11 Works

Oceansat-2 OSCAT Arctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the OSCAT scatterometer on Oceansat-2 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

ERS-2 Antarctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-2 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

ASCAT-A Antarctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the ASCAT scatterometer on Metop-A result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

Oceansat-2 OSCAT Antarctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the OSCAT scatterometer on Oceansat-2 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

Stress equivalent NWP reference wind for scatterometer use

Ad Stoffelen, Jos. De Kloe & Anton Verhoef
This dataset provides surface wind vectors intended to be used as reference for scatterometer and radiometer wind measurements. The wind vectors are taken from the ERA Interim model and have been corrected in two ways. First a "neutral wind correction" is applied to account for atmospheric stratification. Second a "mass density wind correction" is applied to account for the relation between wind surface stress and wind speed. The bicorrected winds are called stress-equivalent winds and...

ERS-1 Antarctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-1 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

QuikSCAT SeaWinds Antarctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the SeaWinds scatterometer on QuikSCAT result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

ASCAT-A Arctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the ASCAT scatterometer on Metop-A result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

ERS-2 Arctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-2 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

QuikSCAT SeaWinds Arctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the SeaWinds scatterometer on QuikSCAT result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

ERS-1 Arctic daily sea ice extent and backscatter maps

Anton Verhoef, Maria Belmonte Rivas & Ad Stoffelen
The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-1 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age...

Registration Year

  • 2018
    11

Resource Types

  • Dataset
    11