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Lee, Myong-In
Climate-Environment Modeling Lab
Research Interests
  • Climate Change, Seasonal Prediction, Extreme Weather, Aerosol

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Improved representation of the diurnal variation of warm season precipitation by an atmospheric general circulation model at a 10 km horizontal resolution

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dc.contributor.author Kim, Hyerim ko
dc.contributor.author Lee, Myong-In ko
dc.contributor.author Cha, Dong-Hyun ko
dc.contributor.author Lim, Young-Kwon ko
dc.contributor.author Putman, William M. ko
dc.date.available 2019-09-19T08:56:53Z -
dc.date.created 2019-09-16 ko
dc.date.issued 2019-12 ko
dc.identifier.citation CLIMATE DYNAMICS, v.53, no.11, pp.6523 - 6542 ko
dc.identifier.issn 0930-7575 ko
dc.identifier.uri https://scholarworks.unist.ac.kr/handle/201301/27459 -
dc.description.abstract This study investigates the diurnal variation of the warm season precipitation simulated by the Goddard Earth Observing System version 5 atmospheric general circulation model for 2 years (2005–2006) at a horizontal resolution of 10 km. The simulation was validated with the satellite-derived Tropical Rainfall Measuring Mission (TRMM) 3B42 precipitation data and the Modern-Era Retrospective analysis for Research and Applications atmospheric reanalysis for atmospheric winds and moisture. The simulation is compared with the coarse-resolution run in 50 km to examine the impacts driven by resolution change. Overall, the 10 km model tends to reproduce the important features of the observed diurnal variation, such as the amplitude and phase at which precipitation peaks in the evening on land and in the morning over the ocean, despite an excessive amplitude bias over land. The model also reproduces the realistic propagation patterns of precipitation in the vicinity of ocean coasts and major mountains. The regional characteristics of the diurnal precipitation over two regions, the Bay of Bengal and the Great Plains in North America, are examined in detail, where the observed diurnal cycle exhibits a systematic transition in the peak phase due to the development and propagation of regional-scale convective systems. The model is able to reproduce this pattern as well as the diurnal variation of low-level wind and moisture convergence; however, it is less effective at representing the nocturnal peak of precipitation over the Great Plains. The model results suggest that increasing the horizontal resolution of the model to 10 km substantially improves the representation of the diurnal precipitation cycle. However, intrinsic model deficiencies in topographical precipitation and the accurate representation of mesoscale convective systems remain a challenge. ko
dc.language 영어 ko
dc.publisher Springer Verlag ko
dc.title Improved representation of the diurnal variation of warm season precipitation by an atmospheric general circulation model at a 10 km horizontal resolution ko
dc.type ARTICLE ko
dc.identifier.scopusid 2-s2.0-85071283267 ko
dc.identifier.wosid 000494681900001 ko
dc.type.rims ART ko
dc.identifier.doi 10.1007/s00382-019-04943-6 ko
dc.identifier.url https://link.springer.com/article/10.1007%2Fs00382-019-04943-6 ko
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