The article of record as published may be found at http://dx.doi.org/10.1029/90JC02261The aerodynamic roughness for all major types of sea ice is specified on the basis of surface layer measurements from ship and ice floe platforms. Median neutral surface drag coefficients, Cdn×1000, for grease and nilas ice are 0.7 and 1.6. Small, medium, large, and fused pancake ice have Cdn equal to 0.9, 1.6, 2.4, and 1.9. Young ice Cdn ranges from 2.3 to 3.1. Very smooth first‐year or multiyear ice with no pressure ridges has Cdn equal to 1.5. Pack ice has median values of 2.0 and 2.2 for first‐year and multiyear ice. Marginal ice zone ice averages 3.1 and 3.4 (first‐year, multiyear) if unaffected by wave action. Wave‐affected ice has Cdn values of 4.2 ...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic marg...
The bottom topography of ridged sea ice differs greatly from that of other sea-ice types. The form d...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic margi...
Wind profiles collected by satellite-tracked ice beacons and ice surface roughness data by a helicop...
The sea ice surface is characterized by a varying degree of roughness with partly abrupt transitions...
The summer East Greenland Sea marginal ice zone is a region characterized by extreme horizontal vari...
The article of record as published may be found at https://doi.org/10.1121/1.414657Structural charac...
Sea ice features a variety of obstacles to the flow of air and ocean near its surface. The distribut...
Turbulent surface fluxes of momentum and sensible and latent heat as well as surface temperature, a...
Wind profiles collected by satellite-tracked ice beacons deployed on smooth and rough pack ice of th...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic margi...
Wind and temperature profiles in the constant flux layer obtained by tethersonde were used to comput...
Decrease in Arctic Ocean perennial sea-ice has been observed in recent decades. As sea-ice continues...
Over Arctic sea ice, pressure ridges and floe andmelt pond edges all introduce discrete obstructions...
Ice forms in water bodies under the influence of climate, oceanography, and the geography of the sur...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic marg...
The bottom topography of ridged sea ice differs greatly from that of other sea-ice types. The form d...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic margi...
Wind profiles collected by satellite-tracked ice beacons and ice surface roughness data by a helicop...
The sea ice surface is characterized by a varying degree of roughness with partly abrupt transitions...
The summer East Greenland Sea marginal ice zone is a region characterized by extreme horizontal vari...
The article of record as published may be found at https://doi.org/10.1121/1.414657Structural charac...
Sea ice features a variety of obstacles to the flow of air and ocean near its surface. The distribut...
Turbulent surface fluxes of momentum and sensible and latent heat as well as surface temperature, a...
Wind profiles collected by satellite-tracked ice beacons deployed on smooth and rough pack ice of th...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic margi...
Wind and temperature profiles in the constant flux layer obtained by tethersonde were used to comput...
Decrease in Arctic Ocean perennial sea-ice has been observed in recent decades. As sea-ice continues...
Over Arctic sea ice, pressure ridges and floe andmelt pond edges all introduce discrete obstructions...
Ice forms in water bodies under the influence of climate, oceanography, and the geography of the sur...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic marg...
The bottom topography of ridged sea ice differs greatly from that of other sea-ice types. The form d...
Comprehensive aircraft observations are used to characterise surface roughness over the Arctic margi...