Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa

This study is conducted over the data-poor Limpopo basin centered over southern Africa using reanalysis downscaled to useful resolution. Reanalysis products are of limited value in hydrological applications due to the coarse spatial scales they are available at. Dynamical downscaling of these produc...

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Main Authors: Ditiro B. Moalafhi, Ashish Sharma, Jason P. Evans
Format: Article
Language:English
Published: Elsevier 2017-08-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581817302537
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spelling doaj-a08f736f22b944b39ec02ac80d10e89d2020-11-24T23:47:23ZengElsevierJournal of Hydrology: Regional Studies2214-58182017-08-0112C37839510.1016/j.ejrh.2017.07.001Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern AfricaDitiro B. Moalafhi0Ashish Sharma1Jason P. Evans2Department of Environmental Science, University of Botswana, Gaborone, BotswanaSchool of Civil and Environmental Engineering, University of New South Wales, Sydney, NSW, AustraliaClimate Change Research Centre, University of New South Wales, Sydney, AustraliaThis study is conducted over the data-poor Limpopo basin centered over southern Africa using reanalysis downscaled to useful resolution. Reanalysis products are of limited value in hydrological applications due to the coarse spatial scales they are available at. Dynamical downscaling of these products over a domain of interest offers a means to convert them to finer spatial scales in a dynamically consistent manner. Additionally, this downscaling also offers a way to resolve dominantatmospheric processes, leading to improved accuracy in the atmospheric variables derived. This study thus evaluates high-resolution downscaling of an objectively chosen reanalysis (ERA-I) over the Limpopo basin using Weather Research and Forecasting (WRF) as a regional climate model. The model generally under-estimates temperature and over-estimates precipitation over the basin, although reasonably consistent with observations. The model does well in simulating observed sustained hydrological extremes as assessed using the Standardized Precipitation Index (SPI) although it consistently under-estimates the severity ofmoisture deficit for the wettest part of the year during the dry years. The basin's aridity index (I) is above the severe drought threshold during summer and is more severe in autumn. This practically restricts rain-fed agriculture to around 3 months in a year over the basin. This study presents possible beneficial use of the downscaled simulations foroptimal hydrologic design and water resources planning in data scarce parts of the world.http://www.sciencedirect.com/science/article/pii/S2214581817302537ReanalysesDynamical downscalingHydrological applicationsLimpopo basinSouthern Africa
collection DOAJ
language English
format Article
sources DOAJ
author Ditiro B. Moalafhi
Ashish Sharma
Jason P. Evans
spellingShingle Ditiro B. Moalafhi
Ashish Sharma
Jason P. Evans
Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
Journal of Hydrology: Regional Studies
Reanalyses
Dynamical downscaling
Hydrological applications
Limpopo basin
Southern Africa
author_facet Ditiro B. Moalafhi
Ashish Sharma
Jason P. Evans
author_sort Ditiro B. Moalafhi
title Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
title_short Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
title_full Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
title_fullStr Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
title_full_unstemmed Reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – Application to the Limpopo catchment in southern Africa
title_sort reconstructing hydro-climatological data using dynamical downscaling of reanalysis products in data-sparse regions – application to the limpopo catchment in southern africa
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2017-08-01
description This study is conducted over the data-poor Limpopo basin centered over southern Africa using reanalysis downscaled to useful resolution. Reanalysis products are of limited value in hydrological applications due to the coarse spatial scales they are available at. Dynamical downscaling of these products over a domain of interest offers a means to convert them to finer spatial scales in a dynamically consistent manner. Additionally, this downscaling also offers a way to resolve dominantatmospheric processes, leading to improved accuracy in the atmospheric variables derived. This study thus evaluates high-resolution downscaling of an objectively chosen reanalysis (ERA-I) over the Limpopo basin using Weather Research and Forecasting (WRF) as a regional climate model. The model generally under-estimates temperature and over-estimates precipitation over the basin, although reasonably consistent with observations. The model does well in simulating observed sustained hydrological extremes as assessed using the Standardized Precipitation Index (SPI) although it consistently under-estimates the severity ofmoisture deficit for the wettest part of the year during the dry years. The basin's aridity index (I) is above the severe drought threshold during summer and is more severe in autumn. This practically restricts rain-fed agriculture to around 3 months in a year over the basin. This study presents possible beneficial use of the downscaled simulations foroptimal hydrologic design and water resources planning in data scarce parts of the world.
topic Reanalyses
Dynamical downscaling
Hydrological applications
Limpopo basin
Southern Africa
url http://www.sciencedirect.com/science/article/pii/S2214581817302537
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