<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-26T03:31:48Z</responseDate><request verb="GetRecord" identifier="oai:univendspace.univen.ac.za:11602/1495" metadataPrefix="dim">https://univendspace.univen.ac.za/server/oai/request</request><GetRecord><record><header><identifier>oai:univendspace.univen.ac.za:11602/1495</identifier><datestamp>2024-09-10T14:23:50Z</datestamp><setSpec>com_11602_1928</setSpec><setSpec>com_11602_1914</setSpec><setSpec>com_11602_1897</setSpec><setSpec>com_11602_737</setSpec><setSpec>col_11602_2140</setSpec><setSpec>col_11602_738</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="advisor"/>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Chikoore, H.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Bopape, M. M.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Nethengwe, N. S.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Dlamini, Nohlahla</dim:field>
   <dim:field mdschema="dc" element="date">2019</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2019-10-22T10:36:57Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="available">2019-10-22T10:36:57Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued">2019</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="citation">Dlamini, Nohlahla (2019) Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM), University of Venda, South Africa.&amp;lt;http://hdl.handle.net/11602/1495&amp;gt;.</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">http://hdl.handle.net/11602/1495</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="vancouvercitation" lang="en_ZA">Dlamini N. Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM). []. , 2019 [cited yyyy month dd]. Available from: http://hdl.handle.net/11602/1495</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="apacitation" lang="en_ZA">Dlamini, N. (2019). &amp;lt;i&amp;gt;Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM)&amp;lt;/i&amp;gt;. (). . Retrieved from http://hdl.handle.net/11602/1495</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="chicagocitation" lang="en_ZA">Dlamini, Nohlahla. &amp;lt;i&amp;gt;&amp;quot;Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM).&amp;quot;&amp;lt;/i&amp;gt; ., , 2019. http://hdl.handle.net/11602/1495</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="ris" lang="en_ZA">&#xd;
TY  - Dissertation&#xd;
AU  - Dlamini, Nohlahla&#xd;
AB  - The process of cloud formation and distribution in the atmospheric circulation system is very&#xd;
important yet not easy to comprehend and forecast. Clouds affect the climate system by&#xd;
controlling the amount of solar radiation, precipitation and other climatic variables. Parameterised&#xd;
induced General Circulation Model (GCMs) are unable to represent clouds and aerosol particles&#xd;
explicitly and their influence on the climate and are thought to be responsible for most of the&#xd;
uncertainty in climate predictions. Therefore, the aim of the study is to investigate the climate of&#xd;
South Africa as simulated by Super Parameterised Community Atmosphere Model (SPCAM) for&#xd;
the period of 1987-2016. Community Atmosphere Model (CAM) and SPCAM datasets used in the&#xd;
study were obtained from Colorado State University (CSU), whilst dynamic and thermodynamic&#xd;
fields were obtained from the NCEP reanalysis ll. The simulations were compared against rainfall&#xd;
and temperature observations obtained from the South African Weather Service (SAWS)&#xd;
database. The accuracy of the model output from CAM and SPCAM was tested in simulating&#xd;
rainfall and temperature at seasonal timescales using the Root Mean Square Error (RMSE). It&#xd;
was found that CAM overestimates rainfall over the interior of the subcontinent during December&#xd;
- February (DJF) season whilst SPCAM showed a high performance in depicting summer rainfall&#xd;
particularly in the central and eastern parts of South Africa. During June – August (JJA), both&#xd;
configurations (CAM and SPCAM) had a dry bias with simulating winter rainfall over the south&#xd;
Western Cape region in cases of little rainfall in the observations. CAM was also found to&#xd;
underestimate temperatures during DJF with SPCAM results closer to the reanalysis. The study&#xd;
further analyzed inter-annual variability of rainfall and temperature for different homogenous&#xd;
regions across the whole of South Africa using both configurations. It was found that SPCAM had&#xd;
a higher skill than CAM in simulating inter-annual variability of rainfall and temperature over the&#xd;
summer rainfall regions of South Africa for the period of 1987 to 2016. SPCAM also showed&#xd;
reasonable skill simulating (mean sea level pressure, geopotential height, omega etc) in contrast&#xd;
to the standard CAM for all seasons at the low and middle levels (850 hPa and 500 hPa). The&#xd;
study also focused on major El Niño Southern Oscillation (ENSO) events and found that SPCAM&#xd;
tended to compare better in general with the observations. Although both versions of the model&#xd;
still feature substantial biases in simulating South African climate variables (rainfall, temperature,&#xd;
etc), the magnitude of the biases are generally smaller in the super parameterized CAM than the&#xd;
default CAM, suggesting that the implementation of the super parameterization in CAM improves&#xd;
the model performance and therefore seasonal climate prediction.&#xd;
DA  - 2019&#xd;
DB  - ResearchSpace&#xd;
DP  - Univen&#xd;
KW  - Clouds&#xd;
KW  - Climate&#xd;
KW  - Super Parameterised Community Atmosphere Model (CAM) El Nino.&#xd;
LK  - https://univendspace.univen.ac.za&#xd;
PY  - 2019&#xd;
T1  - Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM)&#xd;
TI  - Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM)&#xd;
UR  - http://hdl.handle.net/11602/1495&#xd;
ER  - &#xd;
</dim:field>
   <dim:field mdschema="dc" element="description" lang="en_US">MENVSC</dim:field>
   <dim:field mdschema="dc" element="description">Department of Geography and Geo-Information Sciences</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract" lang="en_US">The process of cloud formation and distribution in the atmospheric circulation system is very&#xd;
important yet not easy to comprehend and forecast. Clouds affect the climate system by&#xd;
controlling the amount of solar radiation, precipitation and other climatic variables. Parameterised&#xd;
induced General Circulation Model (GCMs) are unable to represent clouds and aerosol particles&#xd;
explicitly and their influence on the climate and are thought to be responsible for most of the&#xd;
uncertainty in climate predictions. Therefore, the aim of the study is to investigate the climate of&#xd;
South Africa as simulated by Super Parameterised Community Atmosphere Model (SPCAM) for&#xd;
the period of 1987-2016. Community Atmosphere Model (CAM) and SPCAM datasets used in the&#xd;
study were obtained from Colorado State University (CSU), whilst dynamic and thermodynamic&#xd;
fields were obtained from the NCEP reanalysis ll. The simulations were compared against rainfall&#xd;
and temperature observations obtained from the South African Weather Service (SAWS)&#xd;
database. The accuracy of the model output from CAM and SPCAM was tested in simulating&#xd;
rainfall and temperature at seasonal timescales using the Root Mean Square Error (RMSE). It&#xd;
was found that CAM overestimates rainfall over the interior of the subcontinent during December&#xd;
- February (DJF) season whilst SPCAM showed a high performance in depicting summer rainfall&#xd;
particularly in the central and eastern parts of South Africa. During June – August (JJA), both&#xd;
configurations (CAM and SPCAM) had a dry bias with simulating winter rainfall over the south&#xd;
Western Cape region in cases of little rainfall in the observations. CAM was also found to&#xd;
underestimate temperatures during DJF with SPCAM results closer to the reanalysis. The study&#xd;
further analyzed inter-annual variability of rainfall and temperature for different homogenous&#xd;
regions across the whole of South Africa using both configurations. It was found that SPCAM had&#xd;
a higher skill than CAM in simulating inter-annual variability of rainfall and temperature over the&#xd;
summer rainfall regions of South Africa for the period of 1987 to 2016. SPCAM also showed&#xd;
reasonable skill simulating (mean sea level pressure, geopotential height, omega etc) in contrast&#xd;
to the standard CAM for all seasons at the low and middle levels (850 hPa and 500 hPa). The&#xd;
study also focused on major El Niño Southern Oscillation (ENSO) events and found that SPCAM&#xd;
tended to compare better in general with the observations. Although both versions of the model&#xd;
still feature substantial biases in simulating South African climate variables (rainfall, temperature,&#xd;
etc), the magnitude of the biases are generally smaller in the super parameterized CAM than the&#xd;
default CAM, suggesting that the implementation of the super parameterization in CAM improves&#xd;
the model performance and therefore seasonal climate prediction.</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="sponsorship" lang="en_US">NRF</dim:field>
   <dim:field mdschema="dc" element="format" qualifier="extent">1 online resources (xviii, 110 leaves :color illustrations, color maps)</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso" lang="en_US">en</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Clouds</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Climate</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Super Parameterised Community Atmosphere Model (CAM) El Nino.</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_ZA">UCTD</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="ddc">551.6968</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Clouds -- South Africa</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Climate changes -- South Africa</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Weather</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Temperature</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Climatology</dim:field>
   <dim:field mdschema="dc" element="title" lang="en_US">Simulating South African Climate with a Super parameterized Community Atmosphere Model (SP-CAM)</dim:field>
   <dim:field mdschema="dc" element="type" lang="en_US">Dissertation</dim:field>
   <dim:field mdschema="others" element="access-status">open.access</dim:field>
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