Climate
Although the country is in the monsoon region, it is arid; except
for the southern slopes of the Himalayas and the sub-Mountainous
tracts which have a rainfall from 76 to 127 cm. on the southern
ranges of the Himalayas, 127 cm. of precipitation takes place, while
under the lee of these mountains (Gilgit and Baltistan) rainfall is
hardly 16 cm. Rainfall also occurs from western cyclonic
disturbances originating in the Mediterranean. It is appreciable in
the western mountains and the immediate for lying area; here the
rainfall average ranges from 27 to 76 cm. The contribution of these
western disturbances to rainfall over the plains is about 4 cm. A
large part of the precipitation in the northern mountain system is
in the form of snow which feeds the rivers. The all-pervasive
aridity over most of Pakistan, the predominant
power on the
life and habitat of the people, coupled with the climatic rhythm,
characteristic of a monsoon climate, are conducive to homogeneity of
the land.
Seasons in Pakistan are:-
Cold season (December to March).
(ii) Hot season (April to June).
(iii) Monsoon season (July to September).
(iv) Post-Monsoon season (October and November).
The cold season sets in by the middle of December. This period is
characterized by fine weather, bracing air-low humidity and large
diurnal range of temperature. Winter disturbances in this season
accordingly cause fairly widespread rain. Average minimum and
maximum temperatures are 4 oC and 18 oC, though on occasions the
mercury falls well below freezing point. The winter sun is glorious.
The hot season is usually dry. Relative humidity in May and June
varies from 50 per cent in the morning to 25 per cent or less in the
afternoon. The temperature soars to 40 oC and beyond. The highest
recorded temperature at Jacob Abad in June is 53 oC. While the
interior is blazing hot, the temperature along the sea Coast Ranges
between 25 oC to 35 oC, but the humidity persists around 70 to 80
per cent. The south-west monsoon reaches Pakistan towards the
beginning of July and establishes itself by the middle of the month.
The strength of the monsoon current increases forms June to July; it
then remains steady, and starts retreating towards the end of
August, though occasionally, it continues to be active even in
September when some of the highest floods of the Indus Basin have
been recorded. From the middle of September to the middle of
November is the transitory period which may be called the
post-monsoon season. In October, the maximum temperature is of the
order of 34 oC to 37 oC all over Pakistan, while the nights are
fairly cool with the minimum temperature around 16 oC. In the month
of November, both the maximum and the minimums temperatures fall by
about 6 oC and the weather becomes pleasant. October and November
are by far the driest months all over the plains of Pakistan.