Selected physical, biological and biogeochemical implications of a rapidly changing Arctic Marginal Ice Zone
Abstract The Marginal Ice Zone (MIZ) of the Arctic Ocean is changing rapidly due to a
warming Arctic climate with commensurate reductions in sea ice extent and thickness. This …
warming Arctic climate with commensurate reductions in sea ice extent and thickness. This …
A multi-decade record of high-quality fCO2 data in version 3 of the Surface Ocean CO2 Atlas (SOCAT)
DCE Bakker, B Pfeil, CS Landa, N Metzl… - Earth System …, 2016 - essd.copernicus.org
The Surface Ocean CO 2 Atlas (SOCAT) is a synthesis of quality-controlled fCO 2 (fugacity of
carbon dioxide) values for the global surface oceans and coastal seas with regular updates …
carbon dioxide) values for the global surface oceans and coastal seas with regular updates …
[HTML][HTML] Arctic Ocean outflow shelves in the changing Arctic: A review and perspectives
Over the past decade or so, international research efforts, many of which were part of the
International Polar Year, have accrued our understanding of the Arctic outflow shelves. The …
International Polar Year, have accrued our understanding of the Arctic outflow shelves. The …
The Arctic Ocean marine carbon cycle: evaluation of air-sea CO2 exchanges, ocean acidification impacts and potential feedbacks
At present, although seasonal sea-ice cover mitigates atmosphere-ocean gas exchange, the
Arctic Ocean takes up carbon dioxide (CO 2) on the order of− 66 to− 199 Tg C year− 1 (10 …
Arctic Ocean takes up carbon dioxide (CO 2) on the order of− 66 to− 199 Tg C year− 1 (10 …
Decrease in the CO2 Uptake Capacity in an Ice-Free Arctic Ocean Basin
It has been predicted that the Arctic Ocean will sequester much greater amounts of carbon
dioxide (CO2) from the atmosphere as a result of sea ice melt and increasing primary …
dioxide (CO2) from the atmosphere as a result of sea ice melt and increasing primary …
Intraspecific variability in the response of bloom‐forming marine microalgae to changed climate conditions
Phytoplankton populations can display high levels of genetic diversity that, when reflected
by phenotypic variability, may stabilize a species response to environmental changes. We …
by phenotypic variability, may stabilize a species response to environmental changes. We …
Transcriptome‐wide polymorphisms of red abalone (Haliotis rufescens) reveal patterns of gene flow and local adaptation
P De Wit, SR Palumbi - Molecular Ecology, 2013 - Wiley Online Library
Global climate change is projected to accelerate during the next century, altering oceanic
patterns in temperature, p H and oxygen concentrations. Documenting patterns of genetic …
patterns in temperature, p H and oxygen concentrations. Documenting patterns of genetic …
Calcium carbonate saturation in the surface water of the Arctic Ocean: undersaturation in freshwater influenced shelves
M Chierici, A Fransson - Biogeosciences, 2009 - bg.copernicus.org
In the summer of 2005, we sampled surface water and measured pH and total alkalinity (AT)
underway aboard IB Oden along the Northwest Passage from Cape Farewell (South …
underway aboard IB Oden along the Northwest Passage from Cape Farewell (South …
Sea ice contribution to the air–sea CO2 exchange in the Arctic and Southern Oceans
Although salt rejection from sea ice is a key process in deep-water formation in ice-covered
seas, the concurrent rejection of CO2 and the subsequent effect on air–sea CO2 exchange …
seas, the concurrent rejection of CO2 and the subsequent effect on air–sea CO2 exchange …
Seasonality of the physical and biogeochemical hydrography in the inflow to the Arctic Ocean through Fram Strait
Eastern Fram Strait and the shelf slope region north of Svalbard is dominated by the
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …