the whole year and for the
different seasons are calculated and shown in Table 2.
The results show that the POD is higher for V5 than for
Figure 2 shows the monthly rainfall climatology for
the different regions of Thailand computed from the
TG. In the north, northeast, central, and east regions,
there are three seasons: winter (November to February),
hot (March to May/June), and rainy (May/June to
October). Conversely, there are only two seasons in the
south region: rainy (May/June to December) and hot
(January to May).
There are two rainfall peaks during the rainy season:
one in May and the other in August or September,
except in the south region, which shows a minimum in
February and a maximum in November. The secondary
rainfall peak in May is associated with the southwest
monsoon, during which the southwesterly wind from
the Indian Ocean brings moist air toward Thailand.
Some of the moisture is blocked by the mountain
ranges in Burma. In August the northeasterly trade
winds blow in the reverse direction, causing the August
to September maximum rainfall peak. For the onset,
the data show the rainfall pattern in the northward pro
the whole year and for the
different seasons are calculated and shown in Table 2.
The results show that the POD is higher for V5 than for
Figure 2 shows the monthly rainfall climatology for
the different regions of Thailand computed from the
TG. In the north, northeast, central, and east regions,
there are three seasons: winter (November to February),
hot (March to May/June), and rainy (May/June to
October). Conversely, there are only two seasons in the
south region: rainy (May/June to December) and hot
(January to May).
There are two rainfall peaks during the rainy season:
one in May and the other in August or September,
except in the south region, which shows a minimum in
February and a maximum in November. The secondary
rainfall peak in May is associated with the southwest
monsoon, during which the southwesterly wind from
the Indian Ocean brings moist air toward Thailand.
Some of the moisture is blocked by the mountain
ranges in Burma. In August the northeasterly trade
winds blow in the reverse direction, causing the August
to September maximum rainfall peak. For the onset,
the data show the rainfall pattern in the northward pro
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