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Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean
Energies, Volume: 13, Issue: 11, Start page: 3028
Swansea University Author: Harshinie Karunarathna
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DOI (Published version): 10.3390/en13113028
Abstract
This study investigates the impacts of global climate change on the future wave power potential, taking Sri Lanka as a case study from the northern Indian Ocean. The geographical location of Sri Lanka, which receives long-distance swell waves generated in the Southern Indian Ocean, favors wave energ...
Published in: | Energies |
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ISSN: | 1996-1073 1996-1073 |
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2020
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2020-10-16T14:34:34.0915808 v2 54463 2020-06-12 Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean 0d3d327a240d49b53c78e02b7c00e625 0000-0002-9087-3811 Harshinie Karunarathna Harshinie Karunarathna true false 2020-06-12 CIVL This study investigates the impacts of global climate change on the future wave power potential, taking Sri Lanka as a case study from the northern Indian Ocean. The geographical location of Sri Lanka, which receives long-distance swell waves generated in the Southern Indian Ocean, favors wave energy-harvesting. Waves projected by a numerical wave model developed using Simulating Waves Nearshore Waves (SWAN) wave model, which is forced by atmospheric forcings generated by an Atmospheric Global Climate Model (AGCM) within two time slices that represent “present” and “future” (end of century) wave climates, are used to evaluate and compare present and future wave power potential around Sri Lanka. The results reveal that there will be a 12–20% reduction in average available wave power along the south-west and south-east coasts of Sri Lanka in future. This reduction is due mainly to changes to the tropical south-west monsoon system because of global climate change. The available wave power resource attributed to swell wave component remains largely unchanged. Although a detailed analysis of monthly and annual average wave power under both “present” and “future” climates reveals a strong seasonal and some degree of inter-annual variability of wave power, a notable decadal-scale trend of variability is not visible during the simulated 25-year periods. Finally, the results reveal that the wave power attributed to swell waves are very stable over the long term. Journal Article Energies 13 11 3028 MDPI AG 1996-1073 1996-1073 climate change; ocean wave power; wave projections; Sri Lanka; Indian Ocean 11 6 2020 2020-06-11 10.3390/en13113028 COLLEGE NANME Civil Engineering COLLEGE CODE CIVL Swansea University 2020-10-16T14:34:34.0915808 2020-06-12T10:45:54.5324241 Professional Services ISS - Uncategorised Harshinie Karunarathna 0000-0002-9087-3811 1 Pravin Maduwantha 2 Bahareh Kamranzad 3 Harsha Rathnasooriya 4 Kasun De Silva 5 54463__17483__e8194eecbc9d4695bdd9e6ab9494805a.pdf 54463.pdf 2020-06-12T10:49:29.0162477 Output 4354375 application/pdf Version of Record true This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited true |
title |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
spellingShingle |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean Harshinie Karunarathna |
title_short |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
title_full |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
title_fullStr |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
title_full_unstemmed |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
title_sort |
Impacts of Global Climate Change on the Future Ocean Wave Power Potential: A Case Study from the Indian Ocean |
author_id_str_mv |
0d3d327a240d49b53c78e02b7c00e625 |
author_id_fullname_str_mv |
0d3d327a240d49b53c78e02b7c00e625_***_Harshinie Karunarathna |
author |
Harshinie Karunarathna |
author2 |
Harshinie Karunarathna Pravin Maduwantha Bahareh Kamranzad Harsha Rathnasooriya Kasun De Silva |
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Energies |
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13 |
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11 |
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3028 |
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2020 |
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Swansea University |
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1996-1073 1996-1073 |
doi_str_mv |
10.3390/en13113028 |
publisher |
MDPI AG |
college_str |
Professional Services |
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description |
This study investigates the impacts of global climate change on the future wave power potential, taking Sri Lanka as a case study from the northern Indian Ocean. The geographical location of Sri Lanka, which receives long-distance swell waves generated in the Southern Indian Ocean, favors wave energy-harvesting. Waves projected by a numerical wave model developed using Simulating Waves Nearshore Waves (SWAN) wave model, which is forced by atmospheric forcings generated by an Atmospheric Global Climate Model (AGCM) within two time slices that represent “present” and “future” (end of century) wave climates, are used to evaluate and compare present and future wave power potential around Sri Lanka. The results reveal that there will be a 12–20% reduction in average available wave power along the south-west and south-east coasts of Sri Lanka in future. This reduction is due mainly to changes to the tropical south-west monsoon system because of global climate change. The available wave power resource attributed to swell wave component remains largely unchanged. Although a detailed analysis of monthly and annual average wave power under both “present” and “future” climates reveals a strong seasonal and some degree of inter-annual variability of wave power, a notable decadal-scale trend of variability is not visible during the simulated 25-year periods. Finally, the results reveal that the wave power attributed to swell waves are very stable over the long term. |
published_date |
2020-06-11T04:08:00Z |
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1763753570661826560 |
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11.036706 |