A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall

Rainfall data at fine spatial resolutions are often required for various studies in hydrology and water resources. However, such data are not widely available, as their collection is normally expensive and time-consuming. A common practice to obtain fine-spatial-resolution rainfall data is to employ...

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Main Authors: Bellie Sivakumar, Fitsum M. Woldemeskel, Rajendran Vignesh, Vinayakam Jothiprakash
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/6/1/11
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author Bellie Sivakumar
Fitsum M. Woldemeskel
Rajendran Vignesh
Vinayakam Jothiprakash
author_facet Bellie Sivakumar
Fitsum M. Woldemeskel
Rajendran Vignesh
Vinayakam Jothiprakash
author_sort Bellie Sivakumar
collection DOAJ
description Rainfall data at fine spatial resolutions are often required for various studies in hydrology and water resources. However, such data are not widely available, as their collection is normally expensive and time-consuming. A common practice to obtain fine-spatial-resolution rainfall data is to employ interpolation schemes to derive them based on data available at nearby locations. Such interpolation schemes are generally based on rainfall correlation or distance between stations. The present study proposes a combined rainfall correlation-spatial scale-correlation threshold method for representing spatial rainfall variability. The method is applied to monthly rainfall data at a resolution of 0.25 × 0.25 latitude/longitude across Australia, available from the Tropical Rainfall Measuring Mission (TRMM 3B43 version). The results indicate that rainfall dynamics in northern and northeastern Australia have far greater spatial correlations when compared to the other regions, especially in southern and southeastern Australia, suggesting that tropical climates generally have greater spatial rainfall correlations when compared to temperate, oceanic, and continental climates, subject to other influencing factors. The implications of the outcomes for rainfall data interpolation and the rain gauge monitoring network are also discussed, especially based on results obtained for ten major cities in Australia.
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spelling doaj.art-b7e148ef0c174333b475c424e2d6bc022022-12-22T02:59:44ZengMDPI AGHydrology2306-53382019-01-01611110.3390/hydrology6010011hydrology6010011A Correlation–Scale–Threshold Method for Spatial Variability of RainfallBellie Sivakumar0Fitsum M. Woldemeskel1Rajendran Vignesh2Vinayakam Jothiprakash3UNSW Water Research Centre, School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, AustraliaSchool of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, AustraliaVel Tech Rangarajan Dr. Sagunthala R & D Institute of Science and Technology, Avadi, Chennai 600 062, Tamil Nadu, IndiaDepartment of Civil Engineering, Indian Institute of Technology Bombay, Powai, Mumbai 400 076, Maharashtra, IndiaRainfall data at fine spatial resolutions are often required for various studies in hydrology and water resources. However, such data are not widely available, as their collection is normally expensive and time-consuming. A common practice to obtain fine-spatial-resolution rainfall data is to employ interpolation schemes to derive them based on data available at nearby locations. Such interpolation schemes are generally based on rainfall correlation or distance between stations. The present study proposes a combined rainfall correlation-spatial scale-correlation threshold method for representing spatial rainfall variability. The method is applied to monthly rainfall data at a resolution of 0.25 × 0.25 latitude/longitude across Australia, available from the Tropical Rainfall Measuring Mission (TRMM 3B43 version). The results indicate that rainfall dynamics in northern and northeastern Australia have far greater spatial correlations when compared to the other regions, especially in southern and southeastern Australia, suggesting that tropical climates generally have greater spatial rainfall correlations when compared to temperate, oceanic, and continental climates, subject to other influencing factors. The implications of the outcomes for rainfall data interpolation and the rain gauge monitoring network are also discussed, especially based on results obtained for ten major cities in Australia.https://www.mdpi.com/2306-5338/6/1/11rainfallspatial variabilitycorrelationscalethresholdAustralia
spellingShingle Bellie Sivakumar
Fitsum M. Woldemeskel
Rajendran Vignesh
Vinayakam Jothiprakash
A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
Hydrology
rainfall
spatial variability
correlation
scale
threshold
Australia
title A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
title_full A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
title_fullStr A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
title_full_unstemmed A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
title_short A Correlation–Scale–Threshold Method for Spatial Variability of Rainfall
title_sort correlation scale threshold method for spatial variability of rainfall
topic rainfall
spatial variability
correlation
scale
threshold
Australia
url https://www.mdpi.com/2306-5338/6/1/11
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