SlideShare a Scribd company logo
1 of 21
CLIMATOLOGY L-2
PRESSURE SYSTEM OF THE WORLD
 4 BELTS IN THE WORLD
EQUITORIAL LOW PRESSURE BELT
ABSENCE OF ADVECTION OF AIR
BELT OF CALM / DOLDRUM
LIGHT FEEBLE WIND
SUB TROPICAL HIGH PRESSURE BELT
 AKA HORSE LATITUDE
 THE AIR ABOVE EQUATOR MOVES TOWARDS POLES
BUT THEIR PATH DEFLECTED DUE TO CORIOLIS FORCE
( PATH LENGTH INCREASES), ENERGY REDUCED IN MID
PATH & COOLS DOWN.
SUBPOLAR LOW PRESSURE BELT
 COLD WIND FROM POLES MOVES TOWARDS EQUATOR ,
COLLIDE WITH WARM WINDS FROM SUBTROPICAL
HIGH PRESSURE AND WARM WIND RISE UP. THIS
CREATES A LOW PRESSURE.
POLAR HIGH
 AIR ARISEN AT SPLP DESCENDS AT POLES WHICH GIVE
RISE TO HIGH PRESSURE CONDITION . THIS HIGH
PRESSURE IS THERMALLY INDUCED.
PLANETARY WINDS
 HORIZONTAL WINDS
 PRESSURE BELT SYSTEM PROVIDES THEM THE PRESSURE GRADIENT.
 CORIOLIS FORCE MODIFY THEIR DIRECTION ( WIND BLOWS IN SAME DIRECTION
THROUGHOUT YEAR).
TYPE OF WINDS
 TRADE WINDS –MOVE TOWARDS ITCZ , DIRECTION IS EAST
TO WEST DUE TO CORIOLIS FORCE .
 WESTERLIES –FROM WEST TO EAST , FROM STHP TO SPLP.
 0 – 30 DEGREE –TRADE WINDS ( PLACE OF ITCZ ).
 30 – 60 DEGREE – WESTERLIES
 60 – 90 DEGREE – POLAR EASTERLIES
 SEASONAL WINDS – IN WINTER –FROM NORTH TO SOUTH
 - IN SUMMER – FROM SOTH TO NORTH
 LOCAL COLD WINDS IN SIBERIA – BURAN
 LOCAL COLD WINDS IN CANADA - BLIZZARD
TYPES OF WIND
UPPER TROPOSPHERIC WINDS
 WIND ACCUMULATED ABOVE EQUATOR AND START
MOVING TOWARDS POLES .
 MOVE UPWARDS TILL TROPOPAUSE ( FACE CORIOLIS
FORCE THERE).
 AKA GEO STRATIC WINDS
 DUE TO LESS FRICTION & HIGH SPEED, THEY ARE VERY
STRONG WINDS .
 THESE WINDS ARE WESTERLIES WINDS.
 ALMOST 90 DEGREE DEFLECTION DUE TO CORIOLIS
FORCE
TYPES OF WINDS
 ROOSBY WAVES – MEANDERATION OF
WESTERLIES TO MAINTAIN ANGULAR
MUMENTAM.
 JET STREAMS – AT THE MARGINS OF HEAT
CELLS
 4 PERMANENT- 2 POLAR JET & 2 SUBTROPICAL
WETERLY JET STREAM.
 TEMPORARY JET STREAM AT WESTERN INDIA
FROM EQUATOR IN THE MONTHS OF JUNE –
JULY – AUGUST.
OMEGA BLOCK / TRAVELLING DEPRESSION
 JET STREAMS EMBEDDED IN
WESTERLIES CAUSE PRESSURE
VARIABILITY THATSWHY TRAVELLING
DEPRESSISON.
 THE MEETING REGION OF TWO MASSES
IS KNOWN AS FRONT.
CONDITIONS OF LOW PRESSURE
THERMALLY INDUCED
 BECAUSE OF HIGH TEMPERATURE
 EX – LOW PRESSURE AT EQUATOR
 CONVENTIONAL RAINFALL AT
EQUATOR.
DYNAMICALLY INDUCED
 UPLIFTMENT OF WARM AIR
 EX – LOW PRESSURE AT SUBPOLAR
LP BELT
 FRONTAL RAINFALL
DEVELOPMENT OF FRONTAL CYCLONES
 WHEN AIRMASS MOVES FROM THEIR SOURCE REGION (
WARM AND COLD AIRMASS FACE EACH OTHER ),
FRONT IS CREATED BETWEEN THEM CALLED
STATIONARY FRONT, THEN START CIRCULAR
MOVEMENT.
 COLD AIR MAS PUSHES THE WARM AIRMASS , FORCED
UPLIFTMENT OF AIR , CIRCULAR DUE TO CORIOLIS
FORCE.
TYPES OF CYCLONE
EYE OF CLONE – HP , WALL- LP
TEMPERATE CYCLONE
 30 – 40 DEGREE LATITUDE
 DYNAMICALY INDUCED THROUGH
FRONTAL INTERACTION
 WEST TO EAST MOVEMENT IN
LARGE AREAS
 POWERFULL ON LAND
 AFFECT MAINLAND
TROPICAL CYCLONE
 8 – 20 DEGREE LATITUDE
 THERMALLY INDUCED , AIR RISES
ABOVE & CORIOLIS FORCE AFFECTS.
 EAST TO WEST ( SMALL AREAS)
 WEAKER ON LAND
 AFFECT COASTAL AREAS
 REASONS – TROPICAL WARM WATER,
WARM OCEAN CURRENT
THUNDERSTORM
 THUNDERSTORMS FORMS CUMULONIMBUS CLOUDS
 THUNDERING & LIGHTNING CLOUDS ACCUMULATES +VE CHARGE AT HIGH &
LOW POSITIONS & - VE CHARGE INBETWEEN.
 TYPES OF THUNDERSTORMS
 THERMAL – LOCALISED INTENSE HEATING OF CLOUDS
 OROGRAPHIC – WHEN WARM MOIST AIR PASSES OVER MOUNTAINS
 COLD FRONT – FORCEFULL UPLIFTMENT OF WARM MOIST AIR
TORNADO
 INTENSE LOW PRESSURE SYSTEM
 WHEN TORNADO PASSES OVER A WATERBODY , WATER IS SUCKED UP CALLED
WATER FRONT.
 OCCURS MOSTLY IN TEMPERATE REGIONS ( 20-60 ) DEGREE.
POLAR VORTEX
 LARGE SCALE ( 1000 KM SQ) CYCLONE AT POLES IN WINTER.
 DEVELOPS AT UPPER TROPOSPHERE AND STRATOSPHERE.
 DEVELPOPS DUE TO DIFFERENTIAL CREATED BTW EQUATOR AND POLES .
 DEVELOPMENT OF POLAR NIGHT JET STREAMS.
 ROOSBY WAVES CAN DIRUPT THEIR MOVEMENT.
OZONE DEPLETION
 INCREASE CHLORINE CONCENTRATION IN WINTERS , OZONE DEPLETION IN
SUMEMR.
 POLAR VORTEX IS WEAK IN NORTERN HEMISPHERE ( ARTIC ) DUE TO OZONE
DEPLETION.
 OZONE DEPLETION AT ARTIC KNOWN AS OZONE DENT.
 OZONE DEPLETION AT ANTARTIC KNOWN AS OZONE HOLE .
PRESSURE GRADIENT CELLS
 VERTICAL – HADLEY CELL ( EQUATOR TO TROPIC )& FERREL( TROPIC TO POLES )
 HORIZONTAL – WALKER ( FROM PERU TO AUSTRALIA ) AKA ENSO – EL NINO
SOUTHERN OSCILATAION.
 EL NINO – REVERSAL OF ATMOSPHERIC & OCEANIC ACTIVITIES RESULTING IN
RAINFALL AND DROUGHT.
 LA NINO – INTENSIFICATION OF NATURAL ACTIVITIES.
CLIMATIC REGIONS OF THE
WORLD WILL BE COVERED
AFTER INDIAN GEOGRAPHY.

More Related Content

Similar to climatology l 2.pptx

Similar to climatology l 2.pptx (20)

Gd Club Pilot meteorology
Gd Club Pilot meteorologyGd Club Pilot meteorology
Gd Club Pilot meteorology
 
Ocean properties
Ocean propertiesOcean properties
Ocean properties
 
Atmosphere
AtmosphereAtmosphere
Atmosphere
 
Cyclone update 4 dec
Cyclone update 4 decCyclone update 4 dec
Cyclone update 4 dec
 
Earth science
Earth science Earth science
Earth science
 
Wind Energy Course - Mughal
Wind Energy Course - MughalWind Energy Course - Mughal
Wind Energy Course - Mughal
 
Tropical cyclones and temperate cyclones
Tropical cyclones and temperate cyclonesTropical cyclones and temperate cyclones
Tropical cyclones and temperate cyclones
 
Earth Science SOL Review
Earth Science SOL ReviewEarth Science SOL Review
Earth Science SOL Review
 
Financing Disaster Risk in India
Financing Disaster Risk in IndiaFinancing Disaster Risk in India
Financing Disaster Risk in India
 
2019 tg atmosphere2 atmospheric circulation
2019 tg atmosphere2 atmospheric circulation2019 tg atmosphere2 atmospheric circulation
2019 tg atmosphere2 atmospheric circulation
 
Climate
ClimateClimate
Climate
 
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology ChapterAtmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
 
Factors affecting the climate
Factors affecting the climateFactors affecting the climate
Factors affecting the climate
 
A Look Into Climate Types
A Look Into Climate TypesA Look Into Climate Types
A Look Into Climate Types
 
Storm Surges
Storm SurgesStorm Surges
Storm Surges
 
Air Masses, Global Winds, and Fronts
Air Masses, Global Winds, and FrontsAir Masses, Global Winds, and Fronts
Air Masses, Global Winds, and Fronts
 
ATMOSPHERIC PRESSURE AND WINDS copy.pptx
ATMOSPHERIC PRESSURE AND WINDS copy.pptxATMOSPHERIC PRESSURE AND WINDS copy.pptx
ATMOSPHERIC PRESSURE AND WINDS copy.pptx
 
Pertemuan 03 front
Pertemuan 03 frontPertemuan 03 front
Pertemuan 03 front
 
Chapt15 lecture
Chapt15 lectureChapt15 lecture
Chapt15 lecture
 
COOLING TOWER BASIC.pptx
COOLING TOWER BASIC.pptxCOOLING TOWER BASIC.pptx
COOLING TOWER BASIC.pptx
 

More from TrinityEducationDefe

More from TrinityEducationDefe (16)

BGMI 2, role of human sciences and nature.pptx
BGMI 2, role of human sciences and nature.pptxBGMI 2, role of human sciences and nature.pptx
BGMI 2, role of human sciences and nature.pptx
 
Plant_Classification1 in plant kingdom .._PPT1.ppt
Plant_Classification1 in plant kingdom .._PPT1.pptPlant_Classification1 in plant kingdom .._PPT1.ppt
Plant_Classification1 in plant kingdom .._PPT1.ppt
 
IB ACIO MATHS FOR VARIOUS DEFENCE EXAMINATIONS .pptx
IB ACIO MATHS FOR VARIOUS DEFENCE EXAMINATIONS .pptxIB ACIO MATHS FOR VARIOUS DEFENCE EXAMINATIONS .pptx
IB ACIO MATHS FOR VARIOUS DEFENCE EXAMINATIONS .pptx
 
microbialdiseasesfor rimc -160303140348.pptx
microbialdiseasesfor rimc -160303140348.pptxmicrobialdiseasesfor rimc -160303140348.pptx
microbialdiseasesfor rimc -160303140348.pptx
 
fundamental geography.PDF
fundamental geography.PDFfundamental geography.PDF
fundamental geography.PDF
 
percentage.pptx
percentage.pptxpercentage.pptx
percentage.pptx
 
geography part 2.pptx
geography part 2.pptxgeography part 2.pptx
geography part 2.pptx
 
economy lec 1.pptx
economy lec 1.pptxeconomy lec 1.pptx
economy lec 1.pptx
 
AFCAT (1) 2023 CURRENT AFFAIRS.pptx
AFCAT (1) 2023 CURRENT AFFAIRS.pptxAFCAT (1) 2023 CURRENT AFFAIRS.pptx
AFCAT (1) 2023 CURRENT AFFAIRS.pptx
 
ANCIENT HISTORY PART 2.pptx
ANCIENT HISTORY PART 2.pptxANCIENT HISTORY PART 2.pptx
ANCIENT HISTORY PART 2.pptx
 
Digestive System PPT.ppt
Digestive System PPT.pptDigestive System PPT.ppt
Digestive System PPT.ppt
 
GEOGRAPHY L 1.pptx
GEOGRAPHY L 1.pptxGEOGRAPHY L 1.pptx
GEOGRAPHY L 1.pptx
 
scientificinstruments-150510102849-lva1-app6891.pptx
scientificinstruments-150510102849-lva1-app6891.pptxscientificinstruments-150510102849-lva1-app6891.pptx
scientificinstruments-150510102849-lva1-app6891.pptx
 
inventionsandinventors-151206170858-lva1-app6892 (1).pptx
inventionsandinventors-151206170858-lva1-app6892 (1).pptxinventionsandinventors-151206170858-lva1-app6892 (1).pptx
inventionsandinventors-151206170858-lva1-app6892 (1).pptx
 
cds nda biology.pptx
cds nda biology.pptxcds nda biology.pptx
cds nda biology.pptx
 
PARAGRAPH WRITING (2).pptx
PARAGRAPH WRITING (2).pptxPARAGRAPH WRITING (2).pptx
PARAGRAPH WRITING (2).pptx
 

Recently uploaded

microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introductionMaksud Ahmed
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxVishalSingh1417
 
Sanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfSanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfsanyamsingh5019
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeThiyagu K
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingTeacherCyreneCayanan
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsTechSoup
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Disha Kariya
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityGeoBlogs
 
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...fonyou31
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxiammrhaywood
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpinRaunakKeshri1
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactPECB
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfciinovamais
 
Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)eniolaolutunde
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactdawncurless
 
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...christianmathematics
 
The basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptxThe basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptxheathfieldcps1
 

Recently uploaded (20)

microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introduction
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptx
 
Sanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfSanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdf
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writing
 
Mattingly "AI & Prompt Design: The Basics of Prompt Design"
Mattingly "AI & Prompt Design: The Basics of Prompt Design"Mattingly "AI & Prompt Design: The Basics of Prompt Design"
Mattingly "AI & Prompt Design: The Basics of Prompt Design"
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The Basics
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activity
 
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpin
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global Impact
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
 
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptxINDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
 
Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
 
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
 
Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1
 
The basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptxThe basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptx
 

climatology l 2.pptx

  • 2. PRESSURE SYSTEM OF THE WORLD  4 BELTS IN THE WORLD
  • 3. EQUITORIAL LOW PRESSURE BELT ABSENCE OF ADVECTION OF AIR BELT OF CALM / DOLDRUM LIGHT FEEBLE WIND
  • 4. SUB TROPICAL HIGH PRESSURE BELT  AKA HORSE LATITUDE  THE AIR ABOVE EQUATOR MOVES TOWARDS POLES BUT THEIR PATH DEFLECTED DUE TO CORIOLIS FORCE ( PATH LENGTH INCREASES), ENERGY REDUCED IN MID PATH & COOLS DOWN.
  • 5. SUBPOLAR LOW PRESSURE BELT  COLD WIND FROM POLES MOVES TOWARDS EQUATOR , COLLIDE WITH WARM WINDS FROM SUBTROPICAL HIGH PRESSURE AND WARM WIND RISE UP. THIS CREATES A LOW PRESSURE.
  • 6. POLAR HIGH  AIR ARISEN AT SPLP DESCENDS AT POLES WHICH GIVE RISE TO HIGH PRESSURE CONDITION . THIS HIGH PRESSURE IS THERMALLY INDUCED.
  • 7. PLANETARY WINDS  HORIZONTAL WINDS  PRESSURE BELT SYSTEM PROVIDES THEM THE PRESSURE GRADIENT.  CORIOLIS FORCE MODIFY THEIR DIRECTION ( WIND BLOWS IN SAME DIRECTION THROUGHOUT YEAR).
  • 8. TYPE OF WINDS  TRADE WINDS –MOVE TOWARDS ITCZ , DIRECTION IS EAST TO WEST DUE TO CORIOLIS FORCE .  WESTERLIES –FROM WEST TO EAST , FROM STHP TO SPLP.  0 – 30 DEGREE –TRADE WINDS ( PLACE OF ITCZ ).  30 – 60 DEGREE – WESTERLIES  60 – 90 DEGREE – POLAR EASTERLIES  SEASONAL WINDS – IN WINTER –FROM NORTH TO SOUTH  - IN SUMMER – FROM SOTH TO NORTH  LOCAL COLD WINDS IN SIBERIA – BURAN  LOCAL COLD WINDS IN CANADA - BLIZZARD
  • 9. TYPES OF WIND UPPER TROPOSPHERIC WINDS  WIND ACCUMULATED ABOVE EQUATOR AND START MOVING TOWARDS POLES .  MOVE UPWARDS TILL TROPOPAUSE ( FACE CORIOLIS FORCE THERE).  AKA GEO STRATIC WINDS  DUE TO LESS FRICTION & HIGH SPEED, THEY ARE VERY STRONG WINDS .  THESE WINDS ARE WESTERLIES WINDS.  ALMOST 90 DEGREE DEFLECTION DUE TO CORIOLIS FORCE
  • 10. TYPES OF WINDS  ROOSBY WAVES – MEANDERATION OF WESTERLIES TO MAINTAIN ANGULAR MUMENTAM.  JET STREAMS – AT THE MARGINS OF HEAT CELLS  4 PERMANENT- 2 POLAR JET & 2 SUBTROPICAL WETERLY JET STREAM.  TEMPORARY JET STREAM AT WESTERN INDIA FROM EQUATOR IN THE MONTHS OF JUNE – JULY – AUGUST.
  • 11. OMEGA BLOCK / TRAVELLING DEPRESSION  JET STREAMS EMBEDDED IN WESTERLIES CAUSE PRESSURE VARIABILITY THATSWHY TRAVELLING DEPRESSISON.  THE MEETING REGION OF TWO MASSES IS KNOWN AS FRONT.
  • 12. CONDITIONS OF LOW PRESSURE THERMALLY INDUCED  BECAUSE OF HIGH TEMPERATURE  EX – LOW PRESSURE AT EQUATOR  CONVENTIONAL RAINFALL AT EQUATOR. DYNAMICALLY INDUCED  UPLIFTMENT OF WARM AIR  EX – LOW PRESSURE AT SUBPOLAR LP BELT  FRONTAL RAINFALL
  • 13. DEVELOPMENT OF FRONTAL CYCLONES  WHEN AIRMASS MOVES FROM THEIR SOURCE REGION ( WARM AND COLD AIRMASS FACE EACH OTHER ), FRONT IS CREATED BETWEEN THEM CALLED STATIONARY FRONT, THEN START CIRCULAR MOVEMENT.  COLD AIR MAS PUSHES THE WARM AIRMASS , FORCED UPLIFTMENT OF AIR , CIRCULAR DUE TO CORIOLIS FORCE.
  • 14. TYPES OF CYCLONE EYE OF CLONE – HP , WALL- LP TEMPERATE CYCLONE  30 – 40 DEGREE LATITUDE  DYNAMICALY INDUCED THROUGH FRONTAL INTERACTION  WEST TO EAST MOVEMENT IN LARGE AREAS  POWERFULL ON LAND  AFFECT MAINLAND TROPICAL CYCLONE  8 – 20 DEGREE LATITUDE  THERMALLY INDUCED , AIR RISES ABOVE & CORIOLIS FORCE AFFECTS.  EAST TO WEST ( SMALL AREAS)  WEAKER ON LAND  AFFECT COASTAL AREAS  REASONS – TROPICAL WARM WATER, WARM OCEAN CURRENT
  • 15. THUNDERSTORM  THUNDERSTORMS FORMS CUMULONIMBUS CLOUDS  THUNDERING & LIGHTNING CLOUDS ACCUMULATES +VE CHARGE AT HIGH & LOW POSITIONS & - VE CHARGE INBETWEEN.  TYPES OF THUNDERSTORMS  THERMAL – LOCALISED INTENSE HEATING OF CLOUDS  OROGRAPHIC – WHEN WARM MOIST AIR PASSES OVER MOUNTAINS  COLD FRONT – FORCEFULL UPLIFTMENT OF WARM MOIST AIR
  • 16. TORNADO  INTENSE LOW PRESSURE SYSTEM  WHEN TORNADO PASSES OVER A WATERBODY , WATER IS SUCKED UP CALLED WATER FRONT.  OCCURS MOSTLY IN TEMPERATE REGIONS ( 20-60 ) DEGREE.
  • 17. POLAR VORTEX  LARGE SCALE ( 1000 KM SQ) CYCLONE AT POLES IN WINTER.  DEVELOPS AT UPPER TROPOSPHERE AND STRATOSPHERE.  DEVELPOPS DUE TO DIFFERENTIAL CREATED BTW EQUATOR AND POLES .  DEVELOPMENT OF POLAR NIGHT JET STREAMS.  ROOSBY WAVES CAN DIRUPT THEIR MOVEMENT.
  • 18.
  • 19. OZONE DEPLETION  INCREASE CHLORINE CONCENTRATION IN WINTERS , OZONE DEPLETION IN SUMEMR.  POLAR VORTEX IS WEAK IN NORTERN HEMISPHERE ( ARTIC ) DUE TO OZONE DEPLETION.  OZONE DEPLETION AT ARTIC KNOWN AS OZONE DENT.  OZONE DEPLETION AT ANTARTIC KNOWN AS OZONE HOLE .
  • 20. PRESSURE GRADIENT CELLS  VERTICAL – HADLEY CELL ( EQUATOR TO TROPIC )& FERREL( TROPIC TO POLES )  HORIZONTAL – WALKER ( FROM PERU TO AUSTRALIA ) AKA ENSO – EL NINO SOUTHERN OSCILATAION.  EL NINO – REVERSAL OF ATMOSPHERIC & OCEANIC ACTIVITIES RESULTING IN RAINFALL AND DROUGHT.  LA NINO – INTENSIFICATION OF NATURAL ACTIVITIES.
  • 21. CLIMATIC REGIONS OF THE WORLD WILL BE COVERED AFTER INDIAN GEOGRAPHY.