Trees and the Public Realm - Westminster City Council
Trees and the Public Realm - Westminster City Council
Trees and the Public Realm - Westminster City Council
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<strong>Trees</strong> <strong>and</strong> <strong>the</strong> <strong>Public</strong> <strong>Realm</strong> (Draft) Page 43<br />
110. Generally speaking, urban areas will warm more than rural because buildings <strong>and</strong> hard<br />
surfaces absorb heat from <strong>the</strong> sun <strong>and</strong> reradiate <strong>the</strong> stored heat energy back into <strong>the</strong><br />
atmosphere. The result of this ‘heat isl<strong>and</strong> effect’ can be higher temperatures,<br />
particularly at night, <strong>and</strong> in enclosed areas (including under tree canopies) in<br />
comparison to suburban <strong>and</strong> rural areas. The current maximum surface temperature of<br />
woodl<strong>and</strong>s is 18.4 o C, compared to 31.2 o C in town centres 12 .<br />
Summary of expected climate change in <strong>the</strong> UK 13<br />
Temperature • Annual warming by <strong>the</strong> end of <strong>the</strong> century of between 1 o C <strong>and</strong><br />
5 o C<br />
• Greater warming in <strong>the</strong> Sou<strong>the</strong>ast than in <strong>the</strong> Northwest<br />
• Increase in <strong>the</strong> number of very hot days<br />
• Decrease in <strong>the</strong> number of very cold days<br />
Precipitation • Generally wetter winters (by up to 30%) increase in winter<br />
precipitation intensity<br />
• Substantially drier summers<br />
Soil Moisture • Decreases in summer <strong>and</strong> autumn, especially in <strong>the</strong> Sou<strong>the</strong>ast<br />
• Increases in winter<br />
111. Periods of unusually high temperatures (heat waves) are predicted to become more<br />
frequent <strong>and</strong> last longer, with town centres predicted to experience a bigger<br />
temperature rise than rural. Green space, in <strong>the</strong> form of street trees, parks, <strong>and</strong> private<br />
gardens has a significant role to play in reducing <strong>the</strong> urban heat isl<strong>and</strong> effect. A 10%<br />
increase in trees, in <strong>the</strong> right places, can reduce surface temperatures by 3-4 o C.<br />
112. Although it is not straightforward within <strong>Westminster</strong> to plan green space at <strong>the</strong> strategic<br />
level (as would be <strong>the</strong> case with greenfield development) <strong>the</strong>re is much that can be<br />
done at <strong>the</strong> local neighbourhood level to moderate <strong>the</strong> effects of climate change.<br />
Shade provided by trees can keep hard surfaces cooler than unshaded areas by<br />
several degrees, <strong>and</strong> trees, especially when located close to buildings, provide not only<br />
shade but act as natural cooling systems through <strong>the</strong> process of evapotranspiration.<br />
113. While it is recognised that not every street is suitable for trees both in terms of<br />
practicality <strong>and</strong> urban design, maximising <strong>the</strong> opportunities to plant larger growing<br />
shade trees will assist in <strong>the</strong> moderation of high summer temperatures <strong>and</strong> in so doing<br />
make <strong>Westminster</strong> a more liveable city.<br />
114. It is anticipated that trees will also need to be more adapted to a hotter, drier climate<br />
<strong>and</strong> consideration should perhaps be given to tree species that are indigenous in<br />
climates similar to those predicted for <strong>the</strong> south of Engl<strong>and</strong> around 2040-2060. The<br />
adaptability of our existing tree stock (eg. oak) will also be increasingly relevant.<br />
12 Adaption Strategies for Climate Change in <strong>the</strong> Urban Environment<br />
13 CLG, 2007, Climate Change <strong>and</strong> Urban Spaces .