BORA - UiB

Bergen Open Research Archive

On the nature of the factors that control spring bloom development at the entrance to the Barents Sea and their interannual variability

Bergen Open Research Archive

Show simple item record

dc.contributor.author Olsen, Are en_US
dc.contributor.author Johannessen, Truls en_US
dc.contributor.author Rey, Francisco en_US
dc.date.accessioned 2004-08-19T09:33:59Z en_US
dc.date.accessioned 2004-08-26T11:59:02Z
dc.date.available 2004-08-19T09:33:59Z en_US
dc.date.available 2004-08-26T11:59:02Z
dc.date.issued 2003-12 en_US
dc.identifier.citation Sarsia 2003 88:(6) en
dc.identifier.issn 0036-4827 en_US
dc.identifier.issn 1503-1128 en_US
dc.identifier.uri http://hdl.handle.net/1956/415
dc.identifier.uri http://dx.doi.org/10.1080/00364820310003145
dc.description.abstract Analysis of data obtained by the Institute of Marine Research, Norway, at their regular surveys of the Fugløya-Bjørnøya section, between the northern tip of Norway and Bear Island, has allowed for an identification of the factors that control spring bloom development in the region, and their interannual variability. In the southern part of the section the bloom starts as the waters become stratified due to a northward spreading of low salinity water from the Norwegian Coastal Current. In the middle part of the section the bloom is initiated when vernal stratification develops due to heating of the ocean surface, and the bloom may develop in either of two directions throughout summer, depending on the prevailing atmospheric pressure gradient over the region. A north to south high to low pressure gradient will direct surface winds to the west. Ekman drift will then be to the north and a wedge of low salinity, low nutrient water will spread out over the region, leading to the termination of the bloom. When the pressure gradient is reversed, winds will blow to the east and intrusion of fresh water into the region will be limited. In these years the bloom appears to follow a classical Atlantic pattern, unable to fully utilize available nitrate and probably terminated due to extensive grazing. The central part of the Barents Sea Opening is thus yet another northern high latitude region where the bloom is subject to substantial interannual variations, potentially affecting higher trophic levels. en_US
dc.format.extent 379513 bytes en_US
dc.format.extent 137 bytes
dc.format.extent 379513 bytes
dc.format.mimetype application/pdf en_US
dc.format.mimetype text/plain
dc.format.mimetype application/pdf
dc.language.iso eng en_US
dc.publisher Taylor & Francis en
dc.title On the nature of the factors that control spring bloom development at the entrance to the Barents Sea and their interannual variability en_US
dc.type Journal article en_US


Files in this item

 

This item appears in the following Collection(s)

Show simple item record

Search BORA


Browse

My Account