Turbulent exchange processes in the atmospheric boundary layer (ABL) over the polar ocean regions are strongly influenced by the characteristics of the surface. While thick sea ice minimizes turbulent energy transport by its insulating effect, a large part of it can occur through leads, which are elongated open-water channels in sea ice. Especially between late fall and spring, temperature differences between the near-surface ABL and the surface of leads can amount up to 40K causing strong convective plumes over the leads. Our aim is to improve the understanding of the main processes that drive turbulent transport in the convective plumes by means of developing turbulence parametrizations for such a strongly heterogeneous ABL. We model t...
International audienceLeads are linear-like structures of open water within the sea ice cover that d...
Climate change is especially pronounced over the Arctic Ocean, where the atmosphere warmed twice as ...
The importance of leads, sea ice motion, and frazil ice on the wintertime ocean\ud Boundary layer wa...
The polar ocean regions are characterised by a large variety of interactions between sea ice surface...
A non‐eddy‐resolving microscale model is applied to simulate convection over three different leads (...
A new turbulence parametrization is developed for a non-eddy-resolving microscale model to study the...
In the polar regions, the atmospheric boundary layer (ABL) characteristics are strongly influenced b...
The data set consists of model data from simulations of the atmospheric flow over different configur...
Leads are elongated channels in sea ice which play animportant role for theheat andmoisture exchang...
Thick sea ice on the polar oceans acts as a good insulator between the cold atmosphere and the relat...
We investigate the atmospheric boundary layer (ABL) structure over the marginal sea ice zone (MIZ) u...
Even in the central polar ocean regions, the sea ice cover cannot be regarded as a homogeneous and ...
Climate change is especially pronounced over the Arctic Ocean, where the atmosphere warmed twice as ...
The evolution of the atmospheric boundary layer (ABL) during warm-air advection over sea ice in the ...
The evolution of the atmospheric boundary layer (ABL) during warm-air advection over sea ice in the ...
International audienceLeads are linear-like structures of open water within the sea ice cover that d...
Climate change is especially pronounced over the Arctic Ocean, where the atmosphere warmed twice as ...
The importance of leads, sea ice motion, and frazil ice on the wintertime ocean\ud Boundary layer wa...
The polar ocean regions are characterised by a large variety of interactions between sea ice surface...
A non‐eddy‐resolving microscale model is applied to simulate convection over three different leads (...
A new turbulence parametrization is developed for a non-eddy-resolving microscale model to study the...
In the polar regions, the atmospheric boundary layer (ABL) characteristics are strongly influenced b...
The data set consists of model data from simulations of the atmospheric flow over different configur...
Leads are elongated channels in sea ice which play animportant role for theheat andmoisture exchang...
Thick sea ice on the polar oceans acts as a good insulator between the cold atmosphere and the relat...
We investigate the atmospheric boundary layer (ABL) structure over the marginal sea ice zone (MIZ) u...
Even in the central polar ocean regions, the sea ice cover cannot be regarded as a homogeneous and ...
Climate change is especially pronounced over the Arctic Ocean, where the atmosphere warmed twice as ...
The evolution of the atmospheric boundary layer (ABL) during warm-air advection over sea ice in the ...
The evolution of the atmospheric boundary layer (ABL) during warm-air advection over sea ice in the ...
International audienceLeads are linear-like structures of open water within the sea ice cover that d...
Climate change is especially pronounced over the Arctic Ocean, where the atmosphere warmed twice as ...
The importance of leads, sea ice motion, and frazil ice on the wintertime ocean\ud Boundary layer wa...