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Advances towards the development of a cloud-resolving model in South Africa

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dc.contributor.author Bopape, Mary-Jane M
dc.contributor.author Engelbrecht, F
dc.contributor.author Randall, DA
dc.contributor.author Landman, WA
dc.date.accessioned 2014-11-18T09:44:50Z
dc.date.available 2014-11-18T09:44:50Z
dc.date.issued 2014-09
dc.identifier.citation Bopape M-J.M., Engelbrecht, F., Randall, D.A. and Landman, W.A. 2014. Advances towards the development of a cloud-resolving model in South Africa. South African Journal of Science, vol.110(9/10), pp 61-72 en_US
dc.identifier.issn 0038-2353
dc.identifier.uri http://www.sajs.co.za/sites/default/files/publications/pdf/Bopape_Research%20Article.pdf
dc.identifier.uri http://hdl.handle.net/10204/7772
dc.description Copyright: 2014 AOSIS OpenJournals. Published in South African Journal of Science, vol.110(9/10), pp 61-72 en_US
dc.description.abstract Recent advances in supercomputing have made feasible the numerical integration of high-resolution cloud resolving models (CRMs). CRMs are being used increasingly for high-resolution operational numerical weather prediction and for research purposes. We report on the development of a new CRM in South Africa. Two bulk microphysics parameterisation schemes were introduced to a dynamical core of a two-dimensional Non-hydrostatic s-coordinate Model (NSM) developed in South Africa. The resulting CRM was used to simulate two 12-day periods and an 8-day period observed during the Tropical Oceans Global Atmosphere Coupled Ocean-Atmosphere Response Experiment. The response of the NSM to the large-scale forcing which occurred over the three periods, and which included both suppressed and active convection, was examined. The NSM is shown to be able to capture the differences in the three experiments and responds correctly to the large-scale forcing (i.e. it is able to distinguish between suppressed and active regimes). However, the model simulations are cooler and drier than the observations. We demonstrate progress made in the development of a CRM in South Africa, which can be used to study the attributes of convective rainfall over the region. en_US
dc.language.iso en en_US
dc.publisher AOSIS OpenJournals en_US
dc.relation.ispartofseries Workflow;13627
dc.subject Numerical weather prediction en_US
dc.subject Cloud-resolving models en_US
dc.subject Microphysics parameterization en_US
dc.subject Non-hydrostatic models en_US
dc.subject Non-hydrostatic s-coordinate Model en_US
dc.subject Tropical Oceans Global Atmosphere en_US
dc.title Advances towards the development of a cloud-resolving model in South Africa en_US
dc.type Article en_US
dc.identifier.apacitation Bopape, M. M., Engelbrecht, F., Randall, D., & Landman, W. (2014). Advances towards the development of a cloud-resolving model in South Africa. http://hdl.handle.net/10204/7772 en_ZA
dc.identifier.chicagocitation Bopape, Mary-Jane M, F Engelbrecht, DA Randall, and WA Landman "Advances towards the development of a cloud-resolving model in South Africa." (2014) http://hdl.handle.net/10204/7772 en_ZA
dc.identifier.vancouvercitation Bopape MM, Engelbrecht F, Randall D, Landman W. Advances towards the development of a cloud-resolving model in South Africa. 2014; http://hdl.handle.net/10204/7772. en_ZA
dc.identifier.ris TY - Article AU - Bopape, Mary-Jane M AU - Engelbrecht, F AU - Randall, DA AU - Landman, WA AB - Recent advances in supercomputing have made feasible the numerical integration of high-resolution cloud resolving models (CRMs). CRMs are being used increasingly for high-resolution operational numerical weather prediction and for research purposes. We report on the development of a new CRM in South Africa. Two bulk microphysics parameterisation schemes were introduced to a dynamical core of a two-dimensional Non-hydrostatic s-coordinate Model (NSM) developed in South Africa. The resulting CRM was used to simulate two 12-day periods and an 8-day period observed during the Tropical Oceans Global Atmosphere Coupled Ocean-Atmosphere Response Experiment. The response of the NSM to the large-scale forcing which occurred over the three periods, and which included both suppressed and active convection, was examined. The NSM is shown to be able to capture the differences in the three experiments and responds correctly to the large-scale forcing (i.e. it is able to distinguish between suppressed and active regimes). However, the model simulations are cooler and drier than the observations. We demonstrate progress made in the development of a CRM in South Africa, which can be used to study the attributes of convective rainfall over the region. DA - 2014-09 DB - ResearchSpace DP - CSIR KW - Numerical weather prediction KW - Cloud-resolving models KW - Microphysics parameterization KW - Non-hydrostatic models KW - Non-hydrostatic s-coordinate Model KW - Tropical Oceans Global Atmosphere LK - https://researchspace.csir.co.za PY - 2014 SM - 0038-2353 T1 - Advances towards the development of a cloud-resolving model in South Africa TI - Advances towards the development of a cloud-resolving model in South Africa UR - http://hdl.handle.net/10204/7772 ER - en_ZA


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