Chapter 2: Environmental Setting
Atmospheric and oceanographic patterns were mapped using satellite imagery and oceanographic models. These maps were used to describe the regional environment, and to develop models predicting deep-coral, cetacean, and seabird distributions. Seasons around the MHI are driven by changes in the North...
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ftplymouthml:oai:plymsea.ac.uk:7257 2023-05-15T13:14:56+02:00 Chapter 2: Environmental Setting Costa, BM Poti, M Winship, AJ Miller, PI Gove, J Costa, BM Kendall, MS 2016-07-31 text http://plymsea.ac.uk/id/eprint/7257/ http://plymsea.ac.uk/id/eprint/7257/1/MHI_BioAssess%2012.08.2016%20Final_hawaii_ch2_env_setting.pdf http://www2.coastalscience.noaa.gov/publications/handler.aspx?key=9208 en eng Bureau of Ocean Energy Management and National Oceanic and Atmospheric Administration http://plymsea.ac.uk/id/eprint/7257/1/MHI_BioAssess%2012.08.2016%20Final_hawaii_ch2_env_setting.pdf Costa, BM; Poti, M; Winship, AJ; Miller, PI; Gove, J. 2016 Chapter 2: Environmental Setting. In: Costa, BM; Kendall, MS, (eds.) Marine Biogeographic Assessment of the Main Hawaiian Islands. Silver Spring, MD, USA, Bureau of Ocean Energy Management and National Oceanic and Atmospheric Administration, 13-56, 359pp. (OCS Study BOEM 2016-035 and NOAA Technical Memorandum NOS NCCOS 214, OCS St). all_rights_reserved Conservation Ecology and Environment Marine Sciences Planning Policies Publication - Book Section NonPeerReviewed 2016 ftplymouthml 2022-09-13T05:48:56Z Atmospheric and oceanographic patterns were mapped using satellite imagery and oceanographic models. These maps were used to describe the regional environment, and to develop models predicting deep-coral, cetacean, and seabird distributions. Seasons around the MHI are driven by changes in the North Pacific Subtropical High and the Aleutian Low. Winter (November to April) is cooler, rainier, and dominated by the North Pacific swell. Summer (May to October) is warmer, less rainy, and dominated by the northeasterly trade winds and swell. Mountains and submerged topography change the direction and speed of winds and currents. These interactions cause the leeward sides of the island to be warmer and drier, and create frequent convergence, mixing, upwelling, fronts and eddies in the channels between the islands (e.g., the Kaiwi, Pailolo and ʻAlenuihānā Channels), and on the leeward sides of the islands (e.g., Kona Coast, Hawaiʻi). Book Part aleutian low Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) Pacific |
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Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) |
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ftplymouthml |
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English |
topic |
Conservation Ecology and Environment Marine Sciences Planning Policies |
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Conservation Ecology and Environment Marine Sciences Planning Policies Costa, BM Poti, M Winship, AJ Miller, PI Gove, J Chapter 2: Environmental Setting |
topic_facet |
Conservation Ecology and Environment Marine Sciences Planning Policies |
description |
Atmospheric and oceanographic patterns were mapped using satellite imagery and oceanographic models. These maps were used to describe the regional environment, and to develop models predicting deep-coral, cetacean, and seabird distributions. Seasons around the MHI are driven by changes in the North Pacific Subtropical High and the Aleutian Low. Winter (November to April) is cooler, rainier, and dominated by the North Pacific swell. Summer (May to October) is warmer, less rainy, and dominated by the northeasterly trade winds and swell. Mountains and submerged topography change the direction and speed of winds and currents. These interactions cause the leeward sides of the island to be warmer and drier, and create frequent convergence, mixing, upwelling, fronts and eddies in the channels between the islands (e.g., the Kaiwi, Pailolo and ʻAlenuihānā Channels), and on the leeward sides of the islands (e.g., Kona Coast, Hawaiʻi). |
author2 |
Costa, BM Kendall, MS |
format |
Book Part |
author |
Costa, BM Poti, M Winship, AJ Miller, PI Gove, J |
author_facet |
Costa, BM Poti, M Winship, AJ Miller, PI Gove, J |
author_sort |
Costa, BM |
title |
Chapter 2: Environmental Setting |
title_short |
Chapter 2: Environmental Setting |
title_full |
Chapter 2: Environmental Setting |
title_fullStr |
Chapter 2: Environmental Setting |
title_full_unstemmed |
Chapter 2: Environmental Setting |
title_sort |
chapter 2: environmental setting |
publisher |
Bureau of Ocean Energy Management and National Oceanic and Atmospheric Administration |
publishDate |
2016 |
url |
http://plymsea.ac.uk/id/eprint/7257/ http://plymsea.ac.uk/id/eprint/7257/1/MHI_BioAssess%2012.08.2016%20Final_hawaii_ch2_env_setting.pdf http://www2.coastalscience.noaa.gov/publications/handler.aspx?key=9208 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
aleutian low |
genre_facet |
aleutian low |
op_relation |
http://plymsea.ac.uk/id/eprint/7257/1/MHI_BioAssess%2012.08.2016%20Final_hawaii_ch2_env_setting.pdf Costa, BM; Poti, M; Winship, AJ; Miller, PI; Gove, J. 2016 Chapter 2: Environmental Setting. In: Costa, BM; Kendall, MS, (eds.) Marine Biogeographic Assessment of the Main Hawaiian Islands. Silver Spring, MD, USA, Bureau of Ocean Energy Management and National Oceanic and Atmospheric Administration, 13-56, 359pp. (OCS Study BOEM 2016-035 and NOAA Technical Memorandum NOS NCCOS 214, OCS St). |
op_rights |
all_rights_reserved |
_version_ |
1766266171197227008 |