Abstract
‘ARCTIC haze’ refers to turbid layers of air which are found regularly over the pack ice north of Alaska during periods of clear weather1. These layers are diffuse, hundreds to thousands of kilometres wide, 1–3 km thick, and can occur as single or multiple bands of different heights at nearly any level in the troposphere. They are invisible from the ground, but may limit horizontal and slant visibility within a layer to as little as 3–8 km. Their colour is grey–blue in the antisolar direction and reddish–brown in the solar direction, suggesting that they are true aerosol rather than ice crystals.
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References
Mitchell, M. J. Atmos. Terr. Phys. Special Supplement 195–211 (1956).
Holmgren, B., Shaw, G. & Weller, G. AIDJEX Bulletin 27, 135–148 (1974).
Rahn, K. A. The chemical composition of the atmospheric aerosol (University of Rhode Island Technical Report, 1976).
Staff members of the section of Synoptic and Dynamic Meteorology, Institute of Geophysics and Meteorology, Academia Sinica, Peking, Tellus 9, 432–446 (1957); ibid. 10, 58–75 (1958).
Jackson, M. L. et al. Soil Sci. 116, 135–145 (1973).
Carlson, T. N. & Prospero, J. M. J. appl. Meteor. 11, 283–297 (1972).
Shaw, G. E. Tellus 27, 39–49 (1975).
Darby, D. A., Burckle, L. H.. & Clark, D. L. Earth planet. Sci. Lett. 24, 166–172 (1974).
Isono, K. et al. Tellus, 23, 40–59 (1971).
Radke, L. F., Hobbs, P. V. & Pinnons, J. E. J. appl. Meteor. 15, 982–995 (1976).
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RAHN, K., BORYS, R. & SHAW, G. The Asian source of Arctic haze bands. Nature 268, 713–715 (1977). https://doi.org/10.1038/268713a0
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DOI: https://doi.org/10.1038/268713a0
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