The microwave emission from a half-space medium characterized by coordinate dependent scattering and absorbing centers was calculated by numerically solving the radiative transfer equation by the method of invariant imbedding. A Mie scattering phase function and surface polarization was included in the calculation. Also included are the physical temperature profile and the temperature variation of the index of refraction for ice. Using published values of grain size and temperature profile data of polar firn, the brightness temperature was calculated for the 1.55 cm and 0.8 cm wavelengths. For selected regions in Greenland and Antarctica, the results are in reasonable agreement with the observed Nimbus-5 and Nimbus-6 ESMR data
A time series of daily brightness temperature gridded maps (October 25, 1978 through August 15, 1987...
The complex refractive index of sea ice is modeled and used to predict the microwave signatures of v...
A method to retrieve the surface emissivity of sea ice at the window channels of the Advanced Microw...
The microwave brightness temperature for snow fields was studied assuming that the snow cover consis...
Variation in crystal size and physical temperature of snowfield observations from space give large v...
Principles pertinent to the utilization of 1.55 cm wavelength radiation emanating from the surface o...
Airborne observations of 19.35 GHz microwave radiation were taken over the sea ice and firn cover of...
Areas of the Canadian high plains, the Montana and North Dakota high plains, and the steppes of cent...
International audienceTime series of observed microwave brightness temperatures at Dome C, East Anta...
To examine the influence of bright band on the retrieval of precipitation rate, the performance of m...
Applications of microwave brightness temperature measurements in meteorology, hydrology,climatology ...
A radiative transfer model to compute brightness temperatures in the microwave frequency range for p...
An airborne microwave wide-band radiometer (500–2000 MHz) was operated for the first time in Antarct...
Nimbus-5 Electrically Scanned Microwave Radiometer data were analyzed for the fall of 1975 and winte...
Because of its great size, the Antarctic Ice Sheet represents a considerable fresh water resource. F...
A time series of daily brightness temperature gridded maps (October 25, 1978 through August 15, 1987...
The complex refractive index of sea ice is modeled and used to predict the microwave signatures of v...
A method to retrieve the surface emissivity of sea ice at the window channels of the Advanced Microw...
The microwave brightness temperature for snow fields was studied assuming that the snow cover consis...
Variation in crystal size and physical temperature of snowfield observations from space give large v...
Principles pertinent to the utilization of 1.55 cm wavelength radiation emanating from the surface o...
Airborne observations of 19.35 GHz microwave radiation were taken over the sea ice and firn cover of...
Areas of the Canadian high plains, the Montana and North Dakota high plains, and the steppes of cent...
International audienceTime series of observed microwave brightness temperatures at Dome C, East Anta...
To examine the influence of bright band on the retrieval of precipitation rate, the performance of m...
Applications of microwave brightness temperature measurements in meteorology, hydrology,climatology ...
A radiative transfer model to compute brightness temperatures in the microwave frequency range for p...
An airborne microwave wide-band radiometer (500–2000 MHz) was operated for the first time in Antarct...
Nimbus-5 Electrically Scanned Microwave Radiometer data were analyzed for the fall of 1975 and winte...
Because of its great size, the Antarctic Ice Sheet represents a considerable fresh water resource. F...
A time series of daily brightness temperature gridded maps (October 25, 1978 through August 15, 1987...
The complex refractive index of sea ice is modeled and used to predict the microwave signatures of v...
A method to retrieve the surface emissivity of sea ice at the window channels of the Advanced Microw...