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Each
atmospheric layer is defined by its chemical and physical properties.
Troposphere: The lowest,
turbulent part of the atmosphere, in which all weather events
take place (altitude from ground to about 10 km).
Stratosphere: The atmosphere layer above the
troposhere (altitude from about 10 to about 50 km). The upper
layers of the stratosphere are also known as the ozone layer.
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Climate
forcing: Any imposed perturbation
of the global climate system of the Earth. This could happen
through
different mechanisms such as changes in the:
Radiative
climate forcing: The change in the global radiation
energy budget imposed by a change in a factor that interferes
with the radiation budget, such as the concentration of a greenhouse
gas, trapping outgoing (long-wave) radiation in the lower atmosphere,
or the presence aerosols, reflecting incoming (shortwave) radiation
back to space.
Cloud
forcing: The radiative forcing associated with changes
in the cloud cover. Clouds partially reflect incoming (shortwave)
radiation and thereby cause a cooling effect. At the same
time intercept they have a greenhouse effect on outgoing radiation.
The net balance of these two opposite effects is highly uncertain,
and depends on the form and altitude of the clouds.
For
more
information on climate forcing, see the wikipedia
article "radiative forcing".
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Aerosol: any
solid particle or liquid droplet suspended (i.e. floating) in air.
Most occur naturally, originating from volcanoes, dust storms, forest
and grassland fires, living vegetation (e.g. biogenic organic compounds),
and sea spray. |
edaphic:
relating to soil (including organisms, water, etc).
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Phenology: the study of the impact of the
climate on the cyclic phenomena of plants and animals. |
ENSO (El
Nino South Oscillation): A see-saw
pattern in the tropical Pacific, affecting the prevailing wind
system and ocean currents. ENSO is a major cause of the global
interannual climate variability. |
Termination:
In the glacial-interglacial cycle, the termination marks the transition
from a glacial to an interglacial period. |
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