Wednesday, November 28, 2012
Monday, November 12, 2012
"Responding to Climate Change"
Climate change is a significant and lasting change in
the statistical distribution of weather patterns
over periods ranging from decades to millions of years. It may be a change in
average weather conditions, or in the distribution of weather around the
average conditions.
Scientists actively work to understand past and future
climate by using observations and theoretical models. Borehole temperature
profiles, ice cores, floral and
faunal records, glacial and periglacial processes, stable isotope and other
sediment analyses, and sea level records serve to provide a climate record that
spans the geologic past. More recent data are provided by the instrumental
record. Physically based general circulation
modelsare often used in theoretical approaches to match
past climate data, make future projections, and link causes and effects in
climate change.
On the broadest scale, the rate at which energy is
received from the sun and the rate at which it is lost to space determine the
equilibrium temperature and climate of Earth. This energy is distributed around
the globe by winds, ocean currents, and other mechanisms to affect the climates
of different regions.
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