On cruise KH-94-4 of the research vessel HAKUHO MARU, we measured aerosol concentrations over the western Pacific Ocean and the Southern Ocean. Aitken particle concentration was measured with a Pollak condensation nuclei counter. Size distribution for large and giant particles was measured with an optical particle counter. On this expedition, we observed at a nearly fixed station (64-65.5°S, 140°E) twice, in December 1994 and January 1995,for a total of sixteen days. The concentrations of Aitken particles at the fixed station were somewhat higher than those measured around 10°N latitude during this expedition and previous expeditions. These values were nearly equal to or lower than values obtained by other workers. Moreover, Aitken particle...
Continuous measurements of Aitken particle concentration were carried out by using an improved Polla...
Number–size distributions of aerosol particles with diameters of 10–500 nm in the marine boundary la...
Aerosols influence global climate directly by scattering and absorbing incoming solar radiation and ...
The goals of the International Global Atmospheric Chemistry (IGAC) Program's First Aerosol Character...
The optical and chemical properties of atmospheric aerosols were determined from the ground-based me...
Some 30 years of physical and chemical marine aerosol data are reviewed to derive global-size distri...
The Size distribution and volatility of ultrafine aerosol particles were measured at Syowa Station d...
During the CHARLEX campaign in the Galápagos Islands, a Scanning Particle Mobility Sizer was deploye...
The chemical composition of aerosol particles (Dp ≤ 1.5 μm) was measured over the southeast Pacif...
Concentration and number size distribution of aerosol particles from 4.4 to 168 nm diameter are meas...
xi, 116 leavesDuring the ACE-Asia and TRACE-P field campaigns aircraft measurements over the Yellow ...
Marine background levels of non-sea-salt- (nss-) SO42− (5.0–9.7 neq m−3), NH4+ (2.1–4.4 neq m−3) and...
Aerosol physics measurements made onboard the Swedish icebreaker Oden in the late Summer and early A...
International audienceEven though oceans cover the majority of the Earth, most aerosol measurements ...
In order to investigate the concentration distribution of soil particles and pollutants in the marin...
Continuous measurements of Aitken particle concentration were carried out by using an improved Polla...
Number–size distributions of aerosol particles with diameters of 10–500 nm in the marine boundary la...
Aerosols influence global climate directly by scattering and absorbing incoming solar radiation and ...
The goals of the International Global Atmospheric Chemistry (IGAC) Program's First Aerosol Character...
The optical and chemical properties of atmospheric aerosols were determined from the ground-based me...
Some 30 years of physical and chemical marine aerosol data are reviewed to derive global-size distri...
The Size distribution and volatility of ultrafine aerosol particles were measured at Syowa Station d...
During the CHARLEX campaign in the Galápagos Islands, a Scanning Particle Mobility Sizer was deploye...
The chemical composition of aerosol particles (Dp ≤ 1.5 μm) was measured over the southeast Pacif...
Concentration and number size distribution of aerosol particles from 4.4 to 168 nm diameter are meas...
xi, 116 leavesDuring the ACE-Asia and TRACE-P field campaigns aircraft measurements over the Yellow ...
Marine background levels of non-sea-salt- (nss-) SO42− (5.0–9.7 neq m−3), NH4+ (2.1–4.4 neq m−3) and...
Aerosol physics measurements made onboard the Swedish icebreaker Oden in the late Summer and early A...
International audienceEven though oceans cover the majority of the Earth, most aerosol measurements ...
In order to investigate the concentration distribution of soil particles and pollutants in the marin...
Continuous measurements of Aitken particle concentration were carried out by using an improved Polla...
Number–size distributions of aerosol particles with diameters of 10–500 nm in the marine boundary la...
Aerosols influence global climate directly by scattering and absorbing incoming solar radiation and ...