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Research Spotlight: New interpretation of atmospheric bromine during Arctic spring
Author(s) -
Kumar Mohi,
Tretkoff Ernie
Publication year - 2010
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/eo091i051p00512-03
Subject(s) - spring (device) , bromine , atmospheric sciences , atmosphere (unit) , environmental science , arctic , frost (temperature) , aerosol , satellite , the arctic , ozone , latitude , sea ice , climatology , meteorology , astrobiology , geology , oceanography , geography , materials science , physics , astronomy , geodesy , metallurgy , thermodynamics
Bromine, which destroys ozone, is emitted into the atmosphere during the Arctic spring from inorganic sources including seasalt aerosol, frost flowers, and cracks in sea ice. It had been believed that all areas of enhanced atmospheric bromine observed from space at high latitude during spring originated from these sources at Earth's surface. However, a new analysis by Salawitch et al. suggests that previous satellite measurements may have been misinterpreted.

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