Eva Falck
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View article: An emerging pathway of Atlantic Water to the Barents Sea through the Svalbard Archipelago: drivers and variability
An emerging pathway of Atlantic Water to the Barents Sea through the Svalbard Archipelago: drivers and variability Open
The Barents Sea, an important component of the Arctic Ocean, is experiencing changes in its ocean currents, stratification, sea ice variability, and marine ecosystems. Inflowing Atlantic Water (AW) is a key driver of these changes. As AW p…
View article: Comment on egusphere-2023-3080
Comment on egusphere-2023-3080 Open
Abstract. The Barents Sea, an important component of the Arctic Ocean, is experiencing shifts in ocean currents, stratification, sea-ice variability, and marine ecosystems. Inflowing Atlantic Water (AW) is known to be a key driver of chang…
View article: Review on the manuscript egusphere-2023-3080
Review on the manuscript egusphere-2023-3080 Open
Abstract. The Barents Sea, an important component of the Arctic Ocean, is experiencing shifts in ocean currents, stratification, sea-ice variability, and marine ecosystems. Inflowing Atlantic Water (AW) is known to be a key driver of chang…
View article: An emerging pathway of Atlantic Water to the Barents Sea through the Svalbard Archipelago: drivers and variability
An emerging pathway of Atlantic Water to the Barents Sea through the Svalbard Archipelago: drivers and variability Open
The Barents Sea, an important component of the Arctic Ocean, is experiencing shifts in ocean currents, stratification, sea-ice variability, and marine ecosystems. Inflowing Atlantic Water (AW) is known to be a key driver of change. Althoug…
View article: Wind forcing and tides mediate transport of ocean heat from Storfjordrenna to the Arctic domain of the Barents Sea
Wind forcing and tides mediate transport of ocean heat from Storfjordrenna to the Arctic domain of the Barents Sea Open
The Barents Sea is undergoing changes with impacts on the physical environment, e.g., the seasonal sea ice formation and extent and with large consequences for the ecosystems. There are knowledge-gaps concerning the complex pathways of Atl…
View article: Waterside convection and stratification control methane spreading in supersaturated Arctic fjords (Spitsbergen)
Waterside convection and stratification control methane spreading in supersaturated Arctic fjords (Spitsbergen) Open
Seasonally ice covered in the past, the fjords in West Spitsbergen turn into being perennially ice free in the present. This feedback to Arctic amplification of global warming changes gas fluxes at the atmosphere-ocean interface. Furthermo…
View article: SS-MSC2 Process cruise/mooring service 2020
SS-MSC2 Process cruise/mooring service 2020 Open
The cruise GOS 2020113 (6 October 2020 Longyearbyen, 27 October 2020 Tromsø) aboard the Research Vessel G.O. SARS is a mooring service/deployment and process studies cruise of the Nansen LEGACY project.
View article: Flow over a snow-water-snow surface in the high Arctic, Svalbard: Turbulent fluxes and comparison of observation techniques
Flow over a snow-water-snow surface in the high Arctic, Svalbard: Turbulent fluxes and comparison of observation techniques Open
From observations in a High Arctic valley and ice-free fjord in Svalbard during March and April 2013 we show that, while some caution needs to be applied, ordinary slow-response instruments placed over a snow-water-snow surface can be effe…
View article: Physical Process Cruise 2018
Physical Process Cruise 2018 Open
The cruise KH 2018-709 aboard the Research Vessel Kronprins Haakon was the second process cruise of the project the Nansen Legacy. The cruise contributed to task T1-2, on process studies to investigate the atmospheric, oceanographic, radia…
View article: Ocean Mixing Process Study 2018
Ocean Mixing Process Study 2018 Open
The cruise KB 2018616 aboard the Research Vessel Kristine Bonnevie was the first research cruise of the Nansen Legacy project. The cruise aimed at collecting ocean stratification, currents, and microstructure profiles along selected transe…
View article: UAK 2020: Research School in the Barents Sea with KV Svalbard
UAK 2020: Research School in the Barents Sea with KV Svalbard Open
The project brings together leading researchers, educators and young scientists working on selected Arctic science topics. The UAK researcher school on board KV Svalbard during 20-30 June aimed to address the different steps in the data de…
View article: Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation - an indicator for climate change in the European Arctic
Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation - an indicator for climate change in the European Arctic Open
<p>Isfjorden, a broad Arctic fjord in western Spitsbergen, has shown significant changes in hydrography and inflow of Atlantic Water (AW) the last decades that only recently have been observed in the Arctic Ocean north of Svalbard. V…
View article: Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Open
Time series of the marine CO2 system and related parameters at the IsA Station, by Adventfjorden, Svalbard, were investigated between March 2015 and November 2017. The physical and biogeochemical processes that govern changes in total alka…
View article: Enhanced Air–Sea Exchange of Heat and Carbon Dioxide Over a High Arctic Fjord During Unstable Very-Close-to-Neutral Conditions
Enhanced Air–Sea Exchange of Heat and Carbon Dioxide Over a High Arctic Fjord During Unstable Very-Close-to-Neutral Conditions Open
Eddy-covariance measurements made in the marine atmospheric boundary layer above a high Arctic fjord (Adventfjorden, Svalbard) are analyzed. When conditions are unstable, but close to neutral −0.1 &lt; z/L &lt; 0, where z is the he…
View article: Temporal Variability in Surface Water <i>p</i>CO<sub>2</sub> in Adventfjorden (West Spitsbergen) With Emphasis on Physical and Biogeochemical Drivers
Temporal Variability in Surface Water <i>p</i>CO<sub>2</sub> in Adventfjorden (West Spitsbergen) With Emphasis on Physical and Biogeochemical Drivers Open
Seasonal and interannual variability in surface water partial pressure of CO 2 ( p CO 2 ) and air‐sea CO 2 fluxes from a West Spitsbergen fjord (IsA Station, Adventfjorden) are presented, and the associated driving forces are evaluated. Ma…
View article: Deliverable 2.1 Report on present observing capacities and gaps: ocean and sea ice observing system
Deliverable 2.1 Report on present observing capacities and gaps: ocean and sea ice observing system Open
A major goal of WP2: “Exploitation of existing observing systems” is to analyze strengths, weaknesses, gaps in spatial/temporal coverage, and missing monitoring parameters of the existing observation networks and databases in relation to t…
View article: Interannual variability in hydrography and water mass distribution in Hornsund, an Arctic fjord in Svalbard
Interannual variability in hydrography and water mass distribution in Hornsund, an Arctic fjord in Svalbard Open
Progressing warming in the Arctic and increased extreme weather events can significantly influence the hydrography of Svalbard fjords, leading to changes towards more Atlantic-type waters in the fjords. In this paper, we look into the hydr…
View article: Air‐sea gas transfer in high Arctic fjords
Air‐sea gas transfer in high Arctic fjords Open
In Arctic fjords and high‐latitude seas, strong surface cooling dominates during a large part of the year, generating water‐side convection ( w * w ) and enhanced turbulence in the water. These regions are key areas for the global carbon c…
View article: Norwegian fisheries in the Svalbard zone since 1980. Regulations, profitability and warming waters affect landings
Norwegian fisheries in the Svalbard zone since 1980. Regulations, profitability and warming waters affect landings Open
The Svalbard archipelago in the High Arctic is influenced by cold Arctic water masses from the north-east and the warm West Spitsbergen Current flowing northwards along its western coast. The eastern waters and the fjords are normally froz…