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dc.contributor.authorSun, Jia
dc.contributor.authorHe, Hailun
dc.contributor.authorHu, Xiaomin
dc.contributor.authorWang, Dingqi
dc.contributor.authorGao, Cen
dc.contributor.authorSong, Jinbao
dc.date.accessioned2019-10-05T06:44:40Z
dc.date.available2019-10-05T06:44:40Z
dc.date.copyright6/5/2019 12:00:00 AM
dc.date.issued2019
dc.identifier.otherWAF-D-18-0150.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263286
dc.description.abstractAbstractWe used a mesoscale atmospheric model to simulate Typhoon Hagupit (2008) in the South China Sea (SCS). First, we chose optimized parameterization schemes based on a series of sensitivity tests. The results suggested that a combination of the Kain?Fritsch cumulus scheme and the Goddard microphysics scheme was the best choice for reproducing both the track and intensity of Typhoon Hagupit. Next, the simulated rainfall was compared with microwave remote sensing products. This comparison validated the model results for both the magnitude of rainfall and the location of heavy rain relative to the typhoon?s center. Furthermore, the potential vorticity and vertical wind speed displayed the asymmetric horizontal and tilted vertical structures of Typhoon Hagupit. Finally, we compared the simulation of air?sea turbulent fluxes with estimations from an in situ buoy. The time series of momentum fluxes were roughly consistent, while the model still overestimated heat fluxes, especially right before the typhoon?s arrival at the buoy.
dc.publisherAmerican Meteorological Society
dc.titleNumerical Simulations of Typhoon Hagupit (2008) Using WRF
dc.typeJournal Paper
dc.journal.volume34
dc.journal.issue4
dc.journal.titleWeather and Forecasting
dc.identifier.doi10.1175/WAF-D-18-0150.1
dc.journal.fristpage999
dc.journal.lastpage1015
dc.treeWeather and Forecasting:;2019:;volume 034:;issue 004
dc.contenttypeFulltext


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