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Role of thermal and dynamical subdaily perturbations over the Tibetan Plateau in 30-day extended-range forecast of East Asian precipitation in early summer
The influence of the thermodynamic forcing of the Tibetan Plateau (TP) on the Asian summer monsoon remains controversial because the role of elevated heating across the TP remains unclear at multiple time scales. At the extended-range scale, the boundary forcing is more important than the initial fi...
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Published in: | NPJ climate and atmospheric science 2025-02, Vol.8 (1), p.40-15, Article 40 |
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description | The influence of the thermodynamic forcing of the Tibetan Plateau (TP) on the Asian summer monsoon remains controversial because the role of elevated heating across the TP remains unclear at multiple time scales. At the extended-range scale, the boundary forcing is more important than the initial field in the forecast process. In this study, we investigated the role of subdaily thermodynamic forcing across the TP in generating 30-day predictions of precipitation in East Asia by conducting a series of hindcast experiments. The surface potential vorticity forcing was used to identify typical years when the TP forcings were extremely strong or weak. The results indicated that the subdaily thermal forcing of the TP was very important for improving the East Asian precipitation forecast accuracy, especially for predictions longer than 14 days in June 2022, when diffusion heating is very strong and can develop over the TP. In such a case, the corrected TP heating could not only correct for low-level water vapor transport but also modular uplevel circulation, which could propagate downstream, thus favoring the correct prediction of precipitation over East Asia. However, in the other cases, the individual influences of thermal perturbations across the TP are not the only important factors. These findings reveal ways to improve the extended-range forecast skill over East Asia. |
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At the extended-range scale, the boundary forcing is more important than the initial field in the forecast process. In this study, we investigated the role of subdaily thermodynamic forcing across the TP in generating 30-day predictions of precipitation in East Asia by conducting a series of hindcast experiments. The surface potential vorticity forcing was used to identify typical years when the TP forcings were extremely strong or weak. The results indicated that the subdaily thermal forcing of the TP was very important for improving the East Asian precipitation forecast accuracy, especially for predictions longer than 14 days in June 2022, when diffusion heating is very strong and can develop over the TP. In such a case, the corrected TP heating could not only correct for low-level water vapor transport but also modular uplevel circulation, which could propagate downstream, thus favoring the correct prediction of precipitation over East Asia. However, in the other cases, the individual influences of thermal perturbations across the TP are not the only important factors. 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At the extended-range scale, the boundary forcing is more important than the initial field in the forecast process. In this study, we investigated the role of subdaily thermodynamic forcing across the TP in generating 30-day predictions of precipitation in East Asia by conducting a series of hindcast experiments. The surface potential vorticity forcing was used to identify typical years when the TP forcings were extremely strong or weak. The results indicated that the subdaily thermal forcing of the TP was very important for improving the East Asian precipitation forecast accuracy, especially for predictions longer than 14 days in June 2022, when diffusion heating is very strong and can develop over the TP. In such a case, the corrected TP heating could not only correct for low-level water vapor transport but also modular uplevel circulation, which could propagate downstream, thus favoring the correct prediction of precipitation over East Asia. However, in the other cases, the individual influences of thermal perturbations across the TP are not the only important factors. 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He, Xinyu ; Liu, Yimin ; Wu, Guoxiong ; Bao, Qing ; Hu, Wenting ; Sheng, Chen ; Feng, Shijian</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2611-d4370b9ad596247f0b2d3c353b539ad33ed94a5535281b0d94238274c74de2843</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2025</creationdate><topic>704/106/35</topic><topic>704/106/694/1108</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Atmospheric Sciences</topic><topic>Climate Change/Climate Change Impacts</topic><topic>Climatology</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Experiments</topic><topic>Extreme values</topic><topic>Heat</topic><topic>Heat transmission</topic><topic>Heating</topic><topic>Influence</topic><topic>Monsoons</topic><topic>Perturbation</topic><topic>Precipitation</topic><topic>Predictions</topic><topic>Summer</topic><topic>Thermodynamics</topic><topic>Topography</topic><topic>Vorticity</topic><topic>Water vapor</topic><topic>Weather forecasting</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>He, Bian</creatorcontrib><creatorcontrib>He, Xinyu</creatorcontrib><creatorcontrib>Liu, Yimin</creatorcontrib><creatorcontrib>Wu, Guoxiong</creatorcontrib><creatorcontrib>Bao, Qing</creatorcontrib><creatorcontrib>Hu, Wenting</creatorcontrib><creatorcontrib>Sheng, Chen</creatorcontrib><creatorcontrib>Feng, Shijian</creatorcontrib><collection>Springer_OA刊</collection><collection>CrossRef</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Agriculture & Environmental Science Database</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Earth, Atmospheric & Aquatic Science</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Middle East (New)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><collection>Directory of Open Access Journals</collection><jtitle>NPJ climate and atmospheric science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>He, Bian</au><au>He, Xinyu</au><au>Liu, Yimin</au><au>Wu, Guoxiong</au><au>Bao, Qing</au><au>Hu, Wenting</au><au>Sheng, Chen</au><au>Feng, Shijian</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Role of thermal and dynamical subdaily perturbations over the Tibetan Plateau in 30-day extended-range forecast of East Asian precipitation in early summer</atitle><jtitle>NPJ climate and atmospheric science</jtitle><stitle>npj Clim Atmos Sci</stitle><date>2025-02-05</date><risdate>2025</risdate><volume>8</volume><issue>1</issue><spage>40</spage><epage>15</epage><pages>40-15</pages><artnum>40</artnum><issn>2397-3722</issn><eissn>2397-3722</eissn><abstract>The influence of the thermodynamic forcing of the Tibetan Plateau (TP) on the Asian summer monsoon remains controversial because the role of elevated heating across the TP remains unclear at multiple time scales. At the extended-range scale, the boundary forcing is more important than the initial field in the forecast process. In this study, we investigated the role of subdaily thermodynamic forcing across the TP in generating 30-day predictions of precipitation in East Asia by conducting a series of hindcast experiments. The surface potential vorticity forcing was used to identify typical years when the TP forcings were extremely strong or weak. The results indicated that the subdaily thermal forcing of the TP was very important for improving the East Asian precipitation forecast accuracy, especially for predictions longer than 14 days in June 2022, when diffusion heating is very strong and can develop over the TP. In such a case, the corrected TP heating could not only correct for low-level water vapor transport but also modular uplevel circulation, which could propagate downstream, thus favoring the correct prediction of precipitation over East Asia. However, in the other cases, the individual influences of thermal perturbations across the TP are not the only important factors. These findings reveal ways to improve the extended-range forecast skill over East Asia.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/s41612-025-00931-2</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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subjects | 704/106/35 704/106/694/1108 Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Climate Change/Climate Change Impacts Climatology Earth and Environmental Science Earth Sciences Experiments Extreme values Heat Heat transmission Heating Influence Monsoons Perturbation Precipitation Predictions Summer Thermodynamics Topography Vorticity Water vapor Weather forecasting Wind |
title | Role of thermal and dynamical subdaily perturbations over the Tibetan Plateau in 30-day extended-range forecast of East Asian precipitation in early summer |
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