Matches in SemOpenAlex for { <https://semopenalex.org/work/W808518237> ?p ?o ?g. }
- W808518237 abstract "During the past decade, both research and operational numerical weather prediction models [e.g. Weather Research and Forecasting Model (WRF)] have started using more complex microphysical schemes originally developed for high-resolution cloud resolving models (CRMs) with a 1-2 km or less horizontal resolutions. The WRF is a next-generation meso-scale forecast model and assimilation system that has incorporated a modern software framework, advanced dynamics, numeric and data assimilation techniques, a multiple moveable nesting capability, and improved physical packages. The WRF model can be used for a wide range of applications, from idealized research to operational forecasting, with an emphasis on horizontal grid sizes in the range of 1-10 km. The current WRF includes several different microphysics options. At Goddard, four different cloud microphysics schemes (warm rain only, two-class of ice, two three-class of ice with either graupel or hail) are implemented into the WRF. The performances of these schemes have been compared to those from other WRF microphysics scheme options for an Atlantic hurricane case. In addition, a brief review and comparison on the previous modeling studies on the impact of microphysics schemes and microphysical processes on intensity and track of hurricane will be presented. Generally, almost all modeling studies found that the microphysics schemes did not have major impacts on track forecast, but did have more effect on the intensity. All modeling studies found that the simulated hurricane has rapid deepening and/or intensification for the warm rain-only case. It is because all hydrometeors were very large raindrops, and they fell out quickly at and near the eye-wall region. This would hydrostatically produce the lowest pressure. In addition, these modeling studies suggested that the simulated hurricane becomes unrealistically strong by removing the evaporative cooling of cloud droplets and melting of ice particles. This is due to the much weaker downdraft simulated. However, there are many differences between different modeling studies and these differences were identified and discussed." @default.
- W808518237 created "2016-06-24" @default.
- W808518237 creator A5008901665 @default.
- W808518237 creator A5023979531 @default.
- W808518237 creator A5031243260 @default.
- W808518237 creator A5040960941 @default.
- W808518237 creator A5041900190 @default.
- W808518237 creator A5042298797 @default.
- W808518237 creator A5059686151 @default.
- W808518237 creator A5061228061 @default.
- W808518237 date "2010-01-31" @default.
- W808518237 modified "2023-09-22" @default.
- W808518237 title "The Impact of Microphysical Schemes on Intensity and Track of Hurricane" @default.
- W808518237 cites W1481811138 @default.
- W808518237 cites W1548588257 @default.
- W808518237 cites W1909100498 @default.
- W808518237 cites W1916834146 @default.
- W808518237 cites W1968571511 @default.
- W808518237 cites W1968783543 @default.
- W808518237 cites W1969981719 @default.
- W808518237 cites W1981157660 @default.
- W808518237 cites W1989471056 @default.
- W808518237 cites W1999146269 @default.
- W808518237 cites W2009427477 @default.
- W808518237 cites W2015559976 @default.
- W808518237 cites W2019775760 @default.
- W808518237 cites W2021595836 @default.
- W808518237 cites W2028091784 @default.
- W808518237 cites W2029201947 @default.
- W808518237 cites W2034170725 @default.
- W808518237 cites W2038742869 @default.
- W808518237 cites W2039976721 @default.
- W808518237 cites W2049122557 @default.
- W808518237 cites W2052201417 @default.
- W808518237 cites W2055004415 @default.
- W808518237 cites W2055938690 @default.
- W808518237 cites W2063842720 @default.
- W808518237 cites W2065414670 @default.
- W808518237 cites W2075658968 @default.
- W808518237 cites W2077822207 @default.
- W808518237 cites W2083339292 @default.
- W808518237 cites W2085006979 @default.
- W808518237 cites W2086796296 @default.
- W808518237 cites W2092195269 @default.
- W808518237 cites W2094761433 @default.
- W808518237 cites W2096671520 @default.
- W808518237 cites W2100385052 @default.
- W808518237 cites W2103680334 @default.
- W808518237 cites W2109405689 @default.
- W808518237 cites W2111747687 @default.
- W808518237 cites W2112043279 @default.
- W808518237 cites W2115466864 @default.
- W808518237 cites W2119007429 @default.
- W808518237 cites W2121376696 @default.
- W808518237 cites W2123534154 @default.
- W808518237 cites W2128225313 @default.
- W808518237 cites W2128336281 @default.
- W808518237 cites W2129149786 @default.
- W808518237 cites W2136116296 @default.
- W808518237 cites W2138274386 @default.
- W808518237 cites W2138342164 @default.
- W808518237 cites W2140401725 @default.
- W808518237 cites W2143250545 @default.
- W808518237 cites W2162070159 @default.
- W808518237 cites W2170718992 @default.
- W808518237 cites W2171689034 @default.
- W808518237 cites W2172352847 @default.
- W808518237 cites W2173020645 @default.
- W808518237 cites W2173752470 @default.
- W808518237 cites W2178660751 @default.
- W808518237 cites W2178782307 @default.
- W808518237 cites W2179717256 @default.
- W808518237 cites W2179912439 @default.
- W808518237 cites W2210690755 @default.
- W808518237 cites W2295342167 @default.
- W808518237 cites W2495857162 @default.
- W808518237 cites W2562482716 @default.
- W808518237 cites W626077375 @default.
- W808518237 hasPublicationYear "2010" @default.
- W808518237 type Work @default.
- W808518237 sameAs 808518237 @default.
- W808518237 citedByCount "0" @default.
- W808518237 crossrefType "journal-article" @default.
- W808518237 hasAuthorship W808518237A5008901665 @default.
- W808518237 hasAuthorship W808518237A5023979531 @default.
- W808518237 hasAuthorship W808518237A5031243260 @default.
- W808518237 hasAuthorship W808518237A5040960941 @default.
- W808518237 hasAuthorship W808518237A5041900190 @default.
- W808518237 hasAuthorship W808518237A5042298797 @default.
- W808518237 hasAuthorship W808518237A5059686151 @default.
- W808518237 hasAuthorship W808518237A5061228061 @default.
- W808518237 hasConcept C127313418 @default.
- W808518237 hasConcept C133204551 @default.
- W808518237 hasConcept C147947694 @default.
- W808518237 hasConcept C153294291 @default.
- W808518237 hasConcept C197046000 @default.
- W808518237 hasConcept C205649164 @default.
- W808518237 hasConcept C24552861 @default.
- W808518237 hasConcept C29141058 @default.
- W808518237 hasConcept C39432304 @default.