| Ahmedabad
IndiaGeography and Climate |
Ahmedabad
is located at 23.03° N 72.58° E in western India at
an elevation of 53 metres (174 feet). The city sits on the
banks of the River Sabarmati, in north-central Gujarat. It
spans an area of 205 km² (79.15 square miles). The Sabarmati
frequently dries up in the summer, leaving only a small stream
of water. The city is located in a sandy and dry area. Many
of the localities and roads are often spread in sand, reflecting
the intensifying fallout caused by deforestation. The steady
expansion of the Rann of Kutch threatens to increase desertification
around the city area and much of the state. Except for the
small hills of Thaltej-Jodhpur Tekra, the city is almost flat.
Two
lakes are within the city's limits — Kankaria Lake and
Vastrapur Lake. Kankaria lake, in the neighbourhood of Maninagar,
is an artificial lake developed by the Sultan of Delhi, Qutb-ud-din
Aybak, in 1451. According to the Bureau of Indian Standards,
the town falls under seismic zone-III, in a scale of I to
V (in order of increasing proneness to earthquakes) while
the wind and cyclone zoning is "very high damage risk",
according to UNDP report.
There
are three main seasons: summer, monsoon and winter. Aside
from the monsoon season, the climate is dry. The weather is
hot through the months of March to June — the average
summer maximum is 36 °C (97 °F), and the average minimum
is 23 °C (73 °F). From November to February, the average
maximum temperature is 30 °C (85 °F), the average
minimum is 15 °C (59 °F), and the climate is extremely
dry. Cold northerly winds are responsible for a mild chill
in January. The southwest monsoon brings a humid climate from
mid-June to mid-September. The average rainfall is 93.2 cm
(36.7 inches), but infrequent heavy torrential rains cause
the river to flood. The highest temperature recorded is 47
°C (116.6 °F) and the lowest is 5 °C (41 °F).
In recent years, Ahmedabad has suffered from increasing air,
water and soil pollution from neighbouring industrial areas
and textile mills.
Ahmedabad
is divided by the Sabarmati into two physically distinct eastern
and western regions. The eastern bank of the river houses
the old city, which includes the central town of Bhadra. This
part of Ahmedabad is characterised by packed bazaars, the
clustered and barricaded pol system of shanty buildings, and
numerous places of worship. It houses the main railway station,
the General Post Office, and landmark buildings of the Muzaffarid
and British eras. The colonial period saw the expansion of
the city to the western side of Sabarmati, facilitated by
the construction of Ellis Bridge in 1875 and later with the
modern Nehru Bridge. This part of the city houses educational
institutions, modern buildings, well-planned residential areas,
shopping malls, multiplexes and new business districts centred
around C. G. Road, Ashram Road, and more recently, the Sarkhej-Gandhinagar
Highway.
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