Destination India Climate

guideontravel — Wed, 26 Nov 2008 14:00:07 +0100

India ’s shape, unusual topography, and geographical position give it a diverse climate. Most of India has a tropical or subtropical climate ,
with little variation in temperature between seasons. The northern
plains, however, have a greater temperature range, with cooler winters
and hotter summers. The mountain areas have cold winters and cool
summers. As elevations increase sharply in the mountains, climate type
can change from subtropical to polar within a few miles.

India ’s seasonal cycle
includes three main phases: the cool, dry winter from October to March;
the hot, dry summer from April to June; and the southwest monsoon
season of warm, torrential rains from mid-June to September. India’s
winter season brings cold temperatures to the mountain slopes and
northern plains; temperatures in the Thar Desert reach freezing at
night. Farther south, temperatures are mild. Average daily temperatures
in January range from 13° to 27°C (55° to 81°F) in the northeastern
city of Kolkata (formerly Calcutta); from 8° to 21°C (46° to 70°F) in
the north central city of New Delhi; from 19° to 30°C (67° to 85°F) in
the west central coast city of Mumbai (formerly Bombay); and from 19°
to 29°C (67° to 85°F) in the vicinity of Chennai (formerly Madras) on
the southeastern coast. Dry weather generally accompanies the cool
winter season, although severe storms sometimes traverse the country,
yielding slight precipitation on the northern plains and heavy snowfall
in the Himalayas.

India ’s hot and dry season
reaches its most oppressive stage during May, when temperatures as high
as 49°C (120°F) are commonly recorded in the northern plains.
Temperatures in the southern peninsula are somewhat lower, averaging
35° to 40°C (95° to 104°F). At higher altitudes, as in the Western
Ghats and the Himalayas, temperatures are considerably cooler.

The intense heat breaks
when the summer monsoon season arrives in June. For most of the year
the monsoons, or seasonal winds, blow from the northeast. In the summer
months, however, they begin to blow from the southwest, absorbing
moisture as they cross the Indian Ocean. This warm, moist air creates
heavy rains as it rises over the Indian Peninsula and is finally forced
up the slopes of the Himalayas. The rains start in early June on a
strip of coast lying between the Arabian Sea and the foot of the
Western Ghats. A second “arm” of the monsoon starts from the Bay of
Bengal in the northeast and gradually extends up the Gangetic Plain,
where it meets the Arabian Sea “arm” in the Delhi region around July 1.
In July the average daily temperature range is 26° to 32°C (79° to
89°F) in Kolkata; 27° to 35°C (80° to 94°F) in New Delhi; 25° to 30°C
(78° to 86°F) in Mumbai; and 26° to 36°C (79° to 96°F) in Chennai.

The monsoon season is
critical to India. Farming depends heavily on the monsoon, even though
artificial sources of irrigation are also commonly used. The economy
prospers when the monsoon season is normal and plummets when it is not.
In the past a failure of the monsoon has brought abnormally low rains
in crucial food-growing regions, leading to famine. A failed monsoon season in
the dryland areas of the Deccan Plateau can mean poor or nonexistent
harvests for that year’s crop. In the Gangetic Plain, the groundwater
needed for irrigating the winter crop depends on the monsoon for
replenishing. However, an excessive monsoon may also spell disaster,
especially in the Gangetic Plain of eastern Uttar Pradesh and Bihār,
where rivers can flood and wash away homes and fields.

The average annual rainfall for India
as a whole is 1,250 mm (49 in). The heaviest rainfall occurs along the
Western Ghats, often more than 3,175 mm (125 in), and on the slopes of
the eastern Himalayas and the Khāsi Hills (of Meghalaya), where the
town of Cherrapunji receives 10,900 mm (430 in) annually. The entire
northeast region averages more than 2,000 mm (80 in) annually, with
Jharkhand, Orissa, and the Bengal region receiving nearly as much. Rain
and snow fall in abundance on the entire Himalayan range. New Delhi receives an annual average of 800 to 1,000 mm (32 to 40 in) of rain,
and the broad swath of land extending to the south, much of it in the
rain shadow of the Western Ghats, receives about the same or a little
more.

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Destination India Climate