Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea

Abstract Mustapha, M. A., Sei-Ichi, S., and Lihan, T. 2009. Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea. – ICES Journal of Marine Science, 66: 1557–1569. Seasonal variation in primary production after a retreat of the sea ice in the s...

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Published in:ICES Journal of Marine Science
Main Authors: Mustapha, M. A., Sei-Ichi, S., Lihan, T.
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2009
Subjects:
Online Access:http://dx.doi.org/10.1093/icesjms/fsp142
http://academic.oup.com/icesjms/article-pdf/66/7/1557/29134018/fsp142.pdf
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spelling croxfordunivpr:10.1093/icesjms/fsp142 2024-09-15T18:28:36+00:00 Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea Mustapha, M. A. Sei-Ichi, S. Lihan, T. 2009 http://dx.doi.org/10.1093/icesjms/fsp142 http://academic.oup.com/icesjms/article-pdf/66/7/1557/29134018/fsp142.pdf en eng Oxford University Press (OUP) ICES Journal of Marine Science volume 66, issue 7, page 1557-1569 ISSN 1095-9289 1054-3139 journal-article 2009 croxfordunivpr https://doi.org/10.1093/icesjms/fsp142 2024-06-24T04:25:33Z Abstract Mustapha, M. A., Sei-Ichi, S., and Lihan, T. 2009. Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea. – ICES Journal of Marine Science, 66: 1557–1569. Seasonal variation in primary production after a retreat of the sea ice in the scallop-farming region along the Hokkaido coast of the Okhotsk Sea (1998–2004) was determined using satellite images. Annual variability in primary production was caused by variability in the physical processes associated with retreat of the sea ice, advection of the Sōya Warm Current (SWC), and intrusion of the East Sakhalin Current (ESC). Variability in primary production resulted in variability in the Chl a concentration, which was also demonstrated with an empirical orthogonal function (EOF) analysis. Enhancement of Chl a concentration in the frontal area in late spring was demonstrated by the second EOF mode of Chl a concentration (14.2% of variance), in parallel with the generation of a well-developed frontal area resulting from the advection of warm waters of the SWC along the coast in late spring, as indicated by the second EOF mode of sea surface temperature (SST; 1.8% of variance). Elevated Chl a concentration and the presence of cold water of the ESC in late autumn were also highlighted by the third EOF mode of Chl a concentration (9.0% of variance) and SST (1.5% of variance). Prolonged high primary production within the scallop-farming region after spring is supported by the development of a frontal area in summer and strengthening of the ESC in autumn. Article in Journal/Newspaper okhotsk sea Sakhalin Sea ice Oxford University Press ICES Journal of Marine Science 66 7 1557 1569
institution Open Polar
collection Oxford University Press
op_collection_id croxfordunivpr
language English
description Abstract Mustapha, M. A., Sei-Ichi, S., and Lihan, T. 2009. Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea. – ICES Journal of Marine Science, 66: 1557–1569. Seasonal variation in primary production after a retreat of the sea ice in the scallop-farming region along the Hokkaido coast of the Okhotsk Sea (1998–2004) was determined using satellite images. Annual variability in primary production was caused by variability in the physical processes associated with retreat of the sea ice, advection of the Sōya Warm Current (SWC), and intrusion of the East Sakhalin Current (ESC). Variability in primary production resulted in variability in the Chl a concentration, which was also demonstrated with an empirical orthogonal function (EOF) analysis. Enhancement of Chl a concentration in the frontal area in late spring was demonstrated by the second EOF mode of Chl a concentration (14.2% of variance), in parallel with the generation of a well-developed frontal area resulting from the advection of warm waters of the SWC along the coast in late spring, as indicated by the second EOF mode of sea surface temperature (SST; 1.8% of variance). Elevated Chl a concentration and the presence of cold water of the ESC in late autumn were also highlighted by the third EOF mode of Chl a concentration (9.0% of variance) and SST (1.5% of variance). Prolonged high primary production within the scallop-farming region after spring is supported by the development of a frontal area in summer and strengthening of the ESC in autumn.
format Article in Journal/Newspaper
author Mustapha, M. A.
Sei-Ichi, S.
Lihan, T.
spellingShingle Mustapha, M. A.
Sei-Ichi, S.
Lihan, T.
Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
author_facet Mustapha, M. A.
Sei-Ichi, S.
Lihan, T.
author_sort Mustapha, M. A.
title Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
title_short Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
title_full Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
title_fullStr Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
title_full_unstemmed Satellite-measured seasonal variations in primary production in the scallop-farming region of the Okhotsk Sea
title_sort satellite-measured seasonal variations in primary production in the scallop-farming region of the okhotsk sea
publisher Oxford University Press (OUP)
publishDate 2009
url http://dx.doi.org/10.1093/icesjms/fsp142
http://academic.oup.com/icesjms/article-pdf/66/7/1557/29134018/fsp142.pdf
genre okhotsk sea
Sakhalin
Sea ice
genre_facet okhotsk sea
Sakhalin
Sea ice
op_source ICES Journal of Marine Science
volume 66, issue 7, page 1557-1569
ISSN 1095-9289 1054-3139
op_doi https://doi.org/10.1093/icesjms/fsp142
container_title ICES Journal of Marine Science
container_volume 66
container_issue 7
container_start_page 1557
op_container_end_page 1569
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