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The Tropospheric Chemistry of Ozone in the Polar Regions (Paperback, Softcover reprint of the original 1st ed. 1993)
Loot Price: R3,000
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The Tropospheric Chemistry of Ozone in the Polar Regions (Paperback, Softcover reprint of the original 1st ed. 1993)
Series: Nato ASI Subseries I:, 7
Expected to ship within 10 - 15 working days
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The Arctic troposphere (0 to ca. 8 km) plays an important role in
environmental concerns for global change. It is a unique chemical
reactor influenced by human activity and the Arctic ocean. It is
surrounded by industrialized continents that in winter contribute
gaseous and particulate pollution (Arctic haze). It is underlain by
the flat Arctic ocean from which it is separated by a crack-ridden
ice membrane 3 to 4 m thick. Ocean to atmosphere exchange of heat,
water vapor and marine biogenic gases influence the composition of
the reactor. From September 21 to December 21 to March 21, the
region north of the Arctic circle goes from a completely sunlit
situation to a completely dark one and then back to light. At the
same time the lower troposphere is stably stratified. This hinders
vertical mixing. During this light period, surface temperature
reaches as low as -40 DegreesC. In this environment, chemical
reactions involving sunlight are generally much slower than further
south. Thus, the abundance of photochemically reactive compounds in
the atmosphere can be high prior to polar sunrise. Between complete
dark in February and complete light in April, a number of chemical
changes in the lower troposphere take place.
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