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MOnthly weather bulletin JULY 2007 1. SUMMARY In general, the country received average to very much above average amounts of rainfall. In most places, the temperatures recorded were higher than the long-term average value. The country recorded lower than average amounts of daily solar radiation and experienced lower rates of evaporation. 2. RAINFALL July falls in the
peak of the Southwest Monsoon. During this month, heavy rains
are noted in several areas in Peninsular Malaysia. The total
amount of rainfall is recorded as average to much above average.
This was due to the higher than normal sea surface temperature
at the East of Indian Ocean and the less frequency of tropical
storms activities over the Pacific Ocean and northern South
China Sea. Thus, the southwesterlies flows that usually carries
dry weather in Peninsular Malaysia becomes weak and it caused
the development of convective cloud clusters in afternoon and
early night which as a result, brings about an increase in
rainfall in this month. Other than that, the elongated monsoon
troughs which are normally formed at the northern South China
Sea to the western Pacific Ocean were found unstable during
July. This caused the southwesterlies flows become weak and
allowed trade wind to penetrate into this region. The
convergence between southwesterly and easterly wind had
contributed to increase the formation of cloud clusters and
causing heavy rains with thunderstorms to occur in the evening
over Peninsular Malaysia. 3. TEMPERATURE Generally, most
places in the country had higher than average temperature. The
mean temperature of the month over lowland areas varied from
26.1°C to 27.7°C as recorded at Senai and Kota Bharu
respectively. Mersing recorded the largest positive deviation of
+0.8°C from normal. 4. SOLAR RADIATION The country generally received below average amount of solar radiation. The daily mean values varied from 10.73MJm-2 at Senai to 19.56MJm-2 at Miri. The largest positive and negative deviations from normal were +2.87MJm-2 and -3.78MJm-2 at Miri and Senai respectively. 5. EVAPORATION
In line with low solar radiation, the country
experienced lower rates of evaporation during this July. The
daily mean evaporation rate over the lowland areas ranged from
2.4mm/day (Kluang) to 4.4mm/day (Sibu). The largest negative
deviation was Figures and tables:
Figure
1 : Rainfall Map for Peninsular Malaysia
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