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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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271<br />

an effort to minimize the impact of this building activity. In<br />

contrast the wind measured at the 900 hPa level in the free atmosphere<br />

did not change appreciably during the same period (Peterson, 8))<br />

indicating this feature as the likely source of the reduction in<br />

surface windspeed.<br />

In addition, this increase in building height would result in<br />

the presence of warmer buildings occupying a larger solid angle<br />

relative to the cooler sky. Such a reduction in sky view factor would<br />

reduce the loss of heat by longwave radiation from the surface (factor<br />

2) thereby tending to contribute to elevated night-time minimum<br />

temperatures. Finally, during this period factor 5 probably assumed<br />

increasing importance with greater building volume, increasing<br />

population, more human activity <strong>and</strong> traffic all contributing to the<br />

anthropogenic heat added to the urban canopy. Again, the trend of<br />

more rapidly increasing minima than maxima during this period is<br />

consistent with this scenario.<br />

Lastly, in the 1970 T s <strong>and</strong> 80 f s the increase both in built-up<br />

area <strong>and</strong> building volume has nearly ceased as the area has become<br />

almost totally built-up to the maximum permitted by zoning regulations.<br />

However, the increase in population density, traffic volume <strong>and</strong> the<br />

use of air conditioning has meant that factor 5 probably has assumed a<br />

more dominant role than heretofore. While a continuing increase in<br />

night-time minimum temperatures is consistent with this effect it is<br />

more difficult to explain the steady decline in daytime maxima during<br />

this phase. The explanation may, however, be linked to the fact that<br />

the Royal Observatory is still surrounded in its immediate area by<br />

actively transpiring vegetation. Additional available energy may<br />

enhance this transpiration thus causing a cooling effect not only offsetting<br />

the tendency to further increase in daytime maxima but even<br />

reversing it. In effect the postulation is that factor 6 may not<br />

apply in this situation.<br />

While all that has been postulated so far must be considered<br />

as derived from observed associations it appears to be internally

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