On a hot
summers day it is noticeable that temperatures in a
forest are much lower than those outside. You are no
longer walking under a hot, baking sun. It feels
sheltered and it may feel slightly more humid.
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Radiation exchanges in woodland
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- Examples of tree albedos: Scots pine 9%; Oak (summer)
15%, Oak (spring) 12%; Sitka spruce 12%; Norway
spruce 12%; Orange trees 32%; Tropical forest 13%.
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The effects of woodland type
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Temperature in
woodlands
- Woodlands are normally cooler in summer and
slightly warmer in winter.
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Moisture in
woodlands
- Increased output of moisture - In a forest
, leaves are continually transpirating moisture
into the atmosphere. As winds inside a woodland
area are usually light, this moisture is not
easily dispersed.
- Interception of moisture input - On the
other hand, vegetation is continually
intercepting moisture, so less of it reaches the
forest floor.
- The net effect on humidity levels within a
woodland is small.
- Daytime temperatures within a woodland are cooler
than those outside - this makes the relative
humidity of the air greater within a forest (even
if the forest atmosphere contains the same
absolute amount of water vapour as outside it).
- Experiments suggest a 5% difference, although
much depends on the time of year and weather
conditions.
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| Difference
of relative humidity (per cent) between the inside and
outside of a forest |
Forest type
|
January
|
April
|
July
|
October
|
Year
|
| Deciduous broad leaf |
3.4
|
3.2
|
-0.8
|
1.1
|
2.2
|
| Needle tree conifer |
4.8
|
4.8
|
6.5
|
9.5
|
6.8
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| Japanese cedar |
1.6
|
-1.1
|
1.5
|
0.5
|
0.8
|
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| Positive values indicate
that the inside of the forest was more humid. The
research was undertaken by the University of Tokyo, Japan.
(Briggs & Smithson p140) References: David
Briggs and Peter Smithson (1985) Fundamentals of
Physical Geography pub Hutchison, chp 9.
- Chapter
8 of Lenon & Cleves Fieldwork
Techniques includes suggestions for
studying local climate. Towns, woods and lakes
all create their own climate.
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