Numerical Simulation of a Landfall Typhoon Using a Bogus Data Assimilation Scheme
A typhoon bogus data assimilation scheme (BDA) using dimension-reduced projection four-dimensional variational data assimilation (DRP-4-DVar), called DRP-BDA for short, is built in the Advanced Regional Eta Model (AREM). As an adjoint-free approach, DRP- BDA saves time, and only several minutes are...
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description | A typhoon bogus data assimilation scheme (BDA) using dimension-reduced projection four-dimensional variational data assimilation (DRP-4-DVar), called DRP-BDA for short, is built in the Advanced Regional Eta Model (AREM). As an adjoint-free approach, DRP- BDA saves time, and only several minutes are taken for the full BDA process. To evaluate its performance, the DRP-BDA is applied to a case study on a landfall typhoon, Fengshen (2008), from the Northwestern Pacific Ocean to Guangdong province, in which the bogus sea level pressure (SLP) is assimilated as a kind of observation. The results show that a more realistic typhoon with correct center position, stronger warm core vortex, and more reasonable wind fields is reproduced in the analyzed initial condition through the new approach. Compared with the control run (CTRL) initialized with NCEP Final (FNL) Global Tropospheric Analyses, the DRP-BDA leads to an evidently positive impact on typhoon track forecasting and a small positive impact on typhoon intensity forecasting. Furthermore, the forecast landfall time conforms to the observed landfall time, and the forecast track error at the 36thhour is 32 km, which is much less than that of the CTRL (450 km). |
doi_str_mv | 10.1080/16742834.2011.11446936 |
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As an adjoint-free approach, DRP- BDA saves time, and only several minutes are taken for the full BDA process. To evaluate its performance, the DRP-BDA is applied to a case study on a landfall typhoon, Fengshen (2008), from the Northwestern Pacific Ocean to Guangdong province, in which the bogus sea level pressure (SLP) is assimilated as a kind of observation. The results show that a more realistic typhoon with correct center position, stronger warm core vortex, and more reasonable wind fields is reproduced in the analyzed initial condition through the new approach. Compared with the control run (CTRL) initialized with NCEP Final (FNL) Global Tropospheric Analyses, the DRP-BDA leads to an evidently positive impact on typhoon track forecasting and a small positive impact on typhoon intensity forecasting. Furthermore, the forecast landfall time conforms to the observed landfall time, and the forecast track error at the 36thhour is 32 km, which is much less than that of the CTRL (450 km).</description><identifier>ISSN: 1674-2834</identifier><identifier>EISSN: 2376-6123</identifier><identifier>DOI: 10.1080/16742834.2011.11446936</identifier><language>eng</language><publisher>Beijing: Routledge</publisher><subject>BDA ; Data assimilation ; Data collection ; DRP-4-DVar ; Hurricanes ; Sea level ; Sea level pressure ; typhoon ; Typhoons ; Wind fields ; 伪造 ; 台风路径预报 ; 四维变分资料同化 ; 数值模拟 ; 数据同化 ; 登陆台风 ; 登陆时间 ; 经济技术开发区</subject><ispartof>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2011, Vol.4 (4), p.242-246</ispartof><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences 2011</rights><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences. 2011</rights><rights>Copyright © Wanfang Data Co. Ltd. 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As an adjoint-free approach, DRP- BDA saves time, and only several minutes are taken for the full BDA process. To evaluate its performance, the DRP-BDA is applied to a case study on a landfall typhoon, Fengshen (2008), from the Northwestern Pacific Ocean to Guangdong province, in which the bogus sea level pressure (SLP) is assimilated as a kind of observation. The results show that a more realistic typhoon with correct center position, stronger warm core vortex, and more reasonable wind fields is reproduced in the analyzed initial condition through the new approach. Compared with the control run (CTRL) initialized with NCEP Final (FNL) Global Tropospheric Analyses, the DRP-BDA leads to an evidently positive impact on typhoon track forecasting and a small positive impact on typhoon intensity forecasting. Furthermore, the forecast landfall time conforms to the observed landfall time, and the forecast track error at the 36thhour is 32 km, which is much less than that of the CTRL (450 km).</abstract><cop>Beijing</cop><pub>Routledge</pub><doi>10.1080/16742834.2011.11446936</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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subjects | BDA Data assimilation Data collection DRP-4-DVar Hurricanes Sea level Sea level pressure typhoon Typhoons Wind fields 伪造 台风路径预报 四维变分资料同化 数值模拟 数据同化 登陆台风 登陆时间 经济技术开发区 |
title | Numerical Simulation of a Landfall Typhoon Using a Bogus Data Assimilation Scheme |
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