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DTIC ADA128371: Arctic Haze: Natural or Pollution?
by Defense Technical Information Center
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The overall chemical composition of the Arctic aerosol
was better defined; sulfur and carbon dominate. Different
Mn/V ratios on different sides of the Arctic were found;
both were inconsistent with eastern North American
source. 222Rn data for Barrow were produced. They
indicated a source to the north. Arguments were developed
for a Eurasian source and against a North American source
of Arctic aerosol. Chemical and physical aspects of long-
range transport of polluted air masses to the Arctic were
revealed by numerical simulation. The cloud-active
fraction of the aerosol of Iceland was seen to parallel
pollution-derived SO4 and V. Heating by Arctic aerosol in
spring was calculated. Deposition of aerosol to the
Arctic Ocean was estimated. High Br in North American
Arctic in spring was noted--neither source nor effects is
yet known. Trace-element composition of desert soils was
found to be nearly constant within the aerosol-size range
and form desert to desert, but highly variable for larger
particles. Particle-size distributions of Fairbanks
aerosol were estimated by inverting optical data.
Cloudiness in the Arctic was found to be generally
unchanged since 1920. Haze was reported in 114 of 3274
Ptarmigan flights, with greatest frequency in March-May.
Date Published: 2018-01-11 23:19:42
Identifier: DTIC_ADA128371
Item Size: 122506040
Language: english
Media Type: texts
# Topics
DTIC Archive; Rahn, Kenneth A ; RHODE...
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