When cold-air production areas lie in or near
the catchment areas of valleys and vales leading to developed
areas, natural paths for the supply of fresh cold air are
thereby provided, since cooler air continually flows towards
lower topographical areas. The intensity of flow depends upon
the size of the catchment area, the angle of slope inclination,
the width of the valley, and the degree of freedom from
obstruction. Cleaner fresh air can only be supplied by local air
flows when the environment (in the form of the surrounding area
and larger parks in cities) is intact and not excessively
burdened by pollution.
Potential hindrances for cold air flow include:
Narrowed sections of valleys, dams, noise protection barriers or
walls, rows of trees perpendicular to valley alignment, and
blockages from larger buildings or entirely enclosed urban
structures. Cold air stalls when it encounters hindrances; its
temperature drops strongly and air exchange is reduced in the
area in front of and behind the hindrance (leading to danger of
early or late frost or strengthened fog production). It is
mostly the emanation of heat above built-up areas that leads to
a reduction in the range and effect of cold air flow.
Also to be considered under this aspect are
sections of road that run in the direction of cold air flow,
even when they can be favored as hindrance-free corridors for
air exchange near the ground. In the case of roads perpendicular
to valley alignment, the thermal behavior of the narrow strip of
road plays a subordinated role, whereby the hindrance effect of
relief-altering measures (e.g. road dams and noise protection
edifices) dominates.
Cross-municipal planning must take care that
regional cold-air production areas can fulfill their special
function. This includes the restriction of development on open
areas and, where necessary, artificial foresting.
As long as slopes angled towards a city are
already forested or foreseen for forestation, a sufficiently
large surface in each case is to be kept open between the edge
of the forest and the built-up area in order to ensure the
daytime flow of especially valuable cold air out from the forest.
Valleys and other gorge-like features
important for the supply of fresh air are to be maintained as
fresh-air corridors and should be kept free of development to a
particularly large extent. Perpendicular-standing buildings in
lower valley areas represent a substantial hindrance. Large
changes of elevation in the lengthwise profile of a valley are
also to be avoided. Groups and rows of trees perpendicular to
valley alignment are likewise obstructive for air exchange near
the ground. As far as necessary in individual cases, a hindrance
of the cold air flow can be overcome by thinning or clearing
these trees. If necessary, a desired change in air flow
direction can be accomplish by foresting in the shape of a cork
at a different location. Urban structures should not intrude
into valleys.