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climate change
Observed Climate Change in Hong Kong
Cloud amount, solar radiation and evaporation

An increase in cloud amount can cause a decrease in diurnal temperature range by reducing the solar incoming radiation during day time and trapping of long-wave radiation at night. The diurnal temperature range has decreased worldwide since the 1950s and the coincidental increases in total cloud cover are often cited as a likely cause for the observed decrease in diurnal temperature range.

In Hong Kong, cloud amount is reported in oktas hourly by trained observers at the Hong Kong Observatory Headquarters. The daily mean cloud amount is taken as the average value of the observed hourly cloud amount in a day. Based on these daily mean cloud amounts, annual mean values were calculated. Regression result indicates that the annual mean cloud amount has been increasing at a rate of 1.1% per decade in the period 1961 to 2011. One potential cause for the increase in cloud amount over Hong Kong could be the likely increase in the concentration of condensation nuclei in the air that favoured the formation of clouds, which is known to be associated with urbanization and human activities in the region.

annual mean cloud amount recorded at the hong kong observatory headquarters from 1961 to 2011

Annual mean cloud amount recorded at the Hong Kong Observatory Headquarters (1961-2011)

Both the increase in the concentration of suspended particulates and the increase in cloud amount would reduce the amount of solar radiation reaching the surface. At King's Park (a meteorological station located 900m north of Hong Kong Observatory Headquarters in urban Kowloon), the amount of solar radiation reaching the surface is recorded continuously by thermo-electric pyranometers. Between 1958 and 2011, there has been a clear, broad falling trend. For the whole period, regression result indicates that the annual mean daily global solar radiation decreased at a linear rate of 0.72 MJm-2 per decade.

Annual mean daily total global solar radiation at King's Park (1958-2011)

Annual mean daily total global solar radiation at King's Park (1958-2011)

Evaporation measurements are made daily at King's Park using evaporation pans with evaporation surface 0.18 m above ground. In general, the amount of evaporation depends on the amount of solar radiation received, the relative humidity as well as the wind speed. Accompanying the decrease in solar radiation and wind speed, the annual total evaporation recorded at King's Park also decreased at a rate of 125 mm per decade, according to a regression fit for the period from 1961 to 2011.

Annual total evaporation at King's Park (1961-2011)

Annual total evaporation at King's Park (1961-2011)

 

 

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