climate of india

Subject: Geography

For Class: IX & XI

PRESENTED BY:PRESENTED BY:

ASHUTOSH KARASHARMA MISHRAASHUTOSH KARASHARMA MISHRA

Address: (Personal) At: Srikrisna Nagar

Po: LoisinghaDist: BolangirOrissa-767020

Address: (Official) At: JNV, Koraput

Po: OMP LineDist: KoraputOrissa

Phone No: 9437146288

E-mail: [email protected][email protected]

mailto:[email protected]

mailto:[email protected]

►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.

►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.

Hot weather seasonHot weather season Monsoon seasonMonsoon season

Tropical Cyclone Tropical Cyclone Cold Weather SeasonCold Weather Season

Watch Out Weather News…………….Watch Out Weather News…………….

Four Videos Embedded:

Please right click over the dark square to choose Play or Stop one after another.

Four Videos Embedded:

Please right click over the dark square to choose Play or Stop one after another.

Part-I Climatic Diversity of India

Part-II Factors Affecting Climate of India

Part-III

Part-IV

Rhythm of Seasons

Distribution of Rainfall

Change of ClimatePart-V

CONTENTS OF THE LESSON

Please click on the box to navigate to the pagesPlease click on the box to navigate to the pages

Let us examine…Let us examine…

Why does weather change

spatially & temporally?Why does weather change

spatially & temporally?

550C temperature in June

Tawang 190C in June

Drass -450C in December night

Tiruvanantapuram & Chennai 200C in December night

Kerala Diurnal range of

temperature 80C

Thar desert Diurnal range of temperature 300C

Cherrapunji & Mawsynram have

1080cm rain

MONSOON REGIME IS THE UNITY OF INDIAMONSOON REGIME IS THE UNITY OF INDIA

Jaisalmer receives 9cm

rainfall

MORE DIVERSITIES…………………..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.

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.

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 INDIAMONSOON REGIME IS THE UNITY OF INDIA

► 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 www.allrainfallreports.com .

► 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 1987-2003 & District statistical handbooks)

► Write about the climate of your district and upload it to www.climateofindia.pbwiki.com .

► Make a power point presentation of all the activities you have done.

► 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 www.allrainfallreports.com .

► 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 1987-2003 & District statistical handbooks)

► Write about the climate of your district and upload it to www.climateofindia.pbwiki.com .

► Make a power point presentation of all the activities you have done.

CLICK ON ICON TO DOWNLOAD TEMPLATEDownload Template

http://www.allrainfallreports.com/

http://www.climateofindia.pbwiki.com/

http://www.allrainfallreports.com/


FACTORS AFFECTING INDIAN CLIMATEFACTORS AFFECTING INDIAN CLIMATE

RELATED TO LOCATION & RELIEF

RELATED TO AIR PRESSURE & WIND

•Latitude•Latitude

•The Himalayan Mt.•The Himalayan Mt.

•Distribution of Land & water•Distribution of Land & water

•Distance from Sea•Distance from Sea

•Altitude•Altitude

•Relief•Relief

Surface pressure & windSurface pressure & wind

Upper air circulationUpper air circulation

Western cyclonesWestern cyclones

FAQFAQ

EQUATORIAL REGION

TROPIC OF CANCER

LATITUDELATITUDE

High Temp

Low range

High Temp

Low range

High range of Temp

High range of Temp

FAQFAQ

THE HIMALAYAS- CLIMATIC BARRIERTHE HIMALAYAS- CLIMATIC BARRIER

Mo

nso

on

Win

d

Mo

nso

on

Win

d

Mo

nso

on

Win

d

Mo

nso

on

Win

d

Co

ld W

aveC

old

Wave

Co

ld W

ave

Co

ld W

ave

ARABIAN SEA

ARABIAN SEA BAY OF

BENGALBAY OF BENGAL

INDIAN OCEANINDIAN OCEAN

DISTRIBUTION OF LAND & WATERDISTRIBUTION OF LAND & WATER

LOW PRESSURE IN SUMMER

HIGH PRESSURE IN WINTER

FAQFAQ

MUMBAIMUMBAI

CHENNAICHENNAI

KOLKOTAKOLKOTA

DELHIDELHI

SIMLASIMLA

DISTANCE FROM SEADISTANCE FROM SEA

Coastal areas have equable climate where as Interior parts have extreme climate.

Coastal areas have equable climate where as Interior parts have extreme climate.

AGRA160C in Jan

AGRA160C in Jan

DARJILING40C in January

DARJILING40C in January

ALTITUDEALTITUDE

HIGH ALTITUDEHIGH ALTITUDE

LOW ALTITUDELOW ALTITUDE

Temperature decreased from low to high altitudeTemperature decreased from low to high altitude

Dec

reas

e in

Tem

pera

ture

FAQFAQ

Monsoo

n Wind

Monsoo

n Wind

Monsoo

n Wind

Receives high rainfall

Receives low rainfall

RELIEFRELIEF

Western G

hat Mt.

FAQFAQ

NORTH-EAST TRADE WIND

SOUTH-EAST TRADE WIND

INTER TROPICAL CONVERGENCE ZONE

SUB TROPICAL HIGH PRESSURE

SUB TROPICAL HIGH PRESSURE

SUB TROPICAL LOW PRESSURE

SUB TROPICAL LOW PRESSURE

POLAR HIGH

POLAR HIGH

SURFACE WINDSURFACE WIND

TIBET

JET STREAM IN WINTERJET STREAM IN WINTER

JET STREAM IN SUMMERJET STREAM IN SUMMER

Mediterranean seaMediterranean sea

WESTERN DISTURBANCEWESTERN DISTURBANCE

Homboldt Cold Current

EL-NINO EFFECTSEL-NINO EFFECTS

Peru

1990 Delay in Monsoon

Equatorial Warm Current

El-Nino

FAQFAQ

DarwinTahiti

SOUTHERN OSCILLATIONSOUTHERN OSCILLATION

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 www.climateofindia.pbwiki.com.

►Explain the factors affecting the climate of your region in a word/pdf file and upload it to www.think.com or www.climateofindia.pbwiki.com page.

►Invite your friends to your www.think.com or www.epal.com 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.

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 www.climateofindia.pbwiki.com.

►Explain the factors affecting the climate of your region in a word/pdf file and upload it to www.think.com or www.climateofindia.pbwiki.com page.

►Invite your friends to your www.think.com or www.epal.com 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 TEMPLATEMicrosoft

PowerPoint Presentation


http://www.think.com/



http://www.epal.com/





http://www.epal.com/

RHYTHM OF SEASONSRHYTHM OF SEASONS

COLD WEATHERCOLD WEATHER

RETREATING MONSOONRETREATING MONSOONHOT WEATHERHOT WEATHER

SOUTH WEST MONSOONSOUTH WEST MONSOON

Let us discuss each of them individuallyLet us discuss each of them individually

COLD WEATHER SEASONCOLD 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.

► 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 SeasonsRhythm of Seasons

250C

250C

200C

200C200C

150C

200C

100C`

TEMPERATURE- JANUARYTEMPERATURE- JANUARY


PRESSURE- JANUARYPRESSURE- JANUARY

10191018

1018

10181017

1016

1015

1014

HIGH PRESSURE


Ganga

Delta

Northern Plain

WIND DIRECTION- WINTERWIND DIRECTION- WINTER

Bay of Bengal


WINTER RAINFALLWINTER RAINFALL

RAINFALL DUE TO WESTERN

DISTURBANCES

RAINFALL DUE TO NORTH EAST

WIND


HOT WEATHER SEASONHOT 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.

► 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.

March 300CMarch 300C

April 380CApril 380C

May 480CMay 480C


TEMPERATURE- JULYTEMPERATURE- JULY

200C

250C

300C

20 0C

300C

25 0C

30 0C


PRESSURE- JULYPRESSURE- JULY

997

998 999

1000

10011002

100310041005

10061007


LOOLOO

KALBAISAKHIKALBAISAKHI

BARDOLI CHHEERHABARDOLI

CHHEERHA

MANGO SHOWERMANGO

SHOWER

BLOSSOM SHOWER

BLOSSOM SHOWER

STORMS IN HOT WEATHER SEASONSTORMS IN HOT WEATHER SEASON

FAQFAQ


SOUTH WEST MONSOON SEASONSOUTH 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.

► 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 TEMPERATURELOW PRESSURE


INTER TROPICAL CONVERGENCE ZONEEQUATOR

MONSOON WINDMONSOON WIND

SE Tra

de

SE Tra

de

SE Tra

de

SE Tra

de

Arabian sea Branch

Arabian sea Branch

Bay of Bengal Branch

Bay of Bengal Branch


ONSET OF SW MONSOONONSET OF SW MONSOON

1st J

une

5th Ju

ne10

th June

15th J

une

1st J

uly

15th Ju

ly


► 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’

► 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’

RETREATING MONSOON SEASONRETREATING MONSOON SEASON

LOW PRESSURE


15th O

ctobe

r

7th O

ctobe

r30th S

ept.

15th S

ept.

7th S

ept.

WITHDRAWAL OF MONSOONWITHDRAWAL OF MONSOON


Prepare a ppt. answering the following:►Explain the seasonal difference of climate of your

region in a word/pdf file and upload it to www.climateofindia.pbwiki.com.

►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 www.think.com.

►Prepare an analysis of yearly temperature and rainfall data by using different graphs and upload it to www.climateofindia.pbwiki.com.

►Collect photographs of monsoon and upload to www.think.com or www.climateofindia.pbwiki.com.

Prepare a ppt. answering the following:►Explain the seasonal difference of climate of your

region in a word/pdf file and upload it to www.climateofindia.pbwiki.com.

►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 www.think.com.

►Prepare an analysis of yearly temperature and rainfall data by using different graphs and upload it to www.climateofindia.pbwiki.com.

►Collect photographs of monsoon and upload to www.think.com or www.climateofindia.pbwiki.com.

CLICK ON ICON TO DOWNLOAD TEMPLATE

Microsoft PowerPoint Presentation











DISTRIBUTION OF RAINFALLDISTRIBUTION OF RAINFALL

> 200cm

100-200cm

50-100 cm

< 50cm

► 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.

► 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.

VARIABILITY OF RAINFALLVARIABILITY OF RAINFALL

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.

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.

Download Template


CLIMATE CHANGECLIMATE CHANGE

RISEIN

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

►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.

►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.

SOME INTERESTING FACTSSOME INTERESTING FACTS

FAQFAQ

CLIMATE CHANGE & INDIACLIMATE 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.

► 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.

MUMBAIMUMBAI

CHENNAICHENNAI

KOLKOTAKOLKOTA

WHAT CAN BE DONE???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.

►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.

►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 www.climateofindia.pbwiki.com .

►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 www.think.com about their contribution to reduce the impact of climate change.

►Prepare a power point presentation explaining all above.

►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 www.climateofindia.pbwiki.com .

►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 www.think.com about their contribution to reduce the impact of climate change.

►Prepare a power point presentation explaining all above.


Download Template





1. Name the factors affecting climate of India .

2. What is meant by El-nino?

3. Why the south western part of peninsular India receives high rainfall?

4. Name the important green house gases.

5. How altitude affects climate?

6. How distance from sea affect climate?

7. What is meant by mango shower?

8. What is meant by Inter Tropical Convergence Zone?

1. Name the factors affecting climate of India .

2. What is meant by El-nino?

3. Why the south western part of peninsular India receives high rainfall?

4. Name the important green house gases.

5. How altitude affects climate?

6. How distance from sea affect climate?

7. What is meant by mango shower?

8. What is meant by Inter Tropical Convergence Zone?

TEST YOUR KNOWLEDGETEST YOUR KNOWLEDGE

AnswerAnswer

AnswerAnswer

AnswerAnswer

AnswerAnswer

AnswerAnswer

AnswerAnswer

AnswerAnswer

AnswerAnswer

EVALUATION RUBRIC EVALUATION RUBRIC SlNo.

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.(5 Marks)

Technology used for presentation and collection of information.(3 Marks)

Technology used for presentation only.(2 Marks)

3

Collection of new information

Information collected are new, relevant and latest.(5 Marks)

Information collected are new and relevant.(3 Marks)

Information collected are new only.(2 Marks)

4

Presentation of Topic in the classroom

Presentation of topic was clear, able to clarify doubts and with proper flow of topic.(5 Marks)

Presentation of topic was clear and able to clarify doubts.(3 Marks)

Presentation of topic was clear only.(2 Marks)

5

Development of Innovative Thinking

Innovation in presentation, collection of new information and use of technology.(5 Marks)

Innovation in presentation and collection of new information.(3 Marks)

Innovation in presentation only.(2 Marks)

Total 25 15 10

Mark Obtained

Evaluate the classroom presentation of other groups and assign marks.Evaluate the classroom presentation of other groups and assign marks.

CITATIONCITATION► Abraham, K.R.; Dash, S.K. and Mohanty, U.C., 1996: Simulation of

monsoon circulation and cyclones with different types of orography; Mausam, 47, 235-248.

► 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:10.1029/2008GL036313, 1-5.

► Bannerji, S. K., 1950 : Methods of forecasting monsoon and winter rainfall in India. Ind. J. Met. and Geophys., 4, 343-346.

► Bhalme, H.N. and Jadhav, S.K., 1984: The southern oscillation and its relation to the monsoon rainfall. J.Climatol., 4, 509-520.

► 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.► www.imd.gov.in► http://tinyurl.com/q4a6mg► http://timesofindia.indiatimes.com/articleshow/4755025.cms► http://www.nws.noaa.gov/ost/climate/STIP

► Abraham, K.R.; Dash, S.K. and Mohanty, U.C., 1996: Simulation of monsoon circulation and cyclones with different types of orography; Mausam, 47, 235-248.

► 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:10.1029/2008GL036313, 1-5.

► Bannerji, S. K., 1950 : Methods of forecasting monsoon and winter rainfall in India. Ind. J. Met. and Geophys., 4, 343-346.

► Bhalme, H.N. and Jadhav, S.K., 1984: The southern oscillation and its relation to the monsoon rainfall. J.Climatol., 4, 509-520.

► 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.► www.imd.gov.in► http://tinyurl.com/q4a6mg► http://timesofindia.indiatimes.com/articleshow/4755025.cms► http://www.nws.noaa.gov/ost/climate/STIP

ACKNOWLEDGEMENTACKNOWLEDGEMENT

Heartiest Thanks toHeartiest Thanks to

Mr. S. K. Tripathy, Principal JNV, Koraput

Mr. R. P. Maharana, TGT-English, JNV, Koraput

Project Learning, Microsoft, for providing me training.

Mr. S. K. Tripathy, Principal JNV, Koraput

Mr. R. P. Maharana, TGT-English, JNV, Koraput

Project Learning, Microsoft, for providing me training.

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temperature data

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total rainfall

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rainfall data of koraput

temperature rainfallrepresent