The size distribution of aerosols attached to falling snow crystals was measured, utilizing optical microscopic photographs of sublimated traces of the snow crystals in Sapporo where the air is highly polluted, in March 1973. The resolution power of the microscope was insufficient to measure the size distribution of submicron aerosols, and the movement of aerosols towards the center of the snow crystals was recognized. However, within the resolution power, the following results were obtained. 1. In the size distribution of aerosols attached to the snow crystals, the frequency increased smoothly as their size decreased down to I (.t. 2. Several thousand aerosols were attached to one snow crystal. 3. The area number density of aerosols in a r...
Snow crystal observations in Mizuho Plateau, Antarctica, during the 1981 austral summer revealed the...
Snow crystals with small raindrops were observed all day long on 1 January 1990 during the observati...
In situ cloud observations at mountain-top research stations regularly measure ice crystal number co...
Aerosols attached to falling snow crystals were directly observed utilizing optical and electron mic...
International audienceIn early February 2001 (during the austral summer), over 900 000 digital image...
Many snow flakes were photographed between 1951 and 1954 in Japan, and they were classified, accordi...
Experiments to evaporate natural snow crystals and snowflakes under a polarization microscope were c...
Snowflakes composed of snow crystals of cold temperature types were often observed in mid~winter in ...
The snowfall rate is related to microphysical and dynamical processes in weather systems and is furt...
Since 1970, measurements of aerosol spectra have been and are being by our institute simultaneously ...
The information on the aerosol properties from remote locations provides insights into the backgroun...
This paper discusses techniques which have been developed for obtaining photomicrographs of snow cry...
This study was carried out to describe the chemical characteristics of individual residual particles...
During the Cloud and Aerosol Characterization Experiment (CLACE) 2013 field campaign at the High Alt...
The amount of snow blown under high velocity wind conditions was estimated at Syowa Base with the ai...
Snow crystal observations in Mizuho Plateau, Antarctica, during the 1981 austral summer revealed the...
Snow crystals with small raindrops were observed all day long on 1 January 1990 during the observati...
In situ cloud observations at mountain-top research stations regularly measure ice crystal number co...
Aerosols attached to falling snow crystals were directly observed utilizing optical and electron mic...
International audienceIn early February 2001 (during the austral summer), over 900 000 digital image...
Many snow flakes were photographed between 1951 and 1954 in Japan, and they were classified, accordi...
Experiments to evaporate natural snow crystals and snowflakes under a polarization microscope were c...
Snowflakes composed of snow crystals of cold temperature types were often observed in mid~winter in ...
The snowfall rate is related to microphysical and dynamical processes in weather systems and is furt...
Since 1970, measurements of aerosol spectra have been and are being by our institute simultaneously ...
The information on the aerosol properties from remote locations provides insights into the backgroun...
This paper discusses techniques which have been developed for obtaining photomicrographs of snow cry...
This study was carried out to describe the chemical characteristics of individual residual particles...
During the Cloud and Aerosol Characterization Experiment (CLACE) 2013 field campaign at the High Alt...
The amount of snow blown under high velocity wind conditions was estimated at Syowa Base with the ai...
Snow crystal observations in Mizuho Plateau, Antarctica, during the 1981 austral summer revealed the...
Snow crystals with small raindrops were observed all day long on 1 January 1990 during the observati...
In situ cloud observations at mountain-top research stations regularly measure ice crystal number co...