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Bulletin updated at 00:15 HKT
18/ Jul /2018

Yesterday's Weather and Radiation Level

Hong Kong Observatory:
Maximum Air Temperature: 34.3 C
Minimum Air Temperature: 26.9 C
Grass Minimum Temperature: 25.9 C
Relative Humidity: 57 - 92 percent
Rainfall: 6.5 mm

Total Rainfall since 1st January: 880.3 mm
Against an average of 1288.4 mm

Other Stations
Min
Max
King's Park
26.5 C
33.5 C
Wong Chuk Hang
26.7 C
33.6 C
Ta Kwu Ling
25.4 C
34.7 C
Lau Fau Shan
25.7 C
34.4 C
Tai Po
26.4 C
33.0 C
Sha Tin
26.3 C
34.6 C
Tuen Mun
26.3 C
34.1 C
Tseung Kwan O
26.7 C
33.3 C
Sai Kung
27.2 C
33.1 C
Cheung Chau
26.0 C
32.2 C
Chek Lap Kok
27.4 C
35.9 C
Tsing Yi
27.3 C
34.8 C
Shek Kong
25.8 C
34.5 C
Tsuen Wan Ho Koon
25.2 C
33.0 C
Tsuen Wan Shing Mun Valley
25.5 C
33.5 C
Hong Kong Park
26.2 C
34.5 C
Shau Kei Wan
25.8 C
32.9 C
Kowloon City
26.6 C
33.9 C
Happy Valley
27.6 C
35.3 C
Wong Tai Sin
26.9 C
34.6 C
Stanley
27.1 C
32.9 C
Kwun Tong
26.8 C
33.0 C
Sham Shui Po
27.1 C
34.8 C

Duration of Sunshine (King's Park): 8.0 H
The mean UV Index recorded at King's Park yesterday was 5,
the UV intensity was Moderate
The maximum UV Index for yesterday was 12.
Sea surface temperature (Waglan Island):28.2 C

Yesterday's (17 Jul) average ambient gamma radiation dose rate taken outdoors in Hong Kong ranged from 0.08 to 0.14 microsievert per hour. These are within the normal range of fluctuation of the background radiation level in Hong Kong (See Note). The average dose rates measured at the radiation monitoring stations over various parts of the territory were as follows :

Station
Yesterday's average (microsievert/hour)
King's Park
0.14
Ping Chau
0.09
Tap Mun
0.09
Kat O
0.10
Yuen Ng Fan
0.12
Tai Mei Tuk
0.12
Sha Tau Kok
0.10
Kwun Tong
0.12
Sai Wan Ho
0.08
Tsim Bei Tsui
0.13

Note
  1. From readings taken at various locations in Hong Kong in the past, the hourly mean ambient gamma radiation dose rate may vary between 0.06 and 0.3 microsievert per hour. (1 microsievert = 0.000001 sievert = 0.001 millisievert)
  2. Temporal variations are generally caused by changes in meteorological conditions such as rainfall, wind and barometric pressure.
  3. Spatial variations are generally caused by differences in the radioactive content of local rock and soil.
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