To reveal the latitudinal distribution of atmospheric turbidity enhanced by the eruption of Mt. Pinatubo in June 1991 and Mt. Hudson in August 1991,aerosol optical depth at 5 wavelengths was observed with a portable sunphotometer (EKO MS-120) in November to December of 1991 and 1992. The observations were made from Tokyo to Syowa Station, east Antarctica on the icebreaker SHIRASE and on the route from Syowa Station to Dome-F, about 1000km inland. Another sunphotometer observation has been continued at Syowa Station since 1985. The main results of these observations are as follows. From onboard observations, aerosol optical depth at 500 nm in November and December of 1991 reached about 4 times the 1979 or 1987 level in the region of the equa...
Unusual aerosol enhancement is often observed at Syowa Station, Antarctica, during winter and spring...
The direct and indirect effects on solar radiation, temperature and ozone due to volcanic eruptions ...
Vertical distributions of atmospheric aerosol particles were measured nine times up to 5200 m a.s.l....
Attenuation measurements of solar irradiance using an airborne sun photometer were performed for the...
The aerosol optical depth at 4 wavelengths (368, 500, 778 and 868nm) has been measured automatically...
The NOAA/NESDIS operational aerosol optical thickness product has provided an exceptional view of th...
International audienceTwilight sky colour measurements were made using ground-based UV-visible SAOZ ...
Optical depths at visible and infrared wavelengths obtained in Tucson, Arizona before and after the ...
Balloon measurements of aerosols have been made in the winter and spring of 1985 to investigate the ...
Spectral measurements of the direct solar radiation were made by a pyrheliometer at Mizuho Station, ...
International audienceA key limitation of volcanic forcing datasets for the Pinatubo period is the l...
The time evolution of the perturbations in aerosol spectral optical depths associated with the Mt. P...
Lidar measurements made at Poker Flat, Alaska in winter 1991/1992 suggest that stratospheric aerosol...
This paper describes the results of meteorological observations at Syowa Station from February 1,199...
Surface measurements of solar irradiance of the atmosphere were made by a multipurpose computer-cont...
Unusual aerosol enhancement is often observed at Syowa Station, Antarctica, during winter and spring...
The direct and indirect effects on solar radiation, temperature and ozone due to volcanic eruptions ...
Vertical distributions of atmospheric aerosol particles were measured nine times up to 5200 m a.s.l....
Attenuation measurements of solar irradiance using an airborne sun photometer were performed for the...
The aerosol optical depth at 4 wavelengths (368, 500, 778 and 868nm) has been measured automatically...
The NOAA/NESDIS operational aerosol optical thickness product has provided an exceptional view of th...
International audienceTwilight sky colour measurements were made using ground-based UV-visible SAOZ ...
Optical depths at visible and infrared wavelengths obtained in Tucson, Arizona before and after the ...
Balloon measurements of aerosols have been made in the winter and spring of 1985 to investigate the ...
Spectral measurements of the direct solar radiation were made by a pyrheliometer at Mizuho Station, ...
International audienceA key limitation of volcanic forcing datasets for the Pinatubo period is the l...
The time evolution of the perturbations in aerosol spectral optical depths associated with the Mt. P...
Lidar measurements made at Poker Flat, Alaska in winter 1991/1992 suggest that stratospheric aerosol...
This paper describes the results of meteorological observations at Syowa Station from February 1,199...
Surface measurements of solar irradiance of the atmosphere were made by a multipurpose computer-cont...
Unusual aerosol enhancement is often observed at Syowa Station, Antarctica, during winter and spring...
The direct and indirect effects on solar radiation, temperature and ozone due to volcanic eruptions ...
Vertical distributions of atmospheric aerosol particles were measured nine times up to 5200 m a.s.l....