The Arctic marine ecosystem is shaped by the seasonality of the solar cycle, spanning from 24-h light at the sea surface in summer to 24-h darkness in winter. The amount of light available for under-ice ecosystems is the result of different physical and biological processes that affect its path through atmosphere, snow, sea ice and water. In this article, we review the present state of knowledge of the abiotic (clouds, sea ice, snow, suspended matter) and biotic (sea ice algae and phytoplankton) controls on the underwater light field. We focus on how the available light affects the seasonal cycle of primary production (sympagic and pelagic) and discuss the sensitivity of ecosystems to changes in the light field based on model simulations. L...
Optically active water constituents attenuate solar radiation and hence affect the vertical distribu...
The growth of phytoplankton at high latitudes was generally thought to begin in open waters of the m...
International audienceDuring summer, phytoplankton can bloom in the Arctic Ocean, both in open water...
This study was supported by the Changing Arctic Ocean projects EcoLight (03V01465), Arctic PRIZE (NE...
The Arctic marine ecosystem is shaped by the seasonality of the solar cycle, spanning from 24-h ligh...
In July 2011, the observation of a massive phytoplankton bloom underneath a sea ice–covered region o...
International audienceThe decline of sea-ice thickness, area, and volume due to the transition from ...
Observations of the seasonal light field in the upper Arctic Ocean are critical to understanding the...
International audienceArctic sea ice is shifting from a year-round to a seasonal sea ice cover. This...
Arctic sea ice is shifting from a year-round to a seasonal sea ice cover. This substantial transform...
This dataset is linked to this manuscript entitled "Environmental drivers of under-ice phytoplankton...
The ice-covered seas of the Arctic have two major types of primary producers; phytoplankton growing ...
The Arctic is no longer a region dominated by thick multi-year ice (MYI), but by thinner, more dynam...
Optically active water constituents attenuate solar radiation and hence affect the vertical distribu...
The growth of phytoplankton at high latitudes was generally thought to begin in open waters of the m...
International audienceDuring summer, phytoplankton can bloom in the Arctic Ocean, both in open water...
This study was supported by the Changing Arctic Ocean projects EcoLight (03V01465), Arctic PRIZE (NE...
The Arctic marine ecosystem is shaped by the seasonality of the solar cycle, spanning from 24-h ligh...
In July 2011, the observation of a massive phytoplankton bloom underneath a sea ice–covered region o...
International audienceThe decline of sea-ice thickness, area, and volume due to the transition from ...
Observations of the seasonal light field in the upper Arctic Ocean are critical to understanding the...
International audienceArctic sea ice is shifting from a year-round to a seasonal sea ice cover. This...
Arctic sea ice is shifting from a year-round to a seasonal sea ice cover. This substantial transform...
This dataset is linked to this manuscript entitled "Environmental drivers of under-ice phytoplankton...
The ice-covered seas of the Arctic have two major types of primary producers; phytoplankton growing ...
The Arctic is no longer a region dominated by thick multi-year ice (MYI), but by thinner, more dynam...
Optically active water constituents attenuate solar radiation and hence affect the vertical distribu...
The growth of phytoplankton at high latitudes was generally thought to begin in open waters of the m...
International audienceDuring summer, phytoplankton can bloom in the Arctic Ocean, both in open water...