, the tropical Pacific–Indian Ocean sea surface temperature (SST) in winter, the Davis Strait–Barents sea‐ice concentration (SIC) in winter, and the 500‐hPa spring vertical velocity, predicted by the Climate Forecast System, version 2 (CFSv2), are considered in the prediction models. The prediction skill of the downscaling models for the spring SPEI is measured by cross‐validation for the period 1983–2020. The CFSv2 model only shows convincing prediction skill for the spring SPEI at 35 of 677 stations. However, among the 677 stations, the temporal correlation coefficient between the observed and predicted spring SPEI at 621 stations for P1 model, 598 stations for P2 model, 545 stations for P3 model, 674 stations for the statistical downscaling model (SD model), and 675 stations for the hybrid downscaling dynamical–statistical prediction model (HD model) exceeds the 95% confidence level. Therefore, compared to the CFSv2 model, the prediction skill for spring drought is improved by the single‐predictor and multi‐predictor models. The prediction skill of HD model for spring drought, which combines preceding observational predictors and the simultaneous predictor of the CFSv2 model, is higher than that of SD model. In addition, the severe drought that occurred in Northeast and North China in spring 2017 can be successfully predicted by HD model. |
author2 |
National Natural Science Foundation of China National Key Research and Development Program of China |
format |
Article in Journal/Newspaper |
author |
Tian, Baoqiang Fan, Ke |
spellingShingle |
Tian, Baoqiang Fan, Ke New downscaling prediction models for spring drought in China |
author_facet |
Tian, Baoqiang Fan, Ke |
author_sort |
Tian, Baoqiang |
title |
New downscaling prediction models for spring drought in China |
title_short |
New downscaling prediction models for spring drought in China |
title_full |
New downscaling prediction models for spring drought in China |
title_fullStr |
New downscaling prediction models for spring drought in China |
title_full_unstemmed |
New downscaling prediction models for spring drought in China |
title_sort |
new downscaling prediction models for spring drought in china |
publisher |
Wiley |
publishDate |
2022 |
url |
http://dx.doi.org/10.1002/joc.7623 https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7623 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7623 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7623 |
geographic |
Barents Sea Indian Pacific |
geographic_facet |
Barents Sea Indian Pacific |
genre |
Barents Sea Davis Strait Sea ice |
genre_facet |
Barents Sea Davis Strait Sea ice |
op_source |
International Journal of Climatology volume 42, issue 13, page 6960-6975 ISSN 0899-8418 1097-0088 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/joc.7623 |
container_title |
International Journal of Climatology |
container_volume |
42 |
container_issue |
13 |
container_start_page |
6960 |
op_container_end_page |
6975 |
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1802642763885314048 |