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- Publications
- Influence
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… Expand
Atlantic Water flow through the Barents and Kara Seas
- U. Schauer, H. Loeng, Bert Rudels, V. Ozhigin, Wolfgang Dieck
- Geology
- 1 December 2002
Abstract The pathway and transformation of water from the Norwegian Sea across the Barents Sea and through the St. Anna Trough are documented from hydrographic and current measurements of the 1990s.… Expand
Volume and Heat Transports to the Arctic Ocean Via the Norwegian and Barents Seas
- Ø. Skagseth, T. Furevik, +4 authors Vladimir Ozhigin
- Geology
- 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,… Expand
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
Abstract The seasonal cycle in the Atlantic inflow to the Barents Sea is investigated by using 4-year long records from moored current meters, additional moorings of shorter duration, and… Expand
Water fluxes through the Barents Sea
- H. Loeng, Vladimir Ozhigin, B. Ådlandsvik
- Materials 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… Expand
An overview of the ecosystems of the Barents and Norwegian Seas and their response to climate variability
- H. Loeng, K. Drinkwater
- Geology
- 1 November 2007
The principal features of the marine ecosystems in the Barents and Norwegian Seas and some of their responses to climate variations are described. The physical oceanography is dominated by the influx… Expand
Mass and heat transports in the NE Barents Sea: Observations and models
- Tor Gammelsrød, Øyvind Leikvin, V. Lien, W. P. Budgell, H. Loeng, W. Maslowski
- Geology
- 2009
Abstract The strait between Novaya Zemlya and Frans Josef Land, here called the Barents Sea Exit (BSX) is investigated using data obtained from a current-meter array deployed in 1991–1992, and two… Expand
Covariability in early growth and year-class strength of Barents Sea cod, haddock, and herring: the environmental link
- Geir Ottersen, H. Loeng
- Biology
- 1 April 2000
We address the hypothesis that survival of a cohort is directly related to growth rates during the pre-recruit period for marine fish. This hypothesis is widely accepted, but supporting field… Expand
Structure, biomass distribution, and energetics of the pelagic ecosystem in the Barents Sea: A synopsis
- E. Sakshaug, A. Bjørge, B. Gulliksen, H. Loeng, Fritjof Mehlum
- Biology
- Polar Biology
- 1 August 1994
Biomass distribution and energetics of trophic levels in the pelagic ecosystem of the Barents Sea are presented as averages over several years for the whole Barents Sea using data from the research… Expand
Velocity field of the western entrance to the Barents Sea
- R. Ingvaldsen, L. Asplin, H. Loeng
- Geology
- 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… Expand