Add to ORKGContinuous observation of snow drift flux was carried out at Mizuho Station (70°42′S, 44°20′E, 2230m above sea level), East Antarctica, in 1982. Snow drift flux at 1m height was well correlated with wind velocity. The correlation coefficient on a logarithmic plot was between 0.8 and 0.9. The drift flux was proportional to about the 8 power of wind velocity through the year. The power decreased above -20℃. The drift flux increased when precipitation was observed. From the variation of drift flux, precipitation intensity can be estimated
Surface snow accumulation is the primary mass input to the Antarctic ice sheets. As the dominant ter...
In the East Queen Maud Project from 1981 to 1987,accumulation rate on the ice sheet surface was obse...
The detailed meteorological and drifting snow data proposed in this dataset were acquired in the fra...
Measurements were carried out simultaneously of drifting snow and wind speed over the surface from 1...
Several measurements on drifting snow were carried out at Mizuho Station (70°42′S, 44°20′E, 2230m, a...
Precipitation at Mizuho Station, East Antarctica, in 1982 was estimated in two ways. From the drift ...
This paper describes annual precipitation estimated by blowing snow observations made on a strong ka...
A series of observations of drifting snow was carried out at Mizuho Camp, East Antarctica, during th...
At Syowa Station, Antarctica the author investigated the relation between the visibility and the win...
In the convergence slope/coastal areas of Antarctica, a large fraction of snow is continuously erode...
In Antarctica, direct measurements of processes shaping the surface mass balance such as precipitati...
The snow accumulation at Syowa and Mizuho Stations was recorded from the observations during the POL...
International audienceIn Antarctica, blowing snow accounts for a major component of the surface mass...
The influence of drifting and blowing snow on surface mass and energy exchange is difficult to quant...
In the convergence slope/coastal areas of Antarctica, a large fraction of snow is continuously erode...
Surface snow accumulation is the primary mass input to the Antarctic ice sheets. As the dominant ter...
In the East Queen Maud Project from 1981 to 1987,accumulation rate on the ice sheet surface was obse...
The detailed meteorological and drifting snow data proposed in this dataset were acquired in the fra...
Measurements were carried out simultaneously of drifting snow and wind speed over the surface from 1...
Several measurements on drifting snow were carried out at Mizuho Station (70°42′S, 44°20′E, 2230m, a...
Precipitation at Mizuho Station, East Antarctica, in 1982 was estimated in two ways. From the drift ...
This paper describes annual precipitation estimated by blowing snow observations made on a strong ka...
A series of observations of drifting snow was carried out at Mizuho Camp, East Antarctica, during th...
At Syowa Station, Antarctica the author investigated the relation between the visibility and the win...
In the convergence slope/coastal areas of Antarctica, a large fraction of snow is continuously erode...
In Antarctica, direct measurements of processes shaping the surface mass balance such as precipitati...
The snow accumulation at Syowa and Mizuho Stations was recorded from the observations during the POL...
International audienceIn Antarctica, blowing snow accounts for a major component of the surface mass...
The influence of drifting and blowing snow on surface mass and energy exchange is difficult to quant...
In the convergence slope/coastal areas of Antarctica, a large fraction of snow is continuously erode...
Surface snow accumulation is the primary mass input to the Antarctic ice sheets. As the dominant ter...
In the East Queen Maud Project from 1981 to 1987,accumulation rate on the ice sheet surface was obse...
The detailed meteorological and drifting snow data proposed in this dataset were acquired in the fra...