2026-09-24T15:05:11Zhttps://univendspace.univen.ac.za/server/oai/request

oai:univendspace.univen.ac.za:11602/14992024-09-10T14:40:58Zcom_11602_1928com_11602_1914com_11602_1897com_11602_737col_11602_2140col_11602_738

Chikoore, H. Bopape, M. M. Nethengwe, N. S. Muofhe, Tshimbiluni Percy 2019 2019-10-22T12:48:42Z 2019-10-22T12:48:42Z 2019-09-20 Muofhe, Tshimbiluni Percy (2019) Characteristics of deep moist convection and rainfall in cut-off lows over South Africa, University of Venda, South Africa.<http://hdl.handle.net/11602/1499>. http://hdl.handle.net/11602/1499 Muofhe TP. Characteristics of deep moist convection and rainfall in cut-off lows over South Africa. []. , 2019 [cited yyyy month dd]. Available from: http://hdl.handle.net/11602/1499 Muofhe, T. P. (2019). <i>Characteristics of deep moist convection and rainfall in cut-off lows over South Africa</i>. (). . Retrieved from http://hdl.handle.net/11602/1499 Muofhe, Tshimbiluni Percy. <i>"Characteristics of deep moist convection and rainfall in cut-off lows over South Africa."</i> ., , 2019. http://hdl.handle.net/11602/1499 TY - Dissertation AU - Muofhe, Tshimbiluni Percy AB - Out of all rain-producing weather systems, cut-off lows (COLs) are linked with the occurrence of high impact rainfall and in some cases short-lived floods which can last for 24 hours over South Africa. This study examined the characteristics associated with the present occurrence of the severe COL systems over South Africa from 2011 to 2017. The accuracy of the 4.4 km Unified Model (UM) which is currently in use for simulating areas of deep moist convection in South Africa was evaluated. The UM simulated geopotential height at 500 hPa as well as the associated 24 hours precipitation which were compared against the daily fields of geopotential height and 6-hourly precipitation from the European Centre for Medium-Range Weather Forecasts (ECMWF). COL events were categorized and analyzed according to the associated surface circulation patterns at 850 hPa. The seasonal distribution and duration of the systems over northern (10°E-33°E //22°-32°S) and southern (10°E-33°E //32°-35°S) regions of the study area were also analyzed. Results show COL systems shifting with season towards the north eastern parts of the country, with an increased number of events during the austral winter season during the study period. Systems which lasted for long time were observed during the austral winter and spring seasons. The UM tends to simulate areas of heavy precipitation accurately with poor simulation during the initial stages of the systems. The UM provided a more realistic-looking closed geopotential height and rainfall fields for systems which are coupled with a cold front at the surface. Application of the knowledge about the evolution in the characteristics of COL events from this study can improve the operational forecasting of these weather systems over the country. DA - 2019-09-20 DB - ResearchSpace DP - Univen KW - Cut-off lows KW - Circulation KW - Deep moist convection KW - Synoptic patterns KW - Simulation LK - https://univendspace.univen.ac.za PY - 2019 T1 - Characteristics of deep moist convection and rainfall in cut-off lows over South Africa TI - Characteristics of deep moist convection and rainfall in cut-off lows over South Africa UR - http://hdl.handle.net/11602/1499 ER - MENVSC Department of Geography and Geo-Information Sciences Out of all rain-producing weather systems, cut-off lows (COLs) are linked with the occurrence of high impact rainfall and in some cases short-lived floods which can last for 24 hours over South Africa. This study examined the characteristics associated with the present occurrence of the severe COL systems over South Africa from 2011 to 2017. The accuracy of the 4.4 km Unified Model (UM) which is currently in use for simulating areas of deep moist convection in South Africa was evaluated. The UM simulated geopotential height at 500 hPa as well as the associated 24 hours precipitation which were compared against the daily fields of geopotential height and 6-hourly precipitation from the European Centre for Medium-Range Weather Forecasts (ECMWF). COL events were categorized and analyzed according to the associated surface circulation patterns at 850 hPa. The seasonal distribution and duration of the systems over northern (10°E-33°E //22°-32°S) and southern (10°E-33°E //32°-35°S) regions of the study area were also analyzed. Results show COL systems shifting with season towards the north eastern parts of the country, with an increased number of events during the austral winter season during the study period. Systems which lasted for long time were observed during the austral winter and spring seasons. The UM tends to simulate areas of heavy precipitation accurately with poor simulation during the initial stages of the systems. The UM provided a more realistic-looking closed geopotential height and rainfall fields for systems which are coupled with a cold front at the surface. Application of the knowledge about the evolution in the characteristics of COL events from this study can improve the operational forecasting of these weather systems over the country. NRF 1 online resource (xiii, 104 leaves : color illustrations, color maps) en University of Venda Cut-off lows Circulation Deep moist convection Synoptic patterns Simulation UCTD 551.5770968 Rain and rainfall -- South Africa Precipitation (Meteorology) -- South Africa Moisture -- South Africa Characteristics of deep moist convection and rainfall in cut-off lows over South Africa Dissertation open.access