A model of the spring bloom in the North Atlantic and its impact on ocean optics
A model of the development of the spring phytoplankton bloom in the North Atlantic and its effect on light attenuation in the water column is presented. The model uses as input data on the climatological mixed‐layer depth, solar irradiance at the sea surface, and basin‐scale distribution of nitrate...
Published in: | Limnology and Oceanography |
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Language: | English |
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Wiley
1989
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Online Access: | http://dx.doi.org/10.4319/lo.1989.34.8.1563 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1989.34.8.1563 https://onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 |
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crwiley:10.4319/lo.1989.34.8.1563 2024-10-06T13:51:01+00:00 A model of the spring bloom in the North Atlantic and its impact on ocean optics Wroblewski, J. S. 1989 http://dx.doi.org/10.4319/lo.1989.34.8.1563 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1989.34.8.1563 https://onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 34, issue 8, page 1563-1571 ISSN 0024-3590 1939-5590 journal-article 1989 crwiley https://doi.org/10.4319/lo.1989.34.8.1563 2024-09-11T04:15:17Z A model of the development of the spring phytoplankton bloom in the North Atlantic and its effect on light attenuation in the water column is presented. The model uses as input data on the climatological mixed‐layer depth, solar irradiance at the sea surface, and basin‐scale distribution of nitrate at standard depths. The simulated phytoplankton bloom progresses from mid‐ to high latitudes following the shallowing of the mixed layer during March through June. The bloom occurs first in coastal waters where the mixed layer is shallow and later in the open ocean. Local peak concentrations of phytoplankton last 1–2 weeks. As phytoplankton are the major absorbers and scatterers of light in the open ocean, the relationship between chlorophyll concentration and light attenuation can be used to predict time‐varying fields of light extinction. The basin‐scale variability in the attenuation coefficient for downwelling irradiance at 490 nm ( K 490) in May is computed as an example. Article in Journal/Newspaper North Atlantic Wiley Online Library Limnology and Oceanography 34 8 1563 1571 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
A model of the development of the spring phytoplankton bloom in the North Atlantic and its effect on light attenuation in the water column is presented. The model uses as input data on the climatological mixed‐layer depth, solar irradiance at the sea surface, and basin‐scale distribution of nitrate at standard depths. The simulated phytoplankton bloom progresses from mid‐ to high latitudes following the shallowing of the mixed layer during March through June. The bloom occurs first in coastal waters where the mixed layer is shallow and later in the open ocean. Local peak concentrations of phytoplankton last 1–2 weeks. As phytoplankton are the major absorbers and scatterers of light in the open ocean, the relationship between chlorophyll concentration and light attenuation can be used to predict time‐varying fields of light extinction. The basin‐scale variability in the attenuation coefficient for downwelling irradiance at 490 nm ( K 490) in May is computed as an example. |
format |
Article in Journal/Newspaper |
author |
Wroblewski, J. S. |
spellingShingle |
Wroblewski, J. S. A model of the spring bloom in the North Atlantic and its impact on ocean optics |
author_facet |
Wroblewski, J. S. |
author_sort |
Wroblewski, J. S. |
title |
A model of the spring bloom in the North Atlantic and its impact on ocean optics |
title_short |
A model of the spring bloom in the North Atlantic and its impact on ocean optics |
title_full |
A model of the spring bloom in the North Atlantic and its impact on ocean optics |
title_fullStr |
A model of the spring bloom in the North Atlantic and its impact on ocean optics |
title_full_unstemmed |
A model of the spring bloom in the North Atlantic and its impact on ocean optics |
title_sort |
model of the spring bloom in the north atlantic and its impact on ocean optics |
publisher |
Wiley |
publishDate |
1989 |
url |
http://dx.doi.org/10.4319/lo.1989.34.8.1563 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1989.34.8.1563 https://onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1989.34.8.1563 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Limnology and Oceanography volume 34, issue 8, page 1563-1571 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.1989.34.8.1563 |
container_title |
Limnology and Oceanography |
container_volume |
34 |
container_issue |
8 |
container_start_page |
1563 |
op_container_end_page |
1571 |
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1812179147297914880 |