A brief introduction to the issue of climate and marine fisheries

Climatic variability has profound effects on the distribution, abundance and catch of oceanic fish species around the world. The major modes of this climate variability include the El Niño-Southern Oscillation (ENSO) events, the Pacific Decadal Oscillation (PDO) also referred to as the Interdecadal...

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Main Author: M. Salinger
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1007/s10584-013-0762-z
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spelling ftrepec:oai:RePEc:spr:climat:v:119:y:2013:i:1:p:23-35 2023-05-15T15:16:17+02:00 A brief introduction to the issue of climate and marine fisheries M. Salinger http://hdl.handle.net/10.1007/s10584-013-0762-z unknown http://hdl.handle.net/10.1007/s10584-013-0762-z article ftrepec 2020-12-04T13:33:09Z Climatic variability has profound effects on the distribution, abundance and catch of oceanic fish species around the world. The major modes of this climate variability include the El Niño-Southern Oscillation (ENSO) events, the Pacific Decadal Oscillation (PDO) also referred to as the Interdecadal Pacific Oscillation (IPO), the Indian Ocean Dipole (IOD), the Southern Annular Mode (SAM) and the North Atlantic Oscillation (NAO). Other modes of climate variability include the North Pacific Gyre Oscillation (NPGO), the Atlantic Multidecadal Oscillation (AMO) and the Arctic Oscillation (AO). ENSO events are the principle source of interannual global climate variability, centred in the ocean–atmosphere circulations of the tropical Pacific Ocean and operating on seasonal to interannual time scales. ENSO and the strength of its climate teleconnections are modulated on decadal timescales by the IPO. The time scale of the IOD is seasonal to interannual. The SAM in the mid to high latitudes of the Southern Hemisphere operates in the range of 50–60 days. A prominent teleconnection pattern throughout the year in the Northern Hemisphere is the North Atlantic Oscillation (NAO) which modulates the strength of the westerlies across the North Atlantic in winter, has an impact on the catches of marine fisheries. ENSO events affect the distribution of tuna species in the equatorial Pacific, especially skipjack tuna as well as the abundance and distribution of fish along the western coasts of the Americas. The IOD modulates the distribution of tuna populations and catches in the Indian Ocean, whilst the NAO affects cod stocks heavily exploited in the Atlantic Ocean. The SAM, and its effects on sea surface temperatures influence krill biomass and fisheries catches in the Southern Ocean. The response of oceanic fish stocks to these sources of climatic variability can be used as a guide to the likely effects of climate change on these valuable resources. Copyright Springer Science+Business Media Dordrecht 2013 Article in Journal/Newspaper Arctic Climate change North Atlantic North Atlantic oscillation Southern Ocean RePEc (Research Papers in Economics) Arctic Indian Pacific Southern Ocean
institution Open Polar
collection RePEc (Research Papers in Economics)
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language unknown
description Climatic variability has profound effects on the distribution, abundance and catch of oceanic fish species around the world. The major modes of this climate variability include the El Niño-Southern Oscillation (ENSO) events, the Pacific Decadal Oscillation (PDO) also referred to as the Interdecadal Pacific Oscillation (IPO), the Indian Ocean Dipole (IOD), the Southern Annular Mode (SAM) and the North Atlantic Oscillation (NAO). Other modes of climate variability include the North Pacific Gyre Oscillation (NPGO), the Atlantic Multidecadal Oscillation (AMO) and the Arctic Oscillation (AO). ENSO events are the principle source of interannual global climate variability, centred in the ocean–atmosphere circulations of the tropical Pacific Ocean and operating on seasonal to interannual time scales. ENSO and the strength of its climate teleconnections are modulated on decadal timescales by the IPO. The time scale of the IOD is seasonal to interannual. The SAM in the mid to high latitudes of the Southern Hemisphere operates in the range of 50–60 days. A prominent teleconnection pattern throughout the year in the Northern Hemisphere is the North Atlantic Oscillation (NAO) which modulates the strength of the westerlies across the North Atlantic in winter, has an impact on the catches of marine fisheries. ENSO events affect the distribution of tuna species in the equatorial Pacific, especially skipjack tuna as well as the abundance and distribution of fish along the western coasts of the Americas. The IOD modulates the distribution of tuna populations and catches in the Indian Ocean, whilst the NAO affects cod stocks heavily exploited in the Atlantic Ocean. The SAM, and its effects on sea surface temperatures influence krill biomass and fisheries catches in the Southern Ocean. The response of oceanic fish stocks to these sources of climatic variability can be used as a guide to the likely effects of climate change on these valuable resources. Copyright Springer Science+Business Media Dordrecht 2013
format Article in Journal/Newspaper
author M. Salinger
spellingShingle M. Salinger
A brief introduction to the issue of climate and marine fisheries
author_facet M. Salinger
author_sort M. Salinger
title A brief introduction to the issue of climate and marine fisheries
title_short A brief introduction to the issue of climate and marine fisheries
title_full A brief introduction to the issue of climate and marine fisheries
title_fullStr A brief introduction to the issue of climate and marine fisheries
title_full_unstemmed A brief introduction to the issue of climate and marine fisheries
title_sort brief introduction to the issue of climate and marine fisheries
url http://hdl.handle.net/10.1007/s10584-013-0762-z
geographic Arctic
Indian
Pacific
Southern Ocean
geographic_facet Arctic
Indian
Pacific
Southern Ocean
genre Arctic
Climate change
North Atlantic
North Atlantic oscillation
Southern Ocean
genre_facet Arctic
Climate change
North Atlantic
North Atlantic oscillation
Southern Ocean
op_relation http://hdl.handle.net/10.1007/s10584-013-0762-z
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