Evaporation records from pans are frequently used to estimate evaporation
from lakes and reservoirs and ET from an area. Since information about
monthly coefficients is not available in India, these coefficients are
decided using the analogy of spatial variation from arid and humid regions
to the conditions that prevail in India during winter and summer months.
During the transition months, the ambient temperature and the pan
temperature are considered to be the same. Also, as it is generally observed
that a factor of 0.7 is accepted the world over as the coefficient on an
annual basis, the monthly variation has to be plus or minus the value of the
annual coefficient. According to these considerations, the monthly
coefficients can be adopted as 0.6 in cold dry winter months, 0.8 in hot
summer months and 0.7 in the transition months between the winter and the
summer and the vice-versa. For this purpose, the parallel of 22°
latitude has been taken as the demarcating line.
Variation of Pan Coefficient values with month
Location
|
Coefficient |
0.6 |
0.7 |
0.8 |
North of
22°
latitude |
November-February |
March-April and September-October |
May-August |
South of
22°
latitude |
December-January |
February-March and September-November |
May-August |
Evaporation Maps
Evaporation rates closely follow climatic
seasons, and reach their peak in the summer months of April and May.
The central areas of the country display the highest evaporation rates
during this period. With the onset of monsoon, there is a marked fall in the
rate of evaporation. The annual potential evaporation ranges from 150 to 250
cm over most parts of the country. Monthly potential evaporation over the
peninsula increases from 15 cm in December to 40 cm in May. In the
North-East, it varies from 6 cm in December to 20 cm in May. It rises to 40
cm in June in West Rajasthan. After the onset of monsoon, evaporation
decreases all over the country.
India Meteorological Department has published monthly and annual mean
evaporation values of 30 stations in India.
Typical features of evaporation for various months
Month/season |
Evaporation variation over the country |
January |
Evaporation is highest (16 cm) over Saurashtra- Kutch. It
is about 14 cm at Jalgaon in Maharashtra and Raichur -Bellary in North
interior Karnataka. It is 8 to 10 cm over Rajasthan and Peninsular
India, 6 cm over Uttar Pradesh and Bihar and less than 6 cm over Assam. |
February |
There is an increase in evaporation by 2 cm over previous
month. The increase is 4 cm in Saurashtra- Kutch and Jalgaon and 6 cm
over Raichur -Bellary. |
March |
The pattern is similar to January and February.
Evaporation is 27 to 29 cm over Saurashtra-Kutch, Jalgaon and
Raichur-Bellary. Over Rajasthan it varies from 15 cm to 20 cm and around
15 cm in Uttar Pradesh. Evaporation is less than 10 cm over Assam. |
April |
There is an overall increase in evaporation by 8 to 10 cm
over the previous month. |
May |
Evaporation is the highest in this month. It varies from
12 cm over Assam to 50 cm over Jalgaon. Over Kota and Saurashtra-Kutch
it is 40 cm. In north India, it varies from 20 to 35 cm. Gaya with its
characteristic semi-arid climate is isolated with 35 cm. In the
Peninsula it varies from 15 to 35 cm. Over Assam it is less than 15 cm. |
June |
The distribution pattern is similar to May.
However, values of evaporation are slightly less than those in May. |
July |
There is appreciable fall in the evaporation as compared
to the June values. Isolated pockets of 25 cm over Rajasthan and Bellary
-Raichur region are noticed. Near Kovilpatti in Tirunalveli district in
Tamil Nadu, the evaporation is more than 30 cm. It varies from 10 to 25
cm in the peninsula and 12 to 25 cm in north India including North-east. |
August |
The evaporation varies from 10 cm in Assam and west coast
to 20 cm in Rajasthan and central parts of the Peninsula. |
September |
Over Saurashtra-Kutch, Bellary -Raichur region and the
Kovilpatti area the evaporation is 20 cm and rest of India it varies
from 10 to 16 cm. Over Assam, it is less than 10 cm. |
October |
The pattern is similar to September. However, with
reduced evaporation by 2 to 5 cm through out the country. |
November |
The evaporation has decreased further and excepting for
pockets over Saurashtra-Kutch, Jalgaon, Bellary-Raichur and Kovilpatti
where it is 15 cm. Evaporation varies from 10 to 12 cm over Peninsula
and 5 to 10 cm in North India and less than 5 cm in Assam. |
December |
The evaporation pattern is similar to January with high
pockets (12-14 cm) over Saurashtra-Kutch, Jalgaon and Raichur -Bellary.
In other parts it is around 6 to 10 cm. |
Monsoon (June-October) |
The pattern generally resembles those observed during the
months of July, August and September. Evaporation over West-coast and
Assam is less than 60 cm. It is more than 100 cm over Rajasthan and
adjoining areas of Gujarat, Madhya Pradesh, and parts of Haryana and
Uttar Pradesh. Isolated pockets of high evaporation could be seen around
Kovilpatti in Tamil Nadu and Bellary -Raichur in Karnataka. |
Non-monsoon (November-May) |
The pattern very much resembles the monsoon. Evaporation
is less than 100 cm over West-coast, East-coast and Assam and is around
125 cm over Rajasthan and adjoining areas. It is more than 100 cm around
Kovilpatti in Tamil Nadu. Isolated pockets of high evaporation of 150 cm
are seen around Jalgaon in Maharashtra and Bellary. |
Annual |
As is to be expected, the pattern is broadly similar to
the monthly distribution, with centres of high evaporation over
Saurashtra-Kutch, Jalgaon and Kovilpatti in Tamil Nadu. It is lowest,
100 cm over Assam. The 200 cm isoline covers a narrow strip of
north-south tract from Punjab to Karnataka through Rajasthan and
Maharashtra. Parts of Uttar Pradesh and Bihar States have evaporation
ranging from 150 to 200 cm. |
|