1. CLIMATE OF
INDIA
Subject: Geography
For Class: IX & XI

2. ASHUTOSH KARASHARMA MISHRA
PRESENTED BY:
ASHUTOSH KARASHARMA MISHRA
Address: (Personal)
At: Srikrisna Nagar
Po: Loisingha
Dist: Bolangir
Orissa
Address: (Official)
At: JNV, Koraput
Po: OMP Line
Dist: Koraput
Orissa
Phone No:

3. Familiarize students with the terms, key concepts and basic principles associated with the climate of India.
Provide them idea about the mechanism of Indian monsoon.
Study the climate of India through the understanding and analysis of local climate.
Explore the causative factor of the spatial variations in the climate of the country.
Understand and analyze the variation of climatic phenomenon in the cycle of seasons.
Make students aware of the change in climate (global warming) at local level to understand it at national and global level.

4. Watch Out Weather News…………….
Hot weather season
Monsoon season
Cold Weather Season
Tropical Cyclone
Four Videos Embedded:
Please right click over the dark square to choose Play or Stop one after another.

5. Please click on the box to navigate to the pages
CONTENTS OF THE LESSON
Part-I
Climatic Diversity of India
Part-II
Factors Affecting Climate of India
Part-III
Rhythm of Seasons
Part-IV
Distribution of Rainfall
Change of Climate
Part-V
Please click on the box to navigate to the pages

6. Why does weather change spatially & temporally?
Let us examine…

7. MONSOON REGIME IS THE UNITY OF INDIA
Drass -450C in December night
Tawang 190C in June
550C temperature in June
Thar desert Diurnal range of temperature 300C
Jaisalmer receives 9cm rainfall
Cherrapunji & Mawsynram have 1080cm rain
Tiruvanantapuram & Chennai 200C in December night
Kerala Diurnal range of temperature 80C
MONSOON REGIME IS THE UNITY OF INDIA

8. MORE DIVERSITIES…………………..
Churu in Rajasthan records a temperature of 50°C or more on a June day.
Snow fall over the Himalayas.
Most parts of India receives rainfall during June to September.
Tura of Meghalaya receives rainfall in a single day is equal to the total rainfall of Ten years in Jaisalmer of Rajastan.
It is 19°C in Tawang (Arunachal Pradesh) on the same day.
Only rainfall over rest of India.
Tamilnadu coast remains dry during these months.
Very low rainfall in North west Himalayas and western Rajastan which is equal to 10cm per year.
MONSOON REGIME IS THE UNITY OF INDIA

9. CLICK ON ICON TO DOWNLOAD TEMPLATE
Lets divide the class into five groups namely A, B, C, D and E.
Collect the data of temperature and rainfall of different cities of India from web site .
Collect the rainfall and temperature data of your town and compare it with the data of other cities of India.
Make a comparative study of temperature and rainfall data of different districts of Orissa. (Source- Climatological survey of Orissa & District statistical handbooks)
Write about the climate of your district and upload it to .
Make a power point presentation of all the activities you have done.
CLICK ON ICON TO DOWNLOAD TEMPLATE

10. FACTORS AFFECTING INDIAN CLIMATE
FAQ
RELATED TO LOCATION
& RELIEF
RELATED TO AIR
PRESSURE & WIND
Latitude
Surface pressure & wind
Altitude
Upper air circulation
Relief
Western cyclones
Distance from Sea
The Himalayan Mt.
Distribution of Land & water

11. LATITUDE FAQ TROPIC OF CANCER EQUATORIAL REGION High range of Temp
High Temp
Low range

12. THE HIMALAYAS- CLIMATIC BARRIER
Cold Wave
Cold Wave
Cold Wave
Cold Wave
Monsoon Wind
Monsoon Wind
Monsoon Wind
Monsoon Wind

13. DISTRIBUTION OF LAND & WATER
FAQ
HIGH PRESSURE
IN WINTER
LOW PRESSURE IN SUMMER
ARABIAN SEA
BAY OF BENGAL
INDIAN OCEAN

14. DISTANCE FROM SEA
SIMLA
DELHI
KOLKOTA
MUMBAI
CHENNAI
Coastal areas have equable climate where as Interior parts have extreme climate.

15. Temperature decreased from low to high altitude
FAQ
Temperature decreased from low to high altitude
HIGH ALTITUDE
AGRA
160C in Jan
DARJILING
40C in January
Decrease in Temperature
LOW ALTITUDE

16. Receives high rainfall
RELIEF
FAQ
Receives high rainfall
Western Ghat Mt.
Monsoon Wind
Receives low rainfall
Monsoon Wind
Monsoon Wind

17. SURFACE WIND NORTH-EAST TRADE WIND INTER TROPICAL CONVERGENCE ZONE
SUB TROPICAL HIGH PRESSURE
SUB TROPICAL LOW PRESSURE
POLAR HIGH
NORTH-EAST TRADE WIND
SOUTH-EAST TRADE WIND
POLAR HIGH

18. JET STREAM IN WINTER
TIBET

19. JET STREAM IN SUMMER

20. WESTERN DISTURBANCE
Mediterranean sea

21. Equatorial Warm Current
EL-NINO EFFECTS
FAQ
1990 Delay in Monsoon
Equatorial Warm Current
Peru
El-Nino
Homboldt Cold Current

22. SOUTHERN OSCILLATION
Darwin
Tahiti

23. CLICK ON ICON TO DOWNLOAD TEMPLATE
Prepare a ppt. answering the following:
Collect the data on the effect of El-nino over different parts of world and prepare a presentation and upload it to
Explain the factors affecting the climate of your region in a word/pdf file and upload it to or page.
Invite your friends to your or site to explain about the climate of their region.
Explain how jet stream affect the climate of India in word/pdf file and upload it to the suitable web page.
Compare how relief affect the climate of your region.
CLICK ON ICON TO DOWNLOAD TEMPLATE

24. Let us discuss each of them individually
RHYTHM OF SEASONS
HOT WEATHER
RETREATING MONSOON
COLD WEATHER
SOUTH WEST MONSOON
Let us discuss each of them individually

25. COLD WEATHER SEASON It extends from December to February.
Vertical sun rays shift towards southern hemisphere.
North India experiences intense cold where as this season is not well defined in south India.
Light wind blow makes this season pleasant in south India.
Occasional tropical cyclone visit eastern coast in this season.
Tropical Cyclone
Rhythm of Seasons

26. TEMPERATURE- JANUARY 100C` 150C 200C 200C 200C 250C 200C 250C
Rhythm of Seasons

27. PRESSURE- JANUARY
1018
HIGH PRESSURE
1019
1018
1018
1017
1016
1015
1014
Rhythm of Seasons

28. WIND DIRECTION- WINTER
Northern Plain
Ganga Delta
Bay of Bengal
Rhythm of Seasons

29. RAINFALL DUE TO WESTERN DISTURBANCES RAINFALL DUE TO NORTH EAST WIND
WINTER RAINFALL
RAINFALL DUE TO WESTERN DISTURBANCES
RAINFALL DUE TO NORTH EAST WIND
Rhythm of Seasons

30. HOT WEATHER SEASON It extends from March to May.
Vertical sun rays shift towards Northern hemisphere.
Temperature rises gradually from south to north.
Highest Temperature experiences in Karnataka in March, Madhya Pradesh in April and Rajastan in May.
May 480C
April 380C
March 300C
Rhythm of Seasons

31. TEMPERATURE- JULY
250C
200C
300C
250C
200C
300C
300C
Rhythm of Seasons

32. PRESSURE- JULY
997
998
999
1000
1001
1003
1002
1005
1004
1006
1007
Rhythm of Seasons

33. STORMS IN HOT WEATHER SEASON
FAQ
LOO
BARDOLI CHHEERHA
KALBAISAKHI
MANGO SHOWER
BLOSSOM SHOWER
Rhythm of Seasons

34. SOUTH WEST MONSOON SEASON
It extends from June to September.
Intense heating in north west India creates low pressure region.
Low pressure attract the wind from the surrounding region.
After having rains for a few days sometime monsoon fails to occur for one or more weeks is known as break in the monsoon.
HIGH TEMPERATURE
LOW PRESSURE
Rhythm of Seasons

35. INTER TROPICAL CONVERGENCE ZONE
MONSOON WIND
Arabian sea Branch
Bay of Bengal Branch
INTER TROPICAL CONVERGENCE ZONE
EQUATOR
SE Trade
SE Trade
SE Trade
SE Trade
Rhythm of Seasons

36. ONSET OF SW MONSOON 15th June 15th July 1st July 10th June 5th June
1st June
Rhythm of Seasons

37. RETREATING MONSOON SEASON
It extends from October to November
Vertical sun rays start shifting towards Northern hemisphere.
Low pressure region shift from northern parts of India towards south.
Owing to the conditions of high temperature and humidity, the weather becomes rather oppressive. This is commonly known as the ‘October heat’
LOW PRESSURE
Rhythm of Seasons

38. WITHDRAWAL OF MONSOON 15th Sept. 7th Sept. 30th Sept. 7th October
Rhythm of Seasons

39. CLICK ON ICON TO DOWNLOAD TEMPLATE
Prepare a ppt. answering the following:
Explain the seasonal difference of climate of your region in a word/pdf file and upload it to
Search friends from different parts of India and seek their comments and compare the seasonal difference in climate of different parts of India by using
Prepare an analysis of yearly temperature and rainfall data by using different graphs and upload it to
Collect photographs of monsoon and upload to or
CLICK ON ICON TO DOWNLOAD TEMPLATE

40. DISTRIBUTION OF RAINFALL
> 200cm cm cm
< 50cm

41. VARIABILITY OF RAINFALL
The variability of rainfall is computed with the help of the following formula:
C.V.= Standard Deviation/ Mean * 100
Variability of less than 25% exist in Western coasts, Western Ghats, northeastern peninsula, eastern plain of the Ganga, northern India, Uttaranchal, SW J & K & HP.
Variability of more then 50% found in Western Rajastan, J & K and interior parts of Deccan.
Region with high rainfall has less variability.

42. CLICK ON ICON TO DOWNLOAD TEMPLATE
Prepare a power point presentation answering the following:
Why there is variation of rainfall in different parts of India? Explain in a word/pdf file and upload.
Calculate the variability of rainfall of your region.
Compare the variability of rainfall with the total rainfall of your region.
Measure the rainfall in your school and record it in a spread sheet for analysis.
Read out the rainfall and temperature data of your school daily in the morning assembly.
CLICK ON ICON TO DOWNLOAD TEMPLATE

43. INCREASE IN GREEN HOUSE GASES SPREAD OF TROPICAL DISEASES
CLIMATE CHANGE
RISE IN
TEMPERATURE
INCREASE IN GREEN HOUSE GASES
MELTING OF ICE
SEA LEVEL RISE
SINKING COAST
TSUNAMI & EARTHQUAKE
FLOOD
EXCESSIVE SUN STROKE
LOSS OF BIODIVERSITY
FOREST FIRE
FOOD SCARCITY
SPREAD OF TROPICAL DISEASES
IMPACT OF GLOBAL WORMING

44. SOME INTERESTING FACTS
Temperature increased by 0.60C in 20th century.
Eleven out of twelve hottest years are within 1995 to 2006.
Annual rate of increase of CO2 is 1.9ppm after 1995.
Concentration of methane increased from 700ppb in 1750 to 1745ppb at present and Nitrous Oxide from 270ppb to 314ppb where as CFC increased from zero to 533ppb.
Rising of temperature to 30C will lead to melting of all ice on earth surface and sea level rise upto 15 feet.
Existence of large cities like Venis, Bankok, Sanghai, Kolkota and Dhaka will be in danger.
FAQ

45. CLIMATE CHANGE & INDIA
India has long coast line and rise of sea level will submerge large area.
A population of 7.1 million living in coastal areas will be affected.
Production of crops like wheat, rice etc will decrease.
The natural disasters like cyclone, floods and drought will increase in frequency as well as intensity.
KOLKOTA
MUMBAI
CHENNAI

46. WHAT CAN BE DONE???
Switch off the light, fan, TV and other energy using gadgets when they are not in use.
Do not use those equipments that pollute or consume more energy.
create public awareness.
use renewable energy resources like solar, wind, biomass etc.
International conferences like Earth Summit, 1992, Kyoto protocol, Copenhegen summit, 2009 are some steps to bring consensus for crusade against Climate Change.

47. CLICK ON ICON TO DOWNLOAD TEMPLATE
Ask elders of your family or village about their perception of change in climate and explain it in a word/pdf file and upload it to .
Give an analysis of change in temperature of your region by collecting data of fifteen years from climatological survey of orissa.
Explain what you can do to reduce the impact of climate change.
Ask your friends through about their contribution to reduce the impact of climate change.
Prepare a power point presentation explaining all above.
CLICK ON ICON TO DOWNLOAD TEMPLATE

48. TEST YOUR KNOWLEDGE Name the factors affecting climate of India .
What is meant by El-nino?
Why the south western part of peninsular India receives high rainfall?
Name the important green house gases.
How altitude affects climate?
How distance from sea affect climate?
What is meant by mango shower?
What is meant by Inter Tropical Convergence Zone?
Answer
Answer
Answer
Answer
Answer
Answer
Answer
Answer

49. Evaluate the classroom presentation of other groups and assign marks.
EVALUATION RUBRIC Sl
No.
Evaluation points
Excellent
Very Good
Good 1
Participation of all members of the group
All the members have participated
(5 Marks)
Some Members have participated.
(3 Marks)
Few members have participated.
(2 Marks) 2
Efficient use of technology in self-learning
Technology used for presentation, collection of information and understanding.
Technology used for presentation and collection of information.
Technology used for presentation only. 3
Collection of new information
Information collected are new, relevant and latest.
Information collected are new and relevant.
Information collected are new only. 4
Presentation of Topic in the classroom
Presentation of topic was clear, able to clarify doubts and with proper flow of topic.
Presentation of topic was clear and able to clarify doubts.
Presentation of topic was clear only. 5
Development of Innovative Thinking
Innovation in presentation, collection of new information and use of technology.
Innovation in presentation and collection of new information.
Innovation in presentation only.
Total 25 15 10
Mark Obtained
Evaluate the classroom presentation of other groups and assign marks.

50. CITATION
Abraham, K.R.; Dash, S.K. and Mohanty, U.C., 1996: Simulation of monsoon circulation and cyclones with different types of orography; Mausam, 47,
Ashok K., S. Lizuka, S.A Rao, N. H. Saji and W. Lee, 2009 : Processes and boreal summer impacts of the 2004 El Nino Modoki: An AGCM study. Geophysical Research Letters, 36, L04703, doi: /2008GL036313, 1-5.
Bannerji, S. K., 1950 : Methods of forecasting monsoon and winter rainfall in India. Ind. J. Met. and Geophys., 4,
Bhalme, H.N. and Jadhav, S.K., 1984: The southern oscillation and its relation to the monsoon rainfall. J.Climatol., 4,
Krishnakumar V. and K. ‑M. Lau, 1997 : Symmetric Instability of Monsoon Flows. Tellus 49 A, 228‑245.
Physical Geography of India, NCERT, class-IX
Economic & Commercial Geography of India, C.B. Memoria.
Regional Geography of India, R.L. Singh.

51. Heartiest Thanks to ACKNOWLEDGEMENT
Mr. S. K. Tripathy, Principal JNV, Koraput
Mr. R. P. Maharana, TGT-English, JNV, Koraput
Project Learning, Microsoft, for providing me training.