Phesheya Dlamini

Prof. Phesheya Dlamini

orcid

Research Focus & Metrics

Academic Career Length

17Years (2010-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 April 2016 in Agriculture, Ecosystems & Environment
Verified
Journal Article
Closed access
PDPhesheya Dlamini
Phesheya Dlamini
PCPauline Chivenge
Pauline Chivenge
VCVincent Chaplot
Vincent Chaplot

1 December 2014 in Geoderma
Verified
Journal Article
Closed access
PDPhesheya Dlamini
Phesheya Dlamini
PCPauline Chivenge
Pauline Chivenge
AMAlan Manson
Alan Manson
VCVincent Chaplot
Vincent Chaplot

1 September 2011 in Agricultural Water Management
Verified
Journal Article
Closed access
PDPhesheya Dlamini
Phesheya Dlamini
COC. Orchard
C. Orchard
GJG. Jewitt
G. Jewitt
SLS. Lorentz
S. Lorentz
LTL. Titshall
L. Titshall
VCVincent Chaplot
Vincent Chaplot

1 March 2010 in Geoderma
Verified
Journal Article
Closed access
KPK. Phachomphon
K. Phachomphon
PDPhesheya Dlamini
Phesheya Dlamini
VCVincent Chaplot
Vincent Chaplot

1 June 2016 in Geoderma
Verified
Journal Article
Closed access
VCVincent Chaplot
Vincent Chaplot
PDPhesheya Dlamini
Phesheya Dlamini
PCPauline Chivenge
Pauline Chivenge

1 January 2017 in Climate Risk Management
Verified
Journal Article
Open access
CTC.M. Tfwala
C.M. Tfwala
LRL.D. van Rensburg
L.D. van Rensburg
RSR. Schall
R. Schall
SMS.M. Mosia
S.M. Mosia
PDPhesheya Dlamini
Phesheya Dlamini
Engineering infrastructures such as stormwater drains and bridges are commonly designed using the concept of Intensity-Duration-Frequency (IDF) curves, which assume that the occurrence of precipitation patterns and distributions are spatially similar within the drainage area and remain unchanged throughout the lifespan of the infrastructures (stationary). Based on the premise that climate change will alter the spatial and temporal variability of precipitation patterns, inaccuracy in the estimation of IDF curves may occur. As such, prior to developing IDF curves, it is crucial to analyse trends of annual precipitation maxima. The objective of this study was to estimate the precipitation intensities and their uncertainties (lower and upper limits) for durations of 0.125, 0.25, 0.5, 1, 2, 4, and 6 h and return periods of 2, 10, 25, 50 and 100 years in the Ghaap plateau, Northern Cape Province, South Africa using the Generalized Extreme Value (GEV) distribution. The annual precipitation maxima were extracted from long-term (1918–2014) precipitation data for four meteorological stations (Postmasburg, Douglas, Kuruman and Groblershoop) sourced from the South African Weather Services (SAWS). On average, the estimated extreme precipitation intensities for the plateau ranged from 4.2 mm/h for 6 h storm duration to 55.8 mm/h for 0.125 h at 2 years return period. At 100 year return period, the intensity ranged from 13.3 mm/h for 6 h duration to 175.5 mm/h for the duration of 0.125 h. The lower limit of uncertainty ranged from 11.7% at 2 years return period to 26% at 100 year return period, and from 12.8% to 58.4% for the upper limit for the respective return periods. This methodology can be integrated into policy formulation for the design of stormwater and flood management infrastructures in the Ghaap plateau, where mining is the main economic activity