What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?

Observations indicate that spring and fall phytoplankton blooms on the Eastern Bering Sea (EBS) continental shelf tend to co-vary on inter-annual scales - that is, a year with a strong spring bloom also tends to have a strong fall bloom. Similar co-variability of primary production is also seen in t...

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Published in:Deep Sea Research Part II: Topical Studies in Oceanography
Other Authors: Cheng, Wei (author), Curchitser, Enrique (author), Stock, Charles (author), Hermann, Albert (author), Cokelet, Edward (author), Mordy, Calvin (author), Stabeno, Phyllis (author), Hervieux, Gaelle (author), Castruccio, Frederic (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1016/j.dsr2.2015.07.009
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spelling ftncar:oai:drupal-site.org:articles_19393 2023-09-05T13:18:31+02:00 What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf? Cheng, Wei (author) Curchitser, Enrique (author) Stock, Charles (author) Hermann, Albert (author) Cokelet, Edward (author) Mordy, Calvin (author) Stabeno, Phyllis (author) Hervieux, Gaelle (author) Castruccio, Frederic (author) 2016-12 https://doi.org/10.1016/j.dsr2.2015.07.009 en eng Deep Sea Research Part II: Topical Studies in Oceanography--Deep Sea Research Part II: Topical Studies in Oceanography--09670645 articles:19393 ark:/85065/d7rj4m7k doi:10.1016/j.dsr2.2015.07.009 Copyright 2016 Elsevier. article Text 2016 ftncar https://doi.org/10.1016/j.dsr2.2015.07.009 2023-08-14T18:47:31Z Observations indicate that spring and fall phytoplankton blooms on the Eastern Bering Sea (EBS) continental shelf tend to co-vary on inter-annual scales - that is, a year with a strong spring bloom also tends to have a strong fall bloom. Similar co-variability of primary production is also seen in the multiyear (1987-2007) integration of a coupled physical-biological model. Moreover, the modeled seasonal amplitudes of 10-meter chlorophyll-a concentrations at the EBS middle shelf mooring locations, computed using the canonical Redfield ratio and a mean carbon-to-chlorophyll-a ratio, are generally consistent with the in situ mooring measurements. The coupled physical-biological model simulation is used to examine the relative contributions of wind mixing, local nutrient recycling/regeneration, horizontal nutrient advection, and water-column stability to this co-variability. There is no significant correlation between the spring and fall surface wind mixing. Although wind mixing is an important mechanism for bringing nutrients in the lower water column to the surface layers, it is not the mechanism tying the two seasons' productivity together. Local regeneration/recycling of the nutrients initially fueling spring production is an important mechanism for spring-to-fall nutrient accumulation in the bottom layers at the middle shelf. Horizontal advection does not appear to be the dominant factor for supplying nutrients to the middle shelf during the spring-to-fall period. Fall primary production in the model is strongly influenced by the lower water-column stability/stratification. Taken together, these results highlight the importance of local recycling/regeneration of nutrients assimilated by spring phytoplankton bloom in linking together the spring and fall primary productions on EBS middle shelf. (C) 2015 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Bering Sea OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Bering Sea Deep Sea Research Part II: Topical Studies in Oceanography 134 128 140
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Observations indicate that spring and fall phytoplankton blooms on the Eastern Bering Sea (EBS) continental shelf tend to co-vary on inter-annual scales - that is, a year with a strong spring bloom also tends to have a strong fall bloom. Similar co-variability of primary production is also seen in the multiyear (1987-2007) integration of a coupled physical-biological model. Moreover, the modeled seasonal amplitudes of 10-meter chlorophyll-a concentrations at the EBS middle shelf mooring locations, computed using the canonical Redfield ratio and a mean carbon-to-chlorophyll-a ratio, are generally consistent with the in situ mooring measurements. The coupled physical-biological model simulation is used to examine the relative contributions of wind mixing, local nutrient recycling/regeneration, horizontal nutrient advection, and water-column stability to this co-variability. There is no significant correlation between the spring and fall surface wind mixing. Although wind mixing is an important mechanism for bringing nutrients in the lower water column to the surface layers, it is not the mechanism tying the two seasons' productivity together. Local regeneration/recycling of the nutrients initially fueling spring production is an important mechanism for spring-to-fall nutrient accumulation in the bottom layers at the middle shelf. Horizontal advection does not appear to be the dominant factor for supplying nutrients to the middle shelf during the spring-to-fall period. Fall primary production in the model is strongly influenced by the lower water-column stability/stratification. Taken together, these results highlight the importance of local recycling/regeneration of nutrients assimilated by spring phytoplankton bloom in linking together the spring and fall primary productions on EBS middle shelf. (C) 2015 Elsevier Ltd. All rights reserved.
author2 Cheng, Wei (author)
Curchitser, Enrique (author)
Stock, Charles (author)
Hermann, Albert (author)
Cokelet, Edward (author)
Mordy, Calvin (author)
Stabeno, Phyllis (author)
Hervieux, Gaelle (author)
Castruccio, Frederic (author)
format Article in Journal/Newspaper
title What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
spellingShingle What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
title_short What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
title_full What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
title_fullStr What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
title_full_unstemmed What processes contribute to the spring and fall bloom co-variability on the Eastern Bering Sea shelf?
title_sort what processes contribute to the spring and fall bloom co-variability on the eastern bering sea shelf?
publishDate 2016
url https://doi.org/10.1016/j.dsr2.2015.07.009
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
genre_facet Bering Sea
op_relation Deep Sea Research Part II: Topical Studies in Oceanography--Deep Sea Research Part II: Topical Studies in Oceanography--09670645
articles:19393
ark:/85065/d7rj4m7k
doi:10.1016/j.dsr2.2015.07.009
op_rights Copyright 2016 Elsevier.
op_doi https://doi.org/10.1016/j.dsr2.2015.07.009
container_title Deep Sea Research Part II: Topical Studies in Oceanography
container_volume 134
container_start_page 128
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