CLIMATE
The climate of Ambala over most of the year is a pronounced continental in character.It is very hot in summers and markedly cold in winters.May and June can be really
hot with the temperature soaring to over
48°C,while in winter it can be as low
as -1°C.
Ambala has a semi-arid as well as tropical climate.Being far away from the coasts
and close to the Thar desert,it
does not get the full share of the Monsoon current
seen mostly across central and east of the country.
Around 70% rainfall is received during the month of July to September and the remaining
rainfall is received during December to February.Ambala is the maximum rain-hit
area in Haryana with average rainfall being 47.16 inches per annum.
River System
& Water Resources
The district is mainly drained by non-perennial
streams and the drainage system of the district comprises of the following:
1. The Markanda & its tributaries
2. The Dangri (Tangri) & its tributaries
3. The Ghagghar & its tributaries
The Markanda and the Dangri streams ultimately drain
into the Ghagghar river beyond the territory of the district. The Ghagghar along
with its tributaries however constitutes an inland drainage system.
The Markanda
The Markanda which drains the southern slopes of Dharti
Dhar range (Himachal Pradesh) , cuts through the
shivalik range and enters the plains and the district. The river channel which is
broad between Kala Amb and Mullana becomes narrow to the south of Mullana. During
the rainy season, the river carries enormous water which causes flooding in its
lower course.
The Dangri
The Tangri streams rises
in the Morni Hills and flows in a southerly direction upto village Chajju Majra
where it is joined by the Baliali Nadi. It further flows a southerly course running
on the eastern side of Ambala Cantonment. After crossing the Ambala Cantonment Ambala-Jagadhari
railway line it takes south-westerly direction . Near the villages of Segta &
Segti the torrent of Omla and Amri join the Dangri. It is here that the Narwana
branch of Bhakhra main canal crosses the Dangri stream. Thereafter the Dangri takes
a westerly course upto village Niharsi where it turns towards south and leaves the
district to enter the Patiala district of Punjab.
The Dangri rising from Morni Hills , used to flow
on a southerly direction upto Panjokhra, a village in the North-East of Ambala from
where it was separated into two main channels. These two channels still kept a southerly
course running on either side of Ambala cantonment.
The Dangri seems to have changed its course towards the close of 19th century when
the drainage was confined to the eastern channel.The Baliali Nadi rises in the southern
slopes of the Morni Hills and joins the Dangri stream near village Chajju Majra.
The Amri ( also known as Shahzadpur wali or Dadri) is formed of water collected
in plains during the rainy season. It starts near Rataur and flows south-west and
takes the torrent of the Omla and joins the Dangri between the villages of Segta
and Segti.
The Ghaggar
The Ghagghar, another important river also traverses the
district for some distance in the north west. The river originates in Sirmaur district
of Himachal Pradesh and enters the district. It traverses the district near
Ambala City for a very short distance and then flows parallel to the district
boundary outside the district .While in its-upper course , the river contains some
water throughout the year, in its lower course it is generally dry in summer and carries water only during the rainy season.The two tiny lakes at an elevation of
620 metre above mean sea level near village Masiyun in the Morni hill tract are
of little importance as these lakes neither feed any major stream nor are these
being fed by any major river. Only a small stream from one of these lakes joins
the Dangri (Tangri) nadi. Despite the large number of drainage lines passing through
the district, the area suffers from inadequate water resources. Canal irrigation,
which is limited to a few small pockets in the south-western
tip of Ambala tehsil, does not have much scope for extension because of undulating
topography in a large part of the district. Thus, wells and tubewells remain the
major source of irrigation in the district.
Mineral Occurances
Limestone
Two bands of limestone one about 13 metre thick and the other about 25 metre thick,
both extending over 500 metre have been located at Tundapathar. It is very high
grade limestone with an average of 93 percent Calcium Carbonate and low in Magnesium
Oxide.The estimated reserve is about 6 lakh tonnes. A band of thinly bedded
Sabathu limestone, about 5 metre thick, occurs at Barun in Naraingarh tehsil. A
band of limestone, about 20 metre thick and about 1.2 kilometre long occurs at Kharag.
The total reserve in the area is estimated at 50 lakh tonnes of good quality limestone.The
largest deposit of this area occurs at Ramsar and Sherla (Naraingarh tehsil). The
limestone is well bedded about 30 metre thick and extends for about 2.4 kilometres.
The reserve is estimated at about 120 lakh tonnes. The limestone belt extends to
Malla (Kalka tehsil), Jonpur, Dabsu, Ambri and Jabial in Naraingarh tehsil.
Saltpetre
A small quantity of salpetre is extracted from the soils around Ambala and Barara.The
ground water in the district occurs under confined and semi-confined conditions.
The depth of water level varies greatly in the area immediately to the south
of the Shivalik hills. It ranges between 2 and 47 metre, maximum being towards
the hills. The water level in the area further south ranges between 1.5 and
1.2 metre, but generally it varies between 4 and 8 metre. The shallow tubewells
are usually constructed down to a depth of 10 to 45 metre. However at some places
as in Nagia-Mullana belt, have been drilled to a depth of 90 metre. Shallow tubewells
usually tap ground water from single aquifer. The deep tubewells generally range
in depth between 91 and 185 metre but at few places tubewells down to 445 metre
have also been constructed. Ground-water is generally fresh and suitable for domestic
and irrigation purposes.
Seismicity
Seismically Ambala district lies in a region where
earthquakes of moderate to great intensity have been experienced in the past. Being
situated very close to the Himalayan Boundary Fault Zone, it is prone to earthquake
shocks originating there. History of the past two hundered years for which records
are available shows that during the Kangra earthquake of 1905, Ambala district
experienced an intensity of VII-VIII M.M.(Modified Mercalli Intensity Scale of 1951).
A committee of experts under the auspices of Indain Standard institution prepared
seismic zoning map of India, where Ambala district has been placed in zone IV Where
a maximum seismic intensity VIII M.M. is likely to reach in future earthquakes.Taking
into consideration the above factors and also the fact that the extreme cases of
high intensity occur only at long intervals, it is felt that a provision of seismic
ground acceleration of 10 percent gravity (.10 g) may be made for engineering structures
founded on well consolidated soil. For weaker foundations and important structures,
the seismic factor may be suitably increased.