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Heavy rainfall event over Sri Lanka: An assessment with WRF model

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dc.contributor.author Koralegedara, S.B.
dc.contributor.author Lin, Chuan-Yao
dc.contributor.author Sheng, Yang-Fan
dc.date.accessioned 2017-01-06T04:36:19Z
dc.date.available 2017-01-06T04:36:19Z
dc.date.issued 2016
dc.identifier.citation Koralegedara, S.B., Lin, Chuan-Yao and Sheng, Yang-Fan 2016. Heavy rainfall event over Sri Lanka: An assessment with WRF model. In Proceedings of the International Research Symposium on Pure and Applied Sciences (IRSPAS 2016), Faculty of Science, University of Kelaniya, Sri Lanka. p 104. en_US
dc.identifier.isbn 978-955-704-008-0
dc.identifier.uri http://repository.kln.ac.lk/handle/123456789/15759
dc.description.abstract This study used a series of mesoscale cloud-resolving simulations with Weather Research and Forecasting (WRF) Model to reproduce the heavy rainfall and persistent flooding event over Sri Lanka during 14th - 20th May 2016. This major precipitation event, associated with a case of a depression over the Bay of Bengal in the Indian Ocean, originated southeast of Sri Lanka and moved along the east coast of Sri Lanka. This low-pressure system affected most of the country and caused severe flooding and damages particularly in the western part of the Island during this period. Timely availability of an accurate weather forecast can give the lead time for hazards preparedness and minimize potential damages in such situations. Numerical weather prediction with models like WRF is highly utilized for this purpose in many parts of the world. Hence this study aims in finding the ability of the WRF model to reproduce extreme heavy rainfall event and its usefulness in numerical weather prediction in Sri Lanka. The model domain consists of one domain with 9 km grid resolution. Model simulation fields are compared with available daily rainfall data from in-situ weather stations of the Department of Meteorology, Sri Lanka. The WRF model simulated the initiation of the low-pressure system and its development along the east coast of Sri Lanka at nearly the right time. The corresponding precipitation simulation was also reproduced in its spatial distribution aligning with the weather station data, although the overall amount was overestimated. A sensitivity experiment that excludes the orography over the model domain revealed that orographic forcing over the central mountains in Sri Lanka is responsible for about 23% increase in precipitation over the heavy rainfall area in the western Sri Lanka during this event. Moreover, the WRF model able to capture the daily rainfall tendency of this event over Sri Lanka, suggesting it has a potential for operational use in numerical weather prediction in Sri Lanka. en_US
dc.language.iso en en_US
dc.publisher Faculty of Science, University of Kelaniya, Sri Lanka en_US
dc.subject Heavy precipitation en_US
dc.subject WRF model en_US
dc.subject Orographic effect en_US
dc.subject Low-pressure system en_US
dc.title Heavy rainfall event over Sri Lanka: An assessment with WRF model en_US
dc.type Article en_US


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