ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION

Ecological observations of the coloured layer in the sea ice were carried out at Syowa Station from March 1967 to January 1968 The results obtained are as follows 1 A brown layer was formed at the bottom of the new ice in March 1967 It remained till the early part of January 1968 2 The thickness of...

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Main Author: Takao HOSHIAI
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1969
Subjects:
Online Access:https://doi.org/10.15094/00007544
https://doaj.org/article/142485ded8fa499e8d3dc5e3efa75b72
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spelling ftdoajarticles:oai:doaj.org/article:142485ded8fa499e8d3dc5e3efa75b72 2023-05-15T18:17:37+02:00 ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION Takao HOSHIAI 1969-03-01T00:00:00Z https://doi.org/10.15094/00007544 https://doaj.org/article/142485ded8fa499e8d3dc5e3efa75b72 EN JA eng jpn National Institute of Polar Research https://doi.org/10.15094/00007544 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00007544 0085-7289 2432-079X https://doaj.org/article/142485ded8fa499e8d3dc5e3efa75b72 Antarctic Record, Iss 34, Pp 60-72 (1969) Geography (General) G1-922 article 1969 ftdoajarticles https://doi.org/10.15094/00007544 2022-12-31T05:34:25Z Ecological observations of the coloured layer in the sea ice were carried out at Syowa Station from March 1967 to January 1968 The results obtained are as follows 1 A brown layer was formed at the bottom of the new ice in March 1967 It remained till the early part of January 1968 2 The thickness of the coloured layer was 2 cm in March and grew to 20 cm by May The brown colour faded with the lapse of time The chlorophyll-a concentration was high in the coloured layer, especially in the deep-brown part The chlorophyll-a conccntiation increased between March and April, but thereafter it decreased gradually 3 Horizontal extent of the coloured layer was not very wide, being 50m × 150m 4 The vertical situation and the thickness of the coloured layer varied from place to place However, it was geneially recognized that chlorinity and pH value were high in the upper part of the coloured layer and decreased in the lower part 5 Seasonal variation of chlorinity in the coloured layer was relatively remarkable Chlorinity was high between October and December 6 Seasonal change of pH value in the coloured layer was more remarkable than in the colourless part Between the latter part of December and the caily part of January pH value was exuemely high 7 On the 24th ol December, another coloured layer appeared at the bottom of the sea ice, accompanied by some increase of chlorinity and pH It disappeared by the 5th of January. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Syowa Station
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Takao HOSHIAI
ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
topic_facet Geography (General)
G1-922
description Ecological observations of the coloured layer in the sea ice were carried out at Syowa Station from March 1967 to January 1968 The results obtained are as follows 1 A brown layer was formed at the bottom of the new ice in March 1967 It remained till the early part of January 1968 2 The thickness of the coloured layer was 2 cm in March and grew to 20 cm by May The brown colour faded with the lapse of time The chlorophyll-a concentration was high in the coloured layer, especially in the deep-brown part The chlorophyll-a conccntiation increased between March and April, but thereafter it decreased gradually 3 Horizontal extent of the coloured layer was not very wide, being 50m × 150m 4 The vertical situation and the thickness of the coloured layer varied from place to place However, it was geneially recognized that chlorinity and pH value were high in the upper part of the coloured layer and decreased in the lower part 5 Seasonal variation of chlorinity in the coloured layer was relatively remarkable Chlorinity was high between October and December 6 Seasonal change of pH value in the coloured layer was more remarkable than in the colourless part Between the latter part of December and the caily part of January pH value was exuemely high 7 On the 24th ol December, another coloured layer appeared at the bottom of the sea ice, accompanied by some increase of chlorinity and pH It disappeared by the 5th of January.
format Article in Journal/Newspaper
author Takao HOSHIAI
author_facet Takao HOSHIAI
author_sort Takao HOSHIAI
title ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
title_short ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
title_full ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
title_fullStr ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
title_full_unstemmed ECOLOGICAL OBSERVATIONS OF THE COLOURED LAYER OF THE SEA ICE AT SYOWA STATION
title_sort ecological observations of the coloured layer of the sea ice at syowa station
publisher National Institute of Polar Research
publishDate 1969
url https://doi.org/10.15094/00007544
https://doaj.org/article/142485ded8fa499e8d3dc5e3efa75b72
geographic Syowa Station
geographic_facet Syowa Station
genre Sea ice
genre_facet Sea ice
op_source Antarctic Record, Iss 34, Pp 60-72 (1969)
op_relation https://doi.org/10.15094/00007544
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00007544
0085-7289
2432-079X
https://doaj.org/article/142485ded8fa499e8d3dc5e3efa75b72
op_doi https://doi.org/10.15094/00007544
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