An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects

Previous investigations of the large-scale deployment of Ocean Thermal Energy Conversions (OTEC) systems are extended by allowing some atmospheric feedback in an ocean general circulation model. A modified ocean-atmosphere thermal boundary condition is used where relaxation corresponds to atmospheri...

Full description

Bibliographic Details
Published in:Journal of Marine Science and Engineering
Main Authors: Yanli Jia, Gérard Nihous, Krishnakumar Rajagopalan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/jmse6010012
id ftmdpi:oai:mdpi.com:/2077-1312/6/1/12/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2077-1312/6/1/12/ 2023-08-20T04:01:21+02:00 An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects Yanli Jia Gérard Nihous Krishnakumar Rajagopalan agris 2018-01-22 application/pdf https://doi.org/10.3390/jmse6010012 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/jmse6010012 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 6; Issue 1; Pages: 12 Ocean Thermal Energy Conversion OTEC ocean general circulation model Text 2018 ftmdpi https://doi.org/10.3390/jmse6010012 2023-07-31T21:21:36Z Previous investigations of the large-scale deployment of Ocean Thermal Energy Conversions (OTEC) systems are extended by allowing some atmospheric feedback in an ocean general circulation model. A modified ocean-atmosphere thermal boundary condition is used where relaxation corresponds to atmospheric longwave radiation to space, and an additional term expresses horizontal atmospheric transport. This produces lower steady-state OTEC power maxima (8 to 10.2 TW instead of 14.1 TW for global OTEC scenarios, and 7.2 to 9.3 TW instead of 11.9 TW for OTEC implementation within 100 km of coastlines). When power production peaks, power intensity remains practically unchanged, at 0.2 TW per Sverdrup of OTEC deep cold seawater, suggesting a similar degradation of the OTEC thermal resource. Large-scale environmental effects include surface cooling in low latitudes and warming elsewhere, with a net heat intake within the water column. These changes develop rapidly from the propagation of Kelvin and Rossby waves, and ocean current advection. Two deep circulation cells are generated in the Atlantic and Indo-Pacific basins. The Atlantic Meridional Overturning Circulation (AMOC) is reinforced while an AMOC-like feature appears in the North Pacific, with deep convective winter events at high latitudes. Transport between the Indo-Pacific and the Southern Ocean is strengthened, with impacts on the Atlantic via the Antarctic Circumpolar Current (ACC). Text Antarc* Antarctic Southern Ocean MDPI Open Access Publishing Antarctic Southern Ocean The Antarctic Pacific Journal of Marine Science and Engineering 6 1 12
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Ocean Thermal Energy Conversion
OTEC
ocean general circulation model
spellingShingle Ocean Thermal Energy Conversion
OTEC
ocean general circulation model
Yanli Jia
Gérard Nihous
Krishnakumar Rajagopalan
An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
topic_facet Ocean Thermal Energy Conversion
OTEC
ocean general circulation model
description Previous investigations of the large-scale deployment of Ocean Thermal Energy Conversions (OTEC) systems are extended by allowing some atmospheric feedback in an ocean general circulation model. A modified ocean-atmosphere thermal boundary condition is used where relaxation corresponds to atmospheric longwave radiation to space, and an additional term expresses horizontal atmospheric transport. This produces lower steady-state OTEC power maxima (8 to 10.2 TW instead of 14.1 TW for global OTEC scenarios, and 7.2 to 9.3 TW instead of 11.9 TW for OTEC implementation within 100 km of coastlines). When power production peaks, power intensity remains practically unchanged, at 0.2 TW per Sverdrup of OTEC deep cold seawater, suggesting a similar degradation of the OTEC thermal resource. Large-scale environmental effects include surface cooling in low latitudes and warming elsewhere, with a net heat intake within the water column. These changes develop rapidly from the propagation of Kelvin and Rossby waves, and ocean current advection. Two deep circulation cells are generated in the Atlantic and Indo-Pacific basins. The Atlantic Meridional Overturning Circulation (AMOC) is reinforced while an AMOC-like feature appears in the North Pacific, with deep convective winter events at high latitudes. Transport between the Indo-Pacific and the Southern Ocean is strengthened, with impacts on the Atlantic via the Antarctic Circumpolar Current (ACC).
format Text
author Yanli Jia
Gérard Nihous
Krishnakumar Rajagopalan
author_facet Yanli Jia
Gérard Nihous
Krishnakumar Rajagopalan
author_sort Yanli Jia
title An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
title_short An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
title_full An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
title_fullStr An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
title_full_unstemmed An Evaluation of the Large-Scale Implementation of Ocean Thermal Energy Conversion (OTEC) Using an Ocean General Circulation Model with Low-Complexity Atmospheric Feedback Effects
title_sort evaluation of the large-scale implementation of ocean thermal energy conversion (otec) using an ocean general circulation model with low-complexity atmospheric feedback effects
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/jmse6010012
op_coverage agris
geographic Antarctic
Southern Ocean
The Antarctic
Pacific
geographic_facet Antarctic
Southern Ocean
The Antarctic
Pacific
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_source Journal of Marine Science and Engineering; Volume 6; Issue 1; Pages: 12
op_relation https://dx.doi.org/10.3390/jmse6010012
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse6010012
container_title Journal of Marine Science and Engineering
container_volume 6
container_issue 1
container_start_page 12
_version_ 1774724637603659776