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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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261<br />

THE IMPACT OF URBANIZATION ON <strong>CLIMATE</strong><br />

IN HONG KONG <strong>AND</strong> ITS IMPLICATIONS FOR<br />

HUMAN ENERGY EXCHANGES<br />

by<br />

William J. Kyle<br />

Department of Geography & Geology<br />

University of Hong Kong<br />

Hong Kong<br />

ABSTRACT<br />

The impact of urbanization on long-term climatic changes<br />

as evidenced by trends in temperature <strong>and</strong> wind speed<br />

measured at the Royal Observatory, Hong Kong is examined.<br />

Evidence shows a long-term warming trend concurrent with<br />

increasing urbanization. Further investigation<br />

attributes this trend to both horizontal expansion in<br />

the built-up areas around the Observatory as well as<br />

vertical expansion in more recent years. A definite<br />

declining trend in post-war surface wind speed is also<br />

evident <strong>and</strong> is linked to this latter phase of<br />

urbanization. These two trends are examined within the<br />

context of the commonly hypothesized causal factors for<br />

the development of an urban canopy layer heat isl<strong>and</strong>.<br />

The implications for human energy exchanges of this<br />

warming trend are examined <strong>and</strong> an evaluation of the<br />

likely effect on human thermal comfort is presented.<br />

INTRODUCTION<br />

It has been stated that the most obvious climatic manifestation<br />

of urbanization is the trend towards higher temperatures, thi's trend<br />

depending on the prevailing synoptic conditions (L<strong>and</strong>sberg, 6)). Urban<br />

climates are really differentiated topoclimates <strong>and</strong> as such depend on<br />

variation of radiative fluxes <strong>and</strong> turbulent exchanges, the contrasts of<br />

which are greatest in clear, calm conditions <strong>and</strong> least in cloudy, windy<br />

weather.

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