Das Klima um Grönland - 1996
Based on air temperature data from three sites of West and East Greenland, on ice charts for the area 54°N, 71°N and 20°W, 70°W, and on CTD profile observations around Greenland, the annual variability of climate is shown. Mean monthly air temperature data from Nuuk/West Greenland reveal the long-te...
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ftaquaticcommons:oai:generic.eprints.org:3798 2023-05-15T15:35:36+02:00 Das Klima um Grönland - 1996 Stein, Manfred 1997 application/pdf http://aquacomm.fcla.edu/3798 http://aquaticcommons.org/3798/ http://aquaticcommons.org/3798/1/97-3_Seite097-102.pdf de ger http://aquaticcommons.org/3798/1/97-3_Seite097-102.pdf Stein, Manfred (1997) Das Klima um Grönland - 1996. Informationen für die Fischwirtschaft aus der Fischereiforschung, 44(3), pp. 97-102. Oceanography Article NonPeerReviewed 1997 ftaquaticcommons 2020-02-27T09:20:32Z Based on air temperature data from three sites of West and East Greenland, on ice charts for the area 54°N, 71°N and 20°W, 70°W, and on CTD profile observations around Greenland, the annual variability of climate is shown. Mean monthly air temperature data from Nuuk/West Greenland reveal the long-term interannual changes of air temperature anomalies. The warming trend which was observed during November, December 1995 was maintained into 1996 for about five months. Thus, spring warming of the near surface water layers, especially on the shallow bank areas off West Greenland has been favoured. As a result of mild air temperatures over most of 1996, sea ice conditions were about normal around Greenland and off eastern Canada. Subsurface observations indicate considerable warming of the 0-200 m water layer off West Greenland. The thermal anomaly of this layer amounts to +1.59K, which is the second highest value on record since the warm 1964 event. The warmer than normal conditions as recorded since November 1995 off East and West Greenland, point at intermediate warming which is characteristic of the second half of the recent decades. The long-term trend of air temperature anomalies off West Greenland points, however, still at cooling, a trend which is persistent since the early 1970s. As the potential driving mechanism for the intermediate warming in the Labrador Sea area, the sea level air pressure gradient between Iceland and the Azores is identified. The 1996 value of this gradient, the North Atlantic Oscillation (NAO) Index, is strongly negative and this represents the flow of mild air masses from the midlatitude Atlantic Ocean to the Greenland/Labrador Sea region. Accordingly, air temperature anomalies indicated unusual warming during the month of February which amounted to >2K in the region of Baffin Land, Labrador and Greenland. Article in Journal/Newspaper Baffin East Greenland Greenland Grönland Iceland Labrador Sea North Atlantic North Atlantic oscillation Nuuk Sea ice International Association of Aquatic and Marine Science Libraries and Information Centers (IAMSLIC): Aquatic Commons Canada Greenland Nuuk ENVELOPE(-52.150,-52.150,68.717,68.717) |
institution |
Open Polar |
collection |
International Association of Aquatic and Marine Science Libraries and Information Centers (IAMSLIC): Aquatic Commons |
op_collection_id |
ftaquaticcommons |
language |
German |
topic |
Oceanography |
spellingShingle |
Oceanography Stein, Manfred Das Klima um Grönland - 1996 |
topic_facet |
Oceanography |
description |
Based on air temperature data from three sites of West and East Greenland, on ice charts for the area 54°N, 71°N and 20°W, 70°W, and on CTD profile observations around Greenland, the annual variability of climate is shown. Mean monthly air temperature data from Nuuk/West Greenland reveal the long-term interannual changes of air temperature anomalies. The warming trend which was observed during November, December 1995 was maintained into 1996 for about five months. Thus, spring warming of the near surface water layers, especially on the shallow bank areas off West Greenland has been favoured. As a result of mild air temperatures over most of 1996, sea ice conditions were about normal around Greenland and off eastern Canada. Subsurface observations indicate considerable warming of the 0-200 m water layer off West Greenland. The thermal anomaly of this layer amounts to +1.59K, which is the second highest value on record since the warm 1964 event. The warmer than normal conditions as recorded since November 1995 off East and West Greenland, point at intermediate warming which is characteristic of the second half of the recent decades. The long-term trend of air temperature anomalies off West Greenland points, however, still at cooling, a trend which is persistent since the early 1970s. As the potential driving mechanism for the intermediate warming in the Labrador Sea area, the sea level air pressure gradient between Iceland and the Azores is identified. The 1996 value of this gradient, the North Atlantic Oscillation (NAO) Index, is strongly negative and this represents the flow of mild air masses from the midlatitude Atlantic Ocean to the Greenland/Labrador Sea region. Accordingly, air temperature anomalies indicated unusual warming during the month of February which amounted to >2K in the region of Baffin Land, Labrador and Greenland. |
format |
Article in Journal/Newspaper |
author |
Stein, Manfred |
author_facet |
Stein, Manfred |
author_sort |
Stein, Manfred |
title |
Das Klima um Grönland - 1996 |
title_short |
Das Klima um Grönland - 1996 |
title_full |
Das Klima um Grönland - 1996 |
title_fullStr |
Das Klima um Grönland - 1996 |
title_full_unstemmed |
Das Klima um Grönland - 1996 |
title_sort |
das klima um grönland - 1996 |
publishDate |
1997 |
url |
http://aquacomm.fcla.edu/3798 http://aquaticcommons.org/3798/ http://aquaticcommons.org/3798/1/97-3_Seite097-102.pdf |
long_lat |
ENVELOPE(-52.150,-52.150,68.717,68.717) |
geographic |
Canada Greenland Nuuk |
geographic_facet |
Canada Greenland Nuuk |
genre |
Baffin East Greenland Greenland Grönland Iceland Labrador Sea North Atlantic North Atlantic oscillation Nuuk Sea ice |
genre_facet |
Baffin East Greenland Greenland Grönland Iceland Labrador Sea North Atlantic North Atlantic oscillation Nuuk Sea ice |
op_relation |
http://aquaticcommons.org/3798/1/97-3_Seite097-102.pdf Stein, Manfred (1997) Das Klima um Grönland - 1996. Informationen für die Fischwirtschaft aus der Fischereiforschung, 44(3), pp. 97-102. |
_version_ |
1766365943493033984 |