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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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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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 |
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Open Polar |
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Oxford University Press |
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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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1810470041824526336 |