Now showing items 101-110 of 445
Argo Profiling Floats in the Nordic Seas: Deep-water circulation, hydrography and comparisons to the TOPAZ model
(The University of Bergen, 2006-05)
Ein modellstudie av samanhengen mellom reflektert radiansved toppen av atmosfæra og globalstråling ved bakken
(The University of Bergen, 2001)
Stormbaner ved ulikt isdekke i Labradorhavet
(The University of Bergen, 2002)
The seaice in the Arctic is an important component in the climate system, and plays an important role by interacting with atmospheric circulation trough surface-albedo and energy-exchanges. To study the atmospheric response ...
Arctic Ocean carbon biogeochemistry under climate change and ocean acidification
(The University of Bergen, 2013-05-10)
Human-induced CO2 emissions to the atmosphere cause climate change and ocean acidification. The strongest indicators of climate change and ocean acidification are expected to be found in the Arctic Ocean (AO). The AO ...
Metrics to assess the mitigation of global warming by carbon capture and storage in the ocean and in geological reservoirs
(American Geophysical Union, 2004-09-18)
Different metrics to assess mitigation of global warming by carbon capture and storage are discussed. The climatic impact of capturing 30% of the anthropogenic carbon emission and its storage in the ocean or in ...
Small-scale turbulence dynamics under sea surface gravity waves
(The University of Bergen, 2014-08-20)
The ocean surface is a complex boundary where air-sea fluxes of mass, momentum and energy take place. The processes at this dynamic interface are of great importance in the coupled atmosphere-ocean system. The coupling ...
Modeling the dynamics and drift of icebergs in the Barents Sea
(The University of Bergen, 2010-10-22)
Surface wave effects in the upper ocean and consequences for biological modeling
(The University of Bergen, 2014-03-21)
Effects of surface gravity waves on particle transport and currents in the upper ocean are studied using field observations and numerical models. Knowledge on upper ocean particle drift is needed for plankton transport ...
Sensor movement correction for direct turbulence measurements in the marine atmospheric boundary layer
Understanding of the turbulent exchange processes between the ocean and the overlying atmosphere is essential for wind shear and turbulence structure of the Marine Atmospheric Boundary Layer (MABL). This is highly relevant ...
A quantitative description of the West Spitsbergen Current by combining hydrography, altimetry and in-situ current meters
(The University of Bergen and University Centre in Svalbard, UNIS, 2014-06-02)
In a warming Arctic Ocean (AO) it is important to study its main source of oceanic heat and salt. Here, seasonal climatological sections of the West Spitsbergen Current (WSC) across 78.83°N have been constructed using ...