Early-summer melt pond fraction is predicted using late-winter C-band backscatter of snow-covered first-year sea ice. Aerial photographs were acquired during an early-summer 2012 field campaign in Resolute Passage, Nunavut, Canada, on smooth first-year sea ice to estimate the melt pond fraction. RADARSAT-2 Synthetic Aperture Radar (SAR) data were acquired over the study area in late winter prior to melt onset. Correlations between the melt pond fractions and late-winter linear and polarimetric SAR parameters and texture measures derived from the SAR parameters are utilized to develop multivariate regression models that predict melt pond fractions. The results demonstrate substantial capability of the regression models to predict melt pond f...
Melt pond coverage of sea ice in the High Arctic was observed for a period of 28 days: from 24 June ...
Ku- and C-band spaceborne scatterometer sigma nought (σ°) backscatter data of snow covered...
ii This study examines the utility of fully polarimetric C-and SAR parameters and three-component sc...
Early-summer melt pond fraction is predicted using late-winter C-band backscatter of snow-covered fi...
In this study we examine the relationship between sea ice melt pond fraction and two polarimetric C-...
Melt ponds, a common feature on Arctic sea ice, absorb most of the incoming solar radiation and have...
Utilizing synthetic aperture radar (SAR) data to understand and map sea ice roughness is an active a...
The accuracy of microwave radiometer ice concentration (IC) retrievals in the Arctic is degraded by ...
The accuracy of microwave radiometer ice concentration (IC) retrievals in the Arctic is degraded by ...
In this thesis, we explore the possibilities and limitations of using space-borne multi-polarimetric...
C-band synthetic aperture radar (SAR) is widely used for sea ice monitoring and operational activiti...
The Arctic sea ice cover has decreased strongly in extent, thickness, volume and age in recent decad...
AbstractDifferentiating between first-year ice (FYI) and multi-year ice (MYI) in C-band synthetic ap...
Melt ponds, a common feature on Arctic sea ice, absorb most of the incoming solar radiation and have...
This data collection presents snow depth, ice thickness and RADARSAT-2 (RS2) and TerraSAR-X (TSX) ba...
Melt pond coverage of sea ice in the High Arctic was observed for a period of 28 days: from 24 June ...
Ku- and C-band spaceborne scatterometer sigma nought (σ°) backscatter data of snow covered...
ii This study examines the utility of fully polarimetric C-and SAR parameters and three-component sc...
Early-summer melt pond fraction is predicted using late-winter C-band backscatter of snow-covered fi...
In this study we examine the relationship between sea ice melt pond fraction and two polarimetric C-...
Melt ponds, a common feature on Arctic sea ice, absorb most of the incoming solar radiation and have...
Utilizing synthetic aperture radar (SAR) data to understand and map sea ice roughness is an active a...
The accuracy of microwave radiometer ice concentration (IC) retrievals in the Arctic is degraded by ...
The accuracy of microwave radiometer ice concentration (IC) retrievals in the Arctic is degraded by ...
In this thesis, we explore the possibilities and limitations of using space-borne multi-polarimetric...
C-band synthetic aperture radar (SAR) is widely used for sea ice monitoring and operational activiti...
The Arctic sea ice cover has decreased strongly in extent, thickness, volume and age in recent decad...
AbstractDifferentiating between first-year ice (FYI) and multi-year ice (MYI) in C-band synthetic ap...
Melt ponds, a common feature on Arctic sea ice, absorb most of the incoming solar radiation and have...
This data collection presents snow depth, ice thickness and RADARSAT-2 (RS2) and TerraSAR-X (TSX) ba...
Melt pond coverage of sea ice in the High Arctic was observed for a period of 28 days: from 24 June ...
Ku- and C-band spaceborne scatterometer sigma nought (σ°) backscatter data of snow covered...
ii This study examines the utility of fully polarimetric C-and SAR parameters and three-component sc...