Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century

Tropical countries are already experiencing the adverse impacts of climate change. This study presents projections of climate change-driven variations in hydrology and sediment loads in the Kalu River Basin, Sri Lanka. Bias-corrected climate projections (i.e., precipitation and temperature) from thr...

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Autores principales: T.A.J.G. Sirisena, Shreedhar Maskey, Janaka Bamunawala, Erika Coppola, Roshanka Ranasinghe
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/be0e1c9003b74aed9188f723b1250f38
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spelling oai:doaj.org-article:be0e1c9003b74aed9188f723b1250f382021-11-11T19:55:13ZProjected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century10.3390/w132130312073-4441https://doaj.org/article/be0e1c9003b74aed9188f723b1250f382021-10-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3031https://doaj.org/toc/2073-4441Tropical countries are already experiencing the adverse impacts of climate change. This study presents projections of climate change-driven variations in hydrology and sediment loads in the Kalu River Basin, Sri Lanka. Bias-corrected climate projections (i.e., precipitation and temperature) from three high resolution (25 km) regional climate models (viz., RegCM4-MIROC5, MPI-M-MPI-ESM-MR, and NCC-NORESM1-M) are used here to force a calibrated hydrological model to project streamflow and sediment loads for two future periods (mid-century: 2046–2065, and end of the century: 2081–2099) under two representative concentration pathways (i.e., RCPs 2.6 and 8.5). By the end of the century under RCP 8.5, all simulations (forced with the three RCMs) project increased annual streamflow (67–87%) and sediment loads (128–145%). In general, streamflow and sediment loads are projected to increase more during the southwest monsoon season (May–September) than in other periods. Furthermore, by the end of the century, all simulations under the RCP 8.5 project a shift of streamflow and sediment loads in the southwest monsoon peak from May to June, while preserving the peak in the inter-monsoon 2 (in October). The projected changes in annual sediment loads are greater than the projected changes in annual streamflow (in percentage) for both future periods.T.A.J.G. SirisenaShreedhar MaskeyJanaka BamunawalaErika CoppolaRoshanka RanasingheMDPI AGarticleKalu river basinregional climate modelsstreamflowsediment loadsHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3031, p 3031 (2021)
institution DOAJ
collection DOAJ
language EN
topic Kalu river basin
regional climate models
streamflow
sediment loads
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle Kalu river basin
regional climate models
streamflow
sediment loads
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
T.A.J.G. Sirisena
Shreedhar Maskey
Janaka Bamunawala
Erika Coppola
Roshanka Ranasinghe
Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
description Tropical countries are already experiencing the adverse impacts of climate change. This study presents projections of climate change-driven variations in hydrology and sediment loads in the Kalu River Basin, Sri Lanka. Bias-corrected climate projections (i.e., precipitation and temperature) from three high resolution (25 km) regional climate models (viz., RegCM4-MIROC5, MPI-M-MPI-ESM-MR, and NCC-NORESM1-M) are used here to force a calibrated hydrological model to project streamflow and sediment loads for two future periods (mid-century: 2046–2065, and end of the century: 2081–2099) under two representative concentration pathways (i.e., RCPs 2.6 and 8.5). By the end of the century under RCP 8.5, all simulations (forced with the three RCMs) project increased annual streamflow (67–87%) and sediment loads (128–145%). In general, streamflow and sediment loads are projected to increase more during the southwest monsoon season (May–September) than in other periods. Furthermore, by the end of the century, all simulations under the RCP 8.5 project a shift of streamflow and sediment loads in the southwest monsoon peak from May to June, while preserving the peak in the inter-monsoon 2 (in October). The projected changes in annual sediment loads are greater than the projected changes in annual streamflow (in percentage) for both future periods.
format article
author T.A.J.G. Sirisena
Shreedhar Maskey
Janaka Bamunawala
Erika Coppola
Roshanka Ranasinghe
author_facet T.A.J.G. Sirisena
Shreedhar Maskey
Janaka Bamunawala
Erika Coppola
Roshanka Ranasinghe
author_sort T.A.J.G. Sirisena
title Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
title_short Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
title_full Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
title_fullStr Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
title_full_unstemmed Projected Streamflow and Sediment Supply under Changing Climate to the Coast of the Kalu River Basin in Tropical Sri Lanka over the 21st Century
title_sort projected streamflow and sediment supply under changing climate to the coast of the kalu river basin in tropical sri lanka over the 21st century
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/be0e1c9003b74aed9188f723b1250f38
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