DR.K.K.

MISHRA
• India’s climate is dominated by monsoons.

• Monsoons are strong, often violent winds that change

direction with the season.

• The term technically

describes seasonal
reversals of wind direction
caused by temperature
differences between the
land and sea breeze,
creating zones of high and
low pressure over land in
different seasons.
Monsoons occur due to
changes in atmospheric
pressure which are caused by
different rates of heating and
cooling of continents and
oceans.

Monsoons occur every year in

many countries around the
world other than South Asia -
northern Australia, Africa,
South America and the US are
also affected.

The geographical extent of

the global surface
monsoons (the figure
below) can be outlined by
the normalized seasonality
The global surface monsoons contains three kinds of
monsoons: the tropical, subtropical, and temperate-frigid
monsoons, respectively.

The extent of the classical tropical monsoons is surrounded by the

positions of the Inter Tropical Convergence Zone (ITCZ) in
summer and winter, which is the result of the two driving forcings
of the tropical monsoon, the seasonal variation of the planetary
thermal convection and the seasonal variation of the semi-
permanent planetary waves due to the thermal contrast between
ocean and continent. (Li and Zeng, 2000, 2003, 2005).
Surface temperature range that results in the monsoon

Sea surface temperature variations are much smaller than land surface
temperature variations. (Mainly the seasonal cycle)

Tibetan
plateau

Ocean:
range of
3 to 5°C
Monsoon is a term derived form the Arabic word
“Mausim”, meaning season. It was first used by
Arabic navigators to describe the seasonal winds of
the Arabian Sea.

These winds blow from the north-east for one half

of the year and from the south-west for the other
half.

Monsoon winds
blow from cold to
warm regions
because cold air
takes up more space
than warm air
❖ Being a tropical monsoon country
there are two monsoon seasons.
❖ The South –West (summer)
monsoon has warm winds blowing
from Indian Ocean. Its span is
June to September, with 75 % of
the annual rainfall in India. It
varies from 10 cm in western
Rajasthan to over 900 cm in
Meghalaya. Summer monsoon

❖ North- East (winter) monsoon is

characterized by a dry continental
air mass blowing from the vast
Siberian high pressure area from
December to March. The rainfall
includes snowfall during winter
monsoon which is of the order of
1000 km2 in India. This is also known
as Retreating monsoon.
Winter monsoon
• The mountains of southern India split the summer
winds. The western arm of the monsoon is deflected
northwards, by the western Ghats, to Mumbai and then
on to Pakistan.

• The eastern arm travels up through the Bay of Bengal to

Kolkata and Assam, and is deflected north-westwards by
the Himalayas.

• On average, the winds

arrive in southern India
about six weeks before
they arrive in north-west
India.
➢ Thar desert and adjoining areas of
the northern and central
Indian Subcontinent heats up too
much during summer.
This causes a low pressure area
over the northern and central
Indian subcontinent. To fill up this
void, the moisture-laden winds
from the Indian Ocean rush in to
the subcontinent.

➢ These winds, rich in moisture, are

drawn towards the Himalayas,
creating winds blowing storm a fully illuminated view of the Indian Ocea
region shortly after the onset of the SW
clouds towards the subcontinent. Monsoon.
The southwest monsoon is
generally expected to begin
around the middle of June and
dies down by September.
 Indian ocean winds - monsoon

December-March (NE
June-August (SW monsoon) monsoon)
Onset of South West Monsoon
 Retreating Monsoons
( North East Monsoon)
• Much of India experiences
infrequent and relatively
feeble precipitation during the
retreating monsoon.

• An exception to this rule

occurs along the southeastern
coast of India and for some
distance inland.

• When the retreating monsoon

blows from the northeast
across the Bay of Bengal, it
picks up a significant amount
of moisture, which is
subsequently released after
moving back onto the
peninsula.
•.
• Thus, from October to December the
coast of Tamil Nadu state receives at
least half of it’s roughly 1,000 mm of
annual precipitation

• This rainy extension of the generally

dry retreating monsoon is called the
northeast, or winter, monsoon.

• Another type of winter precipitation

occurs in northern India, which
receives weak cyclonic storms
originating in the Mediterranean
basin.
Retreating Monsoon
• In the Himalayas these storms bring
weeks of drizzling rain and
cloudiness and are followed by waves
of cold temperatures and snowfall.
The state of Jammu and Kashmir in
particular receives much of its
precipitation from these storms.
▪ The heaviest monsoon rainfalls occur where the
winds blow side-on to the hills. The higher the hills
and more moist the air, then the greater the amount
of rainfall.

▪ These factors give Cherrapunji, in Assam, one of the

highest rainfalls in the world. On average,
Cherrapunji has an annual rainfall total of nearly 11
metres, the maximum monthly amount occurring in
June.

▪ Mumbai receives about 1.8 metres with the

maximum monthly total in July.

▪ In comparison, Delhi registers only 64 cm of rainfall

each year with the maximum monthly total occurring
in both July and August.

▪ At Chennai the pattern of rainfall is different because

the monsoon winds blow along the coast. Here, the
rainfall increases gradually through the summer
months with larger amounts falling in October and
November, owing to tropical cyclones traveling
westwards across the Bay of Bengal.
• The torrential rainstorms often
cause violent landslides and
widespread floods. Entire villages
have been swept away during
monsoon rains. Despite the
potential for destruction, the
summer monsoons are welcomed
in India.

• Farmers depend on the rains to

irrigate their land.

• Additionally, a great deal of India’s

electricity is generated by water
power provided by the monsoon
rains.
➢ The monsoon delivers most of India's rainfall and has a key impact on
the economy. Only a third of India's crops grow on irrigated land and
a weak monsoon can wipe out many incomes and shrink demand for
farm equipment and consumer goods.
➢ Monsoon rainfalls are
unreliable in that the
amount varies
considerably from year to
year. Low rainfalls cause
great problems for
agriculture and water
supplies in general.
➢ In the Indus river the flood
problem is often made
worse because the
monsoon rainfalls can
coincide with high river
levels in its tributaries,
caused by water from the
melting mountain snows of
the Himalayas
 Interannual variations of Indian
summer monsoon

➢ The rainfall during the Indian summer monsoon season (June, July
,August and September) show considerable inter-annual and
interseasonal variability.

➢ Over any part of India, Some years a lot of rainfall occurs causing
flood, while some other years rainfall amount received is much less
causing drought like situations. This year to year variation of rainfall
over a region during monsoon seasons is termed as Interannual
variability of monsoon rainfall.

➢ This inter-annual variability in the summer monsoon rainfall has a

profound effect on the socioeconomic well being of India. Hence, the
ability to forecast such events became the focus of various
meteorological studies.
Monsoon Rainfall Variability
All-India mean Rainfall
 Predictability of the Indian Monsoon
Rainfall

➢ Short range (1-2 days in advance) and medium (3-10 days in

advance) predictions of rainfall over any region including that over
the Indian region during the monsoon season depend on how well
the initial state of the atmosphere has been defined with large
number of very good quality observed data and the quality dynamic
model used for predictions. The better the initial data, better is the
forecast.

➢ In the tropical region, it is believed that the predictability of day-

to-day weather patterns is restricted to 3-4 days.

➢ Observational studies show that the Indian Monsoon’s seasonal

rainfall is linked with several surface boundary conditions like sea
surface temperature (SST) of the east Pacific, Indian ocean ,land
surface temperature, Eurasian and Himalayan snow cover etc.
 Prediction of Indian summer monsoon

Since 1988, the Indian Meteorological Department has been issuing

forecast based on 16-parameter power regression and
parametric models.
List of 16 parameters
El Nino (same year) (Nino 1 + 2)
El Nino (previous year) (Nino 1 + 2)
South Indian Ocean SST (Feb. + March)
East Coast India temperature (March)
Arabian Sea SST (Nov. + Dec. + Jan.)
Central India temperature (May)
N H Temperature (Jan. + Feb.)
Darwin pressure tendency (April–Jan)
N H Pressure (Jan. to April)
Southern Oscillation Index (Mar to May)
Indian Ocean Equatorial Pressure (Jan to May)
Europe Pressure Gradient (January)
Argentina pressure (April)
50 hPa East–West Ridge Extension (Jan. + Feb.)
Himalayan Snow Cover (Jan. to Mar.)
Eurasian Snow Cover (Dec.)
 Methods of Predicting Indian Monsoon Rainfall

➢ IMD utilizes statistical method for making seasonal predication of

the Indian monsoon rainfall.

➢ Studies of historical data sets, over the years, have brought out
several predictors for the monsoon rainfall forecasting.

➢ The most commonly used statistical technique for seasonal

predication is the linear regression analysis.

➢ IMD has also started using dynamic model forecasts for proving
southwest monsoon rainfall.
 The Hadley Circulation

• The Hadley circulation spans half of the surface area of the

globe, and variability within this system affects the lives of
billions of people.

• Our understanding of this variability is limited to the last century

of instrumental measurements, to the even shorter record of
satellite-derived observations, or to associated modeling studies
aimed at simulating variability in the tropics associated with the
Hadley circulation.

• Only by bringing together climatologists and paleoclimatologists

on the current understanding of the Hadley circulation, by
examining paleoclimatic records that provide evidence of past
variability in this system, and model simulations of expected
future changes, a proper prediction on monsoons can be made.
 Monsoon Circulation

Hadley cell

The Hadley cell is a circulation pattern that dominates the tropical

atmosphere, with rising motion near the equator, pole ward flow 10-15
kilometers above the surface, descending motion in the subtropics, and
equator ward flow near the surface. This circulation is intimately related to
the trade winds, tropical rain belts, subtropical deserts and the jet streams.

The Hadley cell carries heat and moisture from the tropics to the northern
and southern mid-latitudes
During Monsoon season, rising limb of Hadley cell is over the Indian continent and the
sinking limb is over the equatorial Indian ocean.

Therefore the monsoons circulation is opposite to conventional Hadley circulation.

 Walker circulation

➢ The Walker circulation is an atmospheric circulation of air

at the equatorial Pacific Ocean, responsible for creating
ocean upwelling off the coasts of Peru and Ecuador.

➢ This brings nutrient-rich cold water to the surface, increasing

fishing stocks. It was discovered by Jacob Bjerknes in 1969
and was named after the English physicist Sir Gilbert Walker
who discovered the Southern Oscillation .

➢ The Walker circulation is caused by the pressure gradient

force that results from a high pressure system over the
eastern pacific ocean, and a low pressure system over
Indonesia.
It is seen at the surface as easterly trade winds which move water
and air warmed by the sun towards the west.
 HADLEY circulation is intimately related to the trade
winds, tropical rain belts, subtropical deserts and the
jet streams.

❖ The trade winds are a pattern of wind that are found in bands
around the Earth's equatorial region. The trade winds are the
prevailing winds in the tropics, blowing from the high-pressure area
in the horse latitudes towards the low-pressure area around the
equator. The trade winds blow predominantly from the northeast in
the northern hemisphere and from the southeast in the southern
hemisphere.

❖ Jet streams are fast flowing, relatively narrow air currents found in
the atmosphere at around 11 kilometres (36,000 ft) above the
surface of the Earth, just under the tropopause. They form at the
boundaries of adjacent air masses with significant differences in
temperature, such as of the polar region and the warmer air to the
south. The jet stream is mainly found in the Stratosphere.
 El Niño and La Niña relation to Indian Monsoons

El Niño and La Niña are defined as sustained sea surface temperature

anomalies of magnitude greater than 0.5°C across the central tropical
Pacific Ocean.

When the condition is met for a period of less than five months, it is
classified as El Niño or La Niña conditions; if the anomaly persists for
five months or longer, it is classified as an El Niño or La Niña episode.
Historically, it has occurred at irregular intervals of 2-7 years and has
usually lasted one or two years.

The first signs of an El Niño are:

✓ Rise in air pressure over the Indian Ocean, Indonesia, and Australia

✓ Fall in air pressure over Tahiti and the rest of the central and eastern
Pacific Ocean

✓ Trade winds in the south Pacific weaken or head east

✓ Warm air rises near Peru, causing rain in the deserts there

✓ Warm water spreads from the west Pacific and the Indian Ocean
to the east Pacific. It takes the rain with it, causing rainfall in
normally dry areas and extensive drought in eastern areas.
✓ For India a continuous and homogeneous record is available
since 1871.

✓ Monsoon rainfall is increasing (+10 to +12 % per century)

along the west coast, north Andhra Pradesh and in northwest
India. It is decreasing (-6 to –8% per century) over east
Madhya Pradesh and adjoining areas, northeast India and parts
of Gujarat and Kerala.

✓ A weak monsoon, is a result of a large negative Southern

Oscillation Index (SOI) and El Nino event.

✓ A strong monsoon, is a result of a large positive SOI and

the absence of El Nino event.

✓ During the period 1871—1999, 11 of 21 drought years were

El Nino years.

✓ The periods 1895-1932 and 1965-1987 were characterized by

frequent droughts.

✓ The periods 1872-1894 and 1933-1964 were practically

drought free
Relationship of EQUINO and ENSO over Indian Monsoon

➢ Comparison of the evolution of the normal summer monsoon of

2003 with the unanticipated drought of 2002 led to this
investigation of the role of the deep convection in the
atmosphere (deep cloud systems) over the equatorial Indian
Ocean.

➢ The link of the Indian monsoon to events over the equatorial

Indian Ocean is as important as the well-known link to the
dramatic events over the Pacific (El Niño Southern Oscillation;
ENSO).

➢ Over the equatorial Indian Ocean, enhancement of deep

convection in the atmosphere over the western part is generally
associated with suppression over the eastern part and vice versa.
This oscillation between these two states, which is reflected in
the pressure gradients and the wind along the equator, the
Equatorial Indian Ocean Oscillation (EQUINOO).
Monsoon depression

A depression that forms within the monsoon trough.

The term is most frequently used to describe weak
cyclonic disturbances that form over the Bay of
Bengal and generally track northwestward over the
Indian subcontinent. These occasionally intensify into
tropical cyclones if they remain over warm ocean
water long enough.
The criteria followed by the Meteorological Department of India to classify
the low pressure systems in the Bay of Bengal and in the Arabian Sea as
adopted by the World Meteorological Organisation (W.M.O.) are:

Associated wind speed in the

Types of Disturbances
Circulation

1. Low Pressure Area Less than 17 knots ( < 31 kmph)

2. Depression 17 to 27 knots ( 31 to 49 kmph)
3. Deep Depression 28 to 33 knots ( 50 to 61 kmph)
4. Cyclonic Storm 34 to 47 knots ( 62 to 88 kmph)
5. Severe Cyclonic Storm 48 to 63 knots ( 89 to 118 kmph)
6. Very Severe Cyclonic Storm 64 to 119 knots ( 119 to 221 kmph)
7. Super Cyclonic Storm 120 knots and above ( 222 kmph
and above)

1 knot - 1.85 km per hour

 Indian Monsoon can be affected by pollution over
Indian Ocean

❖ A dense brownish haze of microscopic pollutant particles

suspended in air (aerosols) in the Indian Ocean, discovered by an
international team of researchers, could ``affect monsoon
parameters in the long run,'' referred as Atmospheric Brown
cloud.

❖ Widespread pollution observed recently over an area as large as

the United States in the Indian Ocean including the Bay of Bengal
and the Arabian Sea could affect monsoon in the Indian
subcontinent.

❖ The extent of the effect, which depends on other factors like how
aerosols react with clouds, is being studied.
 Monsoons and Climate Change

➢ There is a competition between zonal circulation and monsoon

winds. We have to find which will be favoured by global warming.

➢ Overall, global warming will change conditions in the sea more

slowly than conditions on land, because of the difference in the
rate of response to heating, a concept familiar from the sea
breeze.

➢ Thus, we would expect the summer monsoons to be amplified by

stronger warming in summer. In addition, with more moisture in
the air, extracted from a warming ocean, rainfall (and flooding)
might be expected to increase.
➢ Conversely, in winter, we should expect less of a difference, as the
land refuses to get quite as cold as previously. So, the winter
monsoons should weaken, as should any of the nutrient-supplying
coastal upwelling associated with winter monsoons.
 Will Climate Change Affect India's Monsoon Season?

➢ Changes to India's annual monsoon are

expected to result in severe droughts and
intense flooding in parts of India.
➢ Scientists predict that by the end of the
century the country will experience a 3 to
5 degree C temperature increase and a
20% rise in all summer monsoon rainfall.
➢ Climate change studies undertaken so far Warmer temperature
reveal that action is essential in order to appear to bring
prevent long term damage to India's water
heavier rainfall
cycle.
➢ The livelihood of a vast population in India
depends on agriculture, forestry, wetlands
and fisheries and land use in these areas is
strongly influenced by water-based
ecosystems that depend on monsoon rains.
 Future changes in monsoon variability
➢ India is already vulnerable to variations in the
monsoon, both from year-to-year and within the
season.
➢ One of the key questions in climate change is whether
the remarkable stability of the monsoon rains will
continue, or whether the monsoon will become more
volatile.
➢ Most models predict a modest increase in interannual
variability but to differing degrees. At the heart of this
are the projections of what will happen to El Nino -
whether it will become stronger and/or more frequent -
since El Nino has dominant influence on monsoon
variability.
➢ Monsoon is important and scientists are engaged in
understanding the variability of monsoon using observed data
and numerical models.
➢ Hope that in future we will have more accurate prediction of
Indian monsoon rainfall.
 End of Slide Show

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