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Features of the physical oceanographic conditions of the Barents Sea
- H. Loeng
- Environmental Science
- 1 December 1991
The Barents Sea is a shallow continental shelf sea. Generally, the physical conditions are determined by three main water masses: Coastal Water, (North) Atlantic Water, and Arctic Water. These three…
Atlantic Water flow through the Barents and Kara Seas
- U. Schauer, H. Loeng, B. Rudels, V. Ozhigin, Wolfgang Dieck
- Environmental Science
- 1 December 2002
Volume and Heat Transports to the Arctic Ocean Via the Norwegian and Barents Seas
- Ø. Skagseth, T. Furevik, V. Ozhigin
- Environmental Science
- 2008
The main aim of this paper has been to present a holistic view of the Atlantic water flow along the Norwegian Coast and into the Barents Sea. It has focused on the period starting in the mid-1990s,…
Water fluxes through the Barents Sea
- H. Loeng, V. Ozhigin, B. Ådlandsvik
- Environmental Science
- 1 June 1997
The physical oceanographic conditions in the Barents Sea depend mainly on the variability in the Atlantic inflow from the Norwegian Sea and the inflow of Arctic water from the Kara Sea and the Arctic…
The seasonal cycle in the Atlantic transport to the Barents Sea during the years 1997–2001
- R. Ingvaldsen, L. Asplin, H. Loeng
- Environmental Science
- 1 June 2004
An overview of the ecosystems of the Barents and Norwegian Seas and their response to climate variability
- H. Loeng, K. Drinkwater
- Environmental Science
- 1 November 2007
Mass and heat transports in the NE Barents Sea: Observations and models
- T. Gammelsrød, Øyvind Leikvin, V. Lien, W. Budgell, H. Loeng, W. Maslowski
- Environmental Science
- 2009
Covariability in early growth and year-class strength of Barents Sea cod, haddock, and herring: the environmental link
- Geir Ottersen, H. Loeng
- Environmental Science
- 1 April 2000
TLDR
Reversal of the 1960s to 1990s freshening trend in the northeast North Atlantic and Nordic Seas
- N. P. Holliday, S. Hughes, W. Walczowski
- Environmental Science
- 1 February 2008
Hydrographic time series in the northeast North Atlantic and Nordic Seas show that the freshening trend of the 1960s–1990s has completely reversed in the upper ocean. Since the 1990s temperature and…
Velocity field of the western entrance to the Barents Sea
- R. Ingvaldsen, L. Asplin, H. Loeng
- Environmental Science
- 1 March 2004
[1] By the use of 4-year long records from moored current meters between 71°30′N and 73°30′N of the western entrance to the Barents Sea, the velocity field of the Atlantic inflow is examined. The…
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