Research methods in ecologyClements, Frederic E. (Frederic Edward)
Science
Research methods in ecology
Clements, Frederic E. (Frederic Edward)
Plant ecology; Plant ecology -- Methodology
=124. Exposure= refers primarily to the direction toward which a slope
faces, i. e., its exposition or insolation with respect to sun and wind.
It is not altogether separable from slope, however, inasmuch as the
angle of the slope has some effect upon the degree of exposure. The
chief influence of exposure is exerted through temperature, since slopes
longest exposed to the sun’s rays receive the most heat. This is
supplemented in an important degree by the fact that a group of rays 1
foot square will occupy this area only on slopes upon which they fall at
right angles. In all other cases the rays are spread over a longer area,
with a consequent reduction in the amount of heat received. This effect
is felt principally in evaporation from the soil, and in soil
temperatures. For the leaf, it is largely if not entirely negligible,
since the angle of incidence is determined by the position of the leaf,
which is the same for each species whether on the level or upon a slope.
On this account, exposure has little or no bearing upon light, except
that the total amount of light received by the aggregate vegetation of a
slope will be greater than for a level area of the same size. The effect
of wind varies with the exposure. It is naturally most pronounced in
those directions from which the prevailing dry or cold winds blow, and
it is greatly emphasized by the fact that the opposite exposure is
correspondingly protected. The influence of wind, especially in
producing evaporation from the plant and the soil, increases with the
slope, since the mutual protection of the plants, or that afforded the
soil by the cover, is much reduced. Finally, the distribution of the
snow by the wind, a matter of considerable importance for early spring
vegetation, is largely determined by exposure.
Exposure is expressed directly in terms of direction, to which is added
the angle of the slope. A good field compass, reading to twelve points,
is sufficient. It should be checked, of course, by the declination of
the needle at the place under observation. A convenient instrument is
the one already mentioned, in which compass and clinometer are combined,
since these are regularly used at the same time.
Public-domain text, read in full here on John Shaqi.
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