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Micro
climates
A
microclimate is a local atmospheric zone where the climate differs
from the surrounding area. The term may refer to areas as small
as a few square feet (for example a garden bed) or as large as many
square miles (for example a valley). Microclimates exist, for example,
near bodies of water which may cool the local atmosphere, or in
heavily urban areas where brick, concrete, and asphalt absorb the
sun's energy, heat up, and reradiate that heat to the ambient air:
the resulting urban heat island is a kind of microclimate.
Another contributory factor to microclimate is the slope, or aspect.
South-facing slopes in the Northern Hemisphere and north-facing
slopes in the Southern Hemisphere are exposed to more direct sunlight
than opposite slopes and are therefore warmer for longer.
The area in a developed industrial park may vary greatly from a
wooded park nearby, as natural flora in parks absorb light and heat
in leaves, that a building roof or parking lot just conducts back
to the air. Solar energy advocates argue that widespread use of
solar collection can mitigate overheating of urban environments
by absorbing sunlight and putting it to work instead of heating
the local surface objects.
A microclimate can offer an opportunity as a small growing region
for crops that cannot thrive in the broader area; this concept is
often used in permaculture practiced in northern temperate climates.
Microclimates can be used to the advantage of gardeners who carefully
choose and position their plants. Cities often raise the average
temperature by zoning, and a sheltered position can reduce the severity
of winter. Roof gardening, however, exposes plants to more extreme
temperatures in both summer and winter.
Microclimates can also refer to purpose made environments, such
as those in a room or other enclosure. Microclimates are commonly
created and carefully maintained in museum display and storage environments.
This can be done using passive methods, such as silica gel, or with
active microclimate control devices.
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