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The following excerpt from
the proposal explains its connection to SEARCH.
How well can long-term
climate trends be assessed or predicted?
The polar regions, particularly the Arctic, are especially sensitive to
changes in climate, and models consistently predict future warming to
be much more significant in these regions than in their mid-latitude and
equatorial counterparts. This sensitivity arises primarily from
the positive albedo feedbacks associated with melting of the snow and
ice that blankets most of the region, and the insulating effects of sea
ice which modulate the exchange of energy, moisture, and momentum between
the ocean and the atmosphere. Moreover, the formation and disappearance
of sea ice cover play an important role in ocean circulation, particularly
the Atlantic thermohaline circulation in the northern hemisphere and the
formation of Antarctic bottom water in the southern hemisphere.
Additional factors that influence ocean circulation in polar regions are
high latitude precipitation and freshwater discharge from melting snow
and ice. Investigations are encouraged that will help improve our
knowledge of the feedback processes involving changes in polar regions.
Particular areas of interest are: 1) advancing our understanding
of the coupling between ice at the Earth's surface and the terrestrial
and solar radiation that helps determine the Earth's climate, 2) improving
the representation of high-latitude processes in climate models, and 3)
reducing uncertainty in predictions of how climate changes in polar regions
will influence ocean circulation. Investigations selected that support
NASA's role in investigating Arctic feedbacks will also represent a contribution
to the interagency initiative, SEARCH (Study of Environmental ARctic CHange).
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