Can we extrapolate climate in an inner basin? The case of the Red Sea

We examine the possibility of making useful climate extrapolations in inner basins. Stressing the role of the local geographic features, for a practical example we focus our attention on the Red Sea. We observe that in spite of being an enclosed and relatively small Sea, its climate conditions are h...

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Published in:Global and Planetary Change
Main Authors: Langodan, Sabique, Cavaleri, Luigi, Portilla, Jesus, Abualnaja, Yasser, Hoteit, Ibrahim
Other Authors: Earth Fluid Modeling and Prediction Group, Earth Science and Engineering Program, Physical Science and Engineering (PSE) Division, Red Sea Research Center (RSRC), Institute of Marine Sciences, CNR-ISMAR, Venice, Italy, Department of Mechanical Engineering, Escuela Politécnica Nacional, Quito, Ecuador.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier BV 2020
Subjects:
Online Access:http://hdl.handle.net/10754/662152
https://doi.org/10.1016/j.gloplacha.2020.103151
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spelling ftkingabdullahun:oai:repository.kaust.edu.sa:10754/662152 2023-12-03T10:27:17+01:00 Can we extrapolate climate in an inner basin? The case of the Red Sea Langodan, Sabique Cavaleri, Luigi Portilla, Jesus Abualnaja, Yasser Hoteit, Ibrahim Earth Fluid Modeling and Prediction Group Earth Science and Engineering Program Physical Science and Engineering (PSE) Division Red Sea Research Center (RSRC) Institute of Marine Sciences, CNR-ISMAR, Venice, Italy Department of Mechanical Engineering, Escuela Politécnica Nacional, Quito, Ecuador. 2020-03-16T07:39:49Z application/pdf http://hdl.handle.net/10754/662152 https://doi.org/10.1016/j.gloplacha.2020.103151 unknown Elsevier BV https://linkinghub.elsevier.com/retrieve/pii/S0921818120300412 Langodan, S., Cavaleri, L., Portilla, J., Abualnaja, Y., & Hoteit, I. (2020). Can we extrapolate climate in an inner basin? The case of the Red Sea. Global and Planetary Change, 188, 103151. doi:10.1016/j.gloplacha.2020.103151 doi:10.1016/j.gloplacha.2020.103151 Global and Planetary Change http://hdl.handle.net/10754/662152 NOTICE: this is the author’s version of a work that was accepted for publication in Global and Planetary Change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Global and Planetary Change, [[Volume], [Issue], (2020-02-28)] DOI:10.1016/j.gloplacha.2020.103151 . © 2020. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ 2022-03-05 Article 2020 ftkingabdullahun https://doi.org/10.1016/j.gloplacha.2020.103151 2023-11-04T20:21:59Z We examine the possibility of making useful climate extrapolations in inner basins. Stressing the role of the local geographic features, for a practical example we focus our attention on the Red Sea. We observe that in spite of being an enclosed and relatively small Sea, its climate conditions are heavily affected by those of the larger neighboring regions, in particular the Mediterranean and the Arabian Seas. Using existing high-resolution information of the recent decades, we use both reasoned extrapolation and knowledge of, past and future, longer term general climatic information to frame what is presently possible to assess for the Red Sea. Specifically, the northern part, influenced by the Mediterranean Sea, shows a clear decreasing trend of both the meteorological and wave conditions in the recent decades. However, within a longer span record of 100 years, this decrease appears to be part of a 70-year cycle, which may be overturning, partly at least, in the coming decades. These trends are consistent with the expectations inferred from regional climatic indices, such as North Atlantic Oscillation and Atlantic Multidecadal Oscillation. No similar long term trend has been found for wave, hence implicitly the wind, conditions in the southern part of the basin. As expected, some correlation exists with the typical patterns of the Indian Ocean, but without any specific indication of a future trend. We suggest that, suitably adapted for the specific local conditions and dominant patterns, similar correlation and physical patterns may exist in several of the enclosed areas of the world, opening the possibility of exploring their possible trends in the future decades. This research was supported by the King Abdulla University of Science and Technology (KAUST) under the virtual Red Sea Initiative (Grant # REP/1/3268-01-01). Sabique Langodan was supported by the General Commission of Survey (GCS), under Project RGC/3/1612-01-01 made by Office of Sponsored research (ORS)/KAUST, Kingdom of Saudi Arabia. Luigi. ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation King Abdullah University of Science and Technology: KAUST Repository Indian Global and Planetary Change 188 103151
institution Open Polar
collection King Abdullah University of Science and Technology: KAUST Repository
op_collection_id ftkingabdullahun
language unknown
description We examine the possibility of making useful climate extrapolations in inner basins. Stressing the role of the local geographic features, for a practical example we focus our attention on the Red Sea. We observe that in spite of being an enclosed and relatively small Sea, its climate conditions are heavily affected by those of the larger neighboring regions, in particular the Mediterranean and the Arabian Seas. Using existing high-resolution information of the recent decades, we use both reasoned extrapolation and knowledge of, past and future, longer term general climatic information to frame what is presently possible to assess for the Red Sea. Specifically, the northern part, influenced by the Mediterranean Sea, shows a clear decreasing trend of both the meteorological and wave conditions in the recent decades. However, within a longer span record of 100 years, this decrease appears to be part of a 70-year cycle, which may be overturning, partly at least, in the coming decades. These trends are consistent with the expectations inferred from regional climatic indices, such as North Atlantic Oscillation and Atlantic Multidecadal Oscillation. No similar long term trend has been found for wave, hence implicitly the wind, conditions in the southern part of the basin. As expected, some correlation exists with the typical patterns of the Indian Ocean, but without any specific indication of a future trend. We suggest that, suitably adapted for the specific local conditions and dominant patterns, similar correlation and physical patterns may exist in several of the enclosed areas of the world, opening the possibility of exploring their possible trends in the future decades. This research was supported by the King Abdulla University of Science and Technology (KAUST) under the virtual Red Sea Initiative (Grant # REP/1/3268-01-01). Sabique Langodan was supported by the General Commission of Survey (GCS), under Project RGC/3/1612-01-01 made by Office of Sponsored research (ORS)/KAUST, Kingdom of Saudi Arabia. Luigi. ...
author2 Earth Fluid Modeling and Prediction Group
Earth Science and Engineering Program
Physical Science and Engineering (PSE) Division
Red Sea Research Center (RSRC)
Institute of Marine Sciences, CNR-ISMAR, Venice, Italy
Department of Mechanical Engineering, Escuela Politécnica Nacional, Quito, Ecuador.
format Article in Journal/Newspaper
author Langodan, Sabique
Cavaleri, Luigi
Portilla, Jesus
Abualnaja, Yasser
Hoteit, Ibrahim
spellingShingle Langodan, Sabique
Cavaleri, Luigi
Portilla, Jesus
Abualnaja, Yasser
Hoteit, Ibrahim
Can we extrapolate climate in an inner basin? The case of the Red Sea
author_facet Langodan, Sabique
Cavaleri, Luigi
Portilla, Jesus
Abualnaja, Yasser
Hoteit, Ibrahim
author_sort Langodan, Sabique
title Can we extrapolate climate in an inner basin? The case of the Red Sea
title_short Can we extrapolate climate in an inner basin? The case of the Red Sea
title_full Can we extrapolate climate in an inner basin? The case of the Red Sea
title_fullStr Can we extrapolate climate in an inner basin? The case of the Red Sea
title_full_unstemmed Can we extrapolate climate in an inner basin? The case of the Red Sea
title_sort can we extrapolate climate in an inner basin? the case of the red sea
publisher Elsevier BV
publishDate 2020
url http://hdl.handle.net/10754/662152
https://doi.org/10.1016/j.gloplacha.2020.103151
geographic Indian
geographic_facet Indian
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://linkinghub.elsevier.com/retrieve/pii/S0921818120300412
Langodan, S., Cavaleri, L., Portilla, J., Abualnaja, Y., & Hoteit, I. (2020). Can we extrapolate climate in an inner basin? The case of the Red Sea. Global and Planetary Change, 188, 103151. doi:10.1016/j.gloplacha.2020.103151
doi:10.1016/j.gloplacha.2020.103151
Global and Planetary Change
http://hdl.handle.net/10754/662152
op_rights NOTICE: this is the author’s version of a work that was accepted for publication in Global and Planetary Change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Global and Planetary Change, [[Volume], [Issue], (2020-02-28)] DOI:10.1016/j.gloplacha.2020.103151 . © 2020. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
2022-03-05
op_doi https://doi.org/10.1016/j.gloplacha.2020.103151
container_title Global and Planetary Change
container_volume 188
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