2. Not equally distributed in Pakistan
Small area of northern Punjab & parts of KPK enjoy
humid conditions
Evapotranspiration
Evaporation is when liquid turns into vapour & the loss
of water from soil
Transpiration is the release of water vapour through
plants
3. 2 types of evapotranspiration
1. Potential Evapotranspiration
Maximum of vapour loss from soils & plants at
a given temperature
Higher temperature means higher
evapotranspiration
2. Actual evapotranspiration
Actual water loss
Depends on the amount of water in soil &
plants
4. Types of Rainfall
1. Conventional Rainfall
Surface air heated up and rises up.
žCools down in higher altitude.
žFall down as rain.
žAccompanies with thunder and lightning.
žResultant clouds are cumulonimbus type.
5. 2. Orographic Rainfall
Found on the windward sides of mountain ranges lying
across the path of
the prevailing terrestrial winds.
The leeward sides of the mountains is the rain shadow
region.
6. Saturated air from sea
Hits the mountains
Air cools in high altitude.
Falls as rain in the mountain slope.
7. 3. Cyclonic/Frontal Rainfall
Occurs along the frontal zones of convergence.
Meeting of hot and cold air
Cold air push up the hot air
As altitude increase the hot air cool downs
Condensation happens
Rain occurs.
8.
9. Rainfall Areas in Pakistan
1. Arid Areas
Large part of Pakistan is arid
Whole Sindh, southern Punjab & Southern
Baluchistan
250 mm rain annually
Farming through irrigation
2. Semi-Arid Areas
Northern Punjab, Northern Baluchistan & major
part of KPK
250-750 mm annual rainfall
Irrigation practised extensively
10. 3. Humid Areas
Small area of Pakistan is humid
Northern strip of Punjab, adjoining KPK &
around Parachinar
Rainfall exceeds 750mm
11. Seasonal Distribution of Rainfall
1. Monsoon Rainfall (July-September)
Pakistan receives tail end of monsoon
Monsoon winds from India reach Pakistan in July
& can last up to September
Eastern Pakistan receives more monsoon rainfall
From Sargodha southward rainfall drops to less
than 250mm
From Sahiwal it drop down to less than 125mm
Higher rainfall is recorded in Murree 813mm &
lowest Nok Kundi 2.5 mm
12.
13.
14.
15. 2. Rainfall from Western Disturbances
Enter from west through Afghanistan & Iran
Bring small amount of rain
From December to March
Since it coincides with winter so precipitation at
higher altitudes happens as snowfall
In Murree, Dir, Saidu Sharif 500mm
Northern Punjab, KPK & Baluchistan 125-250
Sindh…
3. Rainfall from Thunderstorms
During driest seasons (October & November)
16.
17. Convectional Currents
Happens when hot air rises from the hot land into the air.
This air is high in moisture, and causes a lot of
condensation when it reaches the atmosphere.
This condensation results in rainfall in different areas in
summer
18. Convectional currents cause some degree of
rainfall in Pakistan during the summer months.
This condensation results in rainfall in the
northern and north-Westren parts of Pakistan in
the summer.
The southern parts of Pakistan are deprived from
convectional currents due to a temperature
inversion layer