E. Linacre and B. Geerts |
10/'97 |
Trees occur in cities at various scales (Table
1). They suppress surface winds, either by the formation and shedding of
eddies in the lee of isolated trees, or, in the case of a close-planted canopy,
by containing mechanical and buoyant turbulence to the top of the canopy. Some
turbulence results from hydrodynamic instability (3), associated with the
roughness of the urban profile. Trees change the urban profile, increasing the
roughness if they protrude above the buildings, or decreasing it by smoothing
the outline as a result of filling in gaps. The roughness is quantified by a 'roughness length' zo, which depends on the frontal area of the average
element divided by the ground area it occupies. Trees within an industrial park
or a region of apartments may reduce zo from 1.2 m to 0.7 m,
whereas in a suburb of (low) detached houses the effect is to raise zo
from 0.25 m to 0.40 m (1). Thus trees slightly increase winds (at 20 m above
ground) in the first case and reduce them in the second. However, these changes
are negligible at ground level.
Table 1. Typical dimensions of various kinds of urban tree canopy in a city of
about a million people (1,2)
Unit |
Built features |
Tree features |
Climate phenomena |
height: m |
width: m |
length: m |
building |
garden |
single tree |
wake, shadow |
10 |
10 |
10 |
canyon |
street |
avenue, boulevard, shelterbelt |
street vortex, shade, temperature |
10 |
30 |
300 |
block |
city block, factory |
park, wood |
local breeze |
- |
500 m |
5 km |
land-use zone |
residence, industry, city centre |
greenbelt, suburban forest |
air quality, topoclimates |
- |
5 km |
5 km |
city |
built-up area |
urban forest |
heat, humidity, city breeze, smog dome, rainfall modification |
- |
25 km |
25 km |
Trees
differ from buildings in that heat is generated within the latter by human
occupancy, and temperatures are not kept close to the air temperature by
evaporation. The temperatures of leaves of well-watered plants rarely differ
more than two or three degrees from air temperature (4, 5, 6). More than 70% of
incoming energy is commonly used in evaporation.
Another
difference is the albedo. That of building materials is often higher than the
22% typical of green foliage, but the multiple surfaces of city buildings tend
to trap reflected radiation, effectively decreasing the albedo overall.
Consequently, there is usually less than 5% albedo difference between built-up
and foliated surfaces.
Taking
into account the various differences, it is possible to compare the net effect
by calculation of the surface temperatures at 3pm on a clear day in summer,
within canopies of either trees or buildings entirely. The forest is typically
8 K cooler, and the difference of air temperatures in the same circumstance is
estimated as 3.5 K (1). With 50% tree cover, the differences would be about
half as much. Hence, trees can improve daytime conditions significantly in hot
climates.
Also,
the reduced heating of a city by trees decreases the 'country breeze', which
blows sometimes in the evening from the rural environs towards the warmer city
centre.
Apart
from the modest effects of trees on topoclimates within city regions, the
vegetation can considerably modify winds around individual buildings. There one
can differentiate between vertical winds down the face of an isolated tall
building, and the cyclone generated within an almost enclosed courtyard, and
the accelerated horizontal winds caused by funnelling down a city canyon or
round the sides of a tall building. In the case of a single tall building,
winds impacting at below 0.7 times its height (called the 'stagnation point')
are directed downwards, with occasional pulses of winds appropriate to that
height (1). If these gusts exceed 22 m/s (ie 80 km/h) at least once a year, the
situation at ground level is regarded as unsatisfactory, since such winds can
blow a pedestrian into the path of traffic (7). In some cases of courtyard
spaces, as in shopping complexes, the induced whirling winds have caused
commercial failure. Spaced trees along streets or beside tall buildings can
substantially reduce wind speeds there (8). However, one has to balance the
advantage of reduced cold winds in winter against the disadvantage of poorer
ventilation in summer.
Often
trees are planted near houses to give shade in summer, on the side facing the
Sun - the north side in the southern hemisphere. Unfortunately, this also
entails less radiation onto the house in winter, when the heat would be
welcome. Even deciduous trees in winter cut out about a third of the radiation.
It
is concluded that care is required when planting trees to improve the
environment within cities.
References
(1) Oke, T.R. 1989. The micrometeorology of
the urban forest. Phil. Trans. Royal Soc., London. B324, 335-49.
(2) Finnigan, J. 1994. Improving the
physical urban environment with trees. Proc 1994 Second National Urban Tree
Seminar. (Royal Australian Inst. Parks an Recreation) 22pp.
(3) Raupach, M.R. 1992. Drag and drag
partition on rough surfaces. Boundary-Layer Meteor. ,60, 375-95.
(4) Linacre, E.T. 1964. A note on a feature
of leaf and air temperatures. Agric. Meteor., 1, 66-72.
(5) Linacre, E.T. 1967. Further notes on a
feature of leaf and air temperatures. Archiv. Meteor. Geophys. Bioklim. B15,
422-36.
(6) Linacre, E.T. 1972. Leaf temperatures,
diffusion resistances and transpiration. Agric. Meteor. 10, 365-82.
(7) Melbourne, W.H. 1978. Criteria for
environmental wind conditions. J. Wind Engineering an Indust. Aerodynamics,
3, 241-9.
(8) Gandemer, J. 1981. The aerodynamic
characteristics of windbreaks, resulting in empirical design rules. J. Wind
Engineering an Indust. Aerodynamics , 4, 15-36.