Cloud distribution characteristics at Mizuho Station, Antarctica are discussed. The transmittance of the direct solar radiation and downward longwave radiation are used as an index of clouds. The frequency of occurrence of the clear sky-1.0 transmittance, minimum extreme of downward longwave radiation-is very high throughout the year, which may be pronounced characteristics at inland stations. The direct solar beam transmittance is a good indicator of clouds in the sunlit season. The downward longwave radiation varies sensitively according to the cloud. The normalized emissivity defined from the longwave flux has a good correlation to the cloud amount, and is a good indicator of clouds throughout the year
The solar radiation balance on the ground surface at Mizuho Camp (70°42.6\u27S, 44°18.9\u27E, elevat...
AbstractVariations of cloud amount and radiative fluxes are a matter of discussion related to the re...
Upward and downward radiation on the snow surface were observed at Asuka Camp (72°31\u27S, 24°08\u27...
Measurements of radiation components were carried out at Mizuho Station in a period from 1979 to 198...
Radiation budget measurements were made at Mizuho Station under the program of POLEX-South. Global a...
Cloud distributions are analyzed from AVHRR data of the NOAA satellite received at Syowa Station (69...
The solar radiation balance on the ground surface at Mizuho Camp (70°42.6'S, 44°18.9'E, elevation 2,...
We critically review and improve a simple method to extract year-round records of cloud optical thic...
The seasonal and spatial variation of downward longwave radiation (L↓) at the surface of the Antarct...
Together with measurements at Mizuho Station during POLEX-South, longwave radiation fluxes are calcu...
The 13th Symposium on Polar Science/Ordinary sessions [OM] Polar meteorology and glaciology, Wed. 16...
ABSTRACT. Hourly measurements of incoming short-wave and long-wave radiation, surface albedo, and ne...
This paper presents the infrared effective emissivity value of low and middle clouds deduced from 26...
The effective emissivity of Antarctic clouds is calculated from radiation measurements using the rad...
Downward solar irradiance at the sea surface, measured on several voyages of an icebreaker in the So...
The solar radiation balance on the ground surface at Mizuho Camp (70°42.6\u27S, 44°18.9\u27E, elevat...
AbstractVariations of cloud amount and radiative fluxes are a matter of discussion related to the re...
Upward and downward radiation on the snow surface were observed at Asuka Camp (72°31\u27S, 24°08\u27...
Measurements of radiation components were carried out at Mizuho Station in a period from 1979 to 198...
Radiation budget measurements were made at Mizuho Station under the program of POLEX-South. Global a...
Cloud distributions are analyzed from AVHRR data of the NOAA satellite received at Syowa Station (69...
The solar radiation balance on the ground surface at Mizuho Camp (70°42.6'S, 44°18.9'E, elevation 2,...
We critically review and improve a simple method to extract year-round records of cloud optical thic...
The seasonal and spatial variation of downward longwave radiation (L↓) at the surface of the Antarct...
Together with measurements at Mizuho Station during POLEX-South, longwave radiation fluxes are calcu...
The 13th Symposium on Polar Science/Ordinary sessions [OM] Polar meteorology and glaciology, Wed. 16...
ABSTRACT. Hourly measurements of incoming short-wave and long-wave radiation, surface albedo, and ne...
This paper presents the infrared effective emissivity value of low and middle clouds deduced from 26...
The effective emissivity of Antarctic clouds is calculated from radiation measurements using the rad...
Downward solar irradiance at the sea surface, measured on several voyages of an icebreaker in the So...
The solar radiation balance on the ground surface at Mizuho Camp (70°42.6\u27S, 44°18.9\u27E, elevat...
AbstractVariations of cloud amount and radiative fluxes are a matter of discussion related to the re...
Upward and downward radiation on the snow surface were observed at Asuka Camp (72°31\u27S, 24°08\u27...