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Arctic aerosol and clouds studied by bistatic lidar technique

Olofson, K. Frans G., 1976 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry
Svensson, Erik, 1977 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry
Witt, Georg (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
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Pettersson, Jan B. C., 1962 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry
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 (creator_code:org_t)
Washington, D.C. American geophysical union, 2009
2009
Engelska.
Ingår i: Journal of Geophysical Research. - Washington, D.C. : American geophysical union. - 0148-0227 .- 2156-2202. ; 114, s. D18208-
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Aerosol and cloud studies were carried out with a polarimetric bistatic lidar setup at the Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) in Andenes (69°N, 16E°), Norway. The measurements were performed from 10 to 23 October 2006 and covered altitudes between 1.5 and 11 km, corresponding to scattering angles between 130 and 170°. The degree of linear polarization, PL, calculated from the experiments was compared with light scattering calculations using Lorenz‐Mie theory for spherical particles, the T‐matrix approach for nonspherical rotationally symmetric particles, and a geometric optics ray‐tracing method. Average PL values between 0.61 and 0.72 were obtained for the background aerosol under cloud‐free conditions. The aerosol results may be qualitatively reproduced by standard aerosol types if a suitable combination of coarse‐ and fine‐mode spherical particles is assumed. The PL values obtained for thin and mildly opaque clouds were in the range from 0.21 to 0.38. These results were not well described by spherical particles, and the results for relatively small prolate and oblate particles studied with the T‐matrix method tended to be slightly higher than the experimental values. Geometric optics calculations for hexagonal column ice particles with surface roughness were able to reproduce the experimental cloud data. This does not rule out contributions from other types of particles, and particle orientation effects may also have influenced the results. We conclude that the experimental results are consistent with earlier in situ studies of cirrus clouds, and the further development and application of the bistatic lidar technique is discussed.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
NATURVETENSKAP  -- Kemi -- Fysikalisk kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences -- Physical Chemistry (hsv//eng)

Nyckelord

Cloud
Aerosol
Lidar
Meteorology
Meteorologi
atmosfärvetenskap
Atmospheric Sciences

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