Arctic Carbon Sinks: Present and Future.

Abstract

Surface air temperatures of the Arctic rose 1.2 deg -1.5 deg C from 1880 to 1980, in contrast to a global warming of only 0.4 deg -0.5 deg C; since 1980, six of the warmest years in the past century have been observed. Polar enhancement of a temperature rise, induced possibly by anthropogenic release of greenhouse gases, C02, N20, CH4, and freons, to the atmosphere, is attributed to altered ice/ snow albedo at sea level, i.e., melting of sea ice. A 5% decline of sea ice extent in the Arctic and Antarctic from 1979 to 1987 may have resulted in increased light availability within previously ice-covered polar regions.

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Document Details

Document Type
Technical Report
Publication Date
Dec 01, 1989
Accession Number
ADA258313

Entities

People

  • John J. Walsh

Organizations

  • University of South Florida St. Petersburg

Tags

Communities of Interest

  • Space

DTIC Thesaurus Topics

  • Boundary Layer
  • Chemical Synthesis
  • Chemistry
  • Climate Change
  • Computational Fluid Dynamics
  • Equations Of State
  • Geography
  • Grids
  • Marine Biology
  • Oceanography
  • Oceans
  • Ridges
  • Sea Water
  • Topography
  • Two Dimensional

Fields of Study

  • Environmental science

Readers

  • Combustion and Flow Dynamics.
  • Mathematics or Statistics
  • Polar and Arctic Studies