Synoptic circulation patterns and atmospheric variables associated with significant snowfall over South Africa in winter

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dc.contributor.advisor Dyson, Liesl L.
dc.contributor.postgraduate Stander, Jan Hendrik
dc.date.accessioned 2013-10-01T08:25:54Z
dc.date.available 2013-10-01T08:25:54Z
dc.date.created 2013-09-06
dc.date.issued 2013-10-01
dc.description Dissertation (MSc)--University of Pretoria, 2013. en_US
dc.description.abstract South Africa is located in the sub tropics with an elevated plateau which is located approximately 1500 m above mean sea level (a.m.s.l). Every year, snow occurs on the mountains of Lesotho, but on occasions this snow descends to lower elevations which impacts on the livelihood of people. Severe weather originating from extra-tropical weather systems has been well documented in South Africa and yet very little research has been done to predict significant snowfall from these weather systems. The main aim of this research is to identify those weather systems responsible for snow and to understand the processes causing snow to form when these systems occur. A comprehensive database of significant snowfall events is supplied from 1981 to 2011. The database is subjectively classified into characteristic synoptic patterns. The snow cases are then objectively classified using self-organising maps (SOMs) to obtain synoptic configurations most typically associated with significant snowfall over South Africa. Case studies which aim to explain the synoptic conditions, formation mechanisms as well as critical surface temperature and relative humidity during snowfall events are described. This is done by analysing each case study with respect to synoptic circulations, surface observations, atmospheric soundings, satellite imagery as well as atmospheric thickness. Conclusions are drawn and critical threshold values of atmospheric thickness, surface temperature and humidity are identified when snowfall occurs. A methodical snow forecasting decision tree is devised. It takes the synoptic classification of circulation patterns during significant snowfall, atmospheric thickness, height of the freezing level, surface temperature, and relative humidity into account. This process is explained by case studies. It is recommended that results from this dissertation are made available to weather forecasters in South Africa and that the results are implemented in the operational forecasting environment. Further case study investigations are suggested, taking the mesoscale processes effects into account. en_US
dc.description.availability Unrestricted en_US
dc.description.degree MSc
dc.description.department Geography, Geoinformatics and Meteorology en_US
dc.description.librarian am2013 en_US
dc.identifier.citation Stander, JH 2013-10-01, Synoptic circulation patterns and atmospheric variables associated with significant snowfall over South Africa in winter, MSc Dissertation, University of Pretoria, Pretoria, viewed yymmdd <http://hdl.handle.net/2263/31860> en_US
dc.identifier.other D/13/9/897 en_US
dc.identifier.uri http://hdl.handle.net/2263/31860
dc.language.iso en en_US
dc.publisher University of Pretoria en_ZA
dc.rights © 2013 University of Pretoria. All rights reserved. The copyright in this work vests in the University of Pretoria. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of the University of Pretoria. en_US
dc.subject Winter, South Africa en_US
dc.subject Mountains of Lesotho en_US
dc.subject Humidity during snow en_US
dc.subject Snowfall en_US
dc.subject Weather sytems en_US
dc.subject UCTD
dc.title Synoptic circulation patterns and atmospheric variables associated with significant snowfall over South Africa in winter en_US
dc.type Dissertation en_US


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