Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases

In this study, the El Nino Southern Oscillation (ENSO) phase index is used for water management over the Kotmale reservoir in Sri Lanka. Daily rainfall data of 9 stations over the Kotmale catchment during 1960–2005 June-September (JJAS) season is investigated over the Kotmale catchment. The ENSO pha...

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Main Authors: Sewwandhi Chandrasekara, Venkatraman Prasanna, Hyun-Han Kwon
Format: Article
Language:English
Published: Hindawi Limited 2017-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2017/4025964
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spelling doaj-90d09ab18ef54914961eb9219d0ff3622020-11-24T23:07:05ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172017-01-01201710.1155/2017/40259644025964Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO PhasesSewwandhi Chandrasekara0Venkatraman Prasanna1Hyun-Han Kwon2Chonbuk National University, Jeonju, Republic of KoreaNational Institute of Meteorological Sciences, Jeju, Republic of KoreaChonbuk National University, Jeonju, Republic of KoreaIn this study, the El Nino Southern Oscillation (ENSO) phase index is used for water management over the Kotmale reservoir in Sri Lanka. Daily rainfall data of 9 stations over the Kotmale catchment during 1960–2005 June-September (JJAS) season is investigated over the Kotmale catchment. The ENSO phases are identified based on the 0.5°C sea surface temperature (SST) anomaly over Nino 3 region. The study has brought out few stations showing increasing and a few decreasing seasonal rainfall trends for JJAS season, while there is no change in the annual rainfall for the catchment. Monthly and seasonal rainfall of all the selected stations showed negative correlation with the sea surface temperature (SST) over the Nino-3 region index during JJAS season with varying magnitudes. During the warm phase of ENSO, below average rainfall is prominent for JJAS season over many stations. The rainfall especially during early September showed a significant below average rainfall during the warm ENSO phase. The seasonal rainfall during neutral and cold ENSO phases does not experience similar significant changes as seen during warm ENSO phase. Inflow of the Kotmale reservoir shows decreasing trend for the period of 1960–2005 in the observation from all stations collectively.http://dx.doi.org/10.1155/2017/4025964
collection DOAJ
language English
format Article
sources DOAJ
author Sewwandhi Chandrasekara
Venkatraman Prasanna
Hyun-Han Kwon
spellingShingle Sewwandhi Chandrasekara
Venkatraman Prasanna
Hyun-Han Kwon
Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
Advances in Meteorology
author_facet Sewwandhi Chandrasekara
Venkatraman Prasanna
Hyun-Han Kwon
author_sort Sewwandhi Chandrasekara
title Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
title_short Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
title_full Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
title_fullStr Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
title_full_unstemmed Monitoring Water Resources over the Kotmale Reservoir in Sri Lanka Using ENSO Phases
title_sort monitoring water resources over the kotmale reservoir in sri lanka using enso phases
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2017-01-01
description In this study, the El Nino Southern Oscillation (ENSO) phase index is used for water management over the Kotmale reservoir in Sri Lanka. Daily rainfall data of 9 stations over the Kotmale catchment during 1960–2005 June-September (JJAS) season is investigated over the Kotmale catchment. The ENSO phases are identified based on the 0.5°C sea surface temperature (SST) anomaly over Nino 3 region. The study has brought out few stations showing increasing and a few decreasing seasonal rainfall trends for JJAS season, while there is no change in the annual rainfall for the catchment. Monthly and seasonal rainfall of all the selected stations showed negative correlation with the sea surface temperature (SST) over the Nino-3 region index during JJAS season with varying magnitudes. During the warm phase of ENSO, below average rainfall is prominent for JJAS season over many stations. The rainfall especially during early September showed a significant below average rainfall during the warm ENSO phase. The seasonal rainfall during neutral and cold ENSO phases does not experience similar significant changes as seen during warm ENSO phase. Inflow of the Kotmale reservoir shows decreasing trend for the period of 1960–2005 in the observation from all stations collectively.
url http://dx.doi.org/10.1155/2017/4025964
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