FACTORS AFFECTING
CLIMATE

K.SUGUNA.R
PGT GEO
FACTORS
1.
2.
3.
4.
5.
6.

LATITUDE
ALTITUDE
DISTANCE FROM THE SEA
PRESSUR AND WIND SYSTEM
RELIEF
OCEAN CURRENTS
LATITUDE
• DUE TO THE CURVATURE OF HE EARTH THE AMOUNT OF SOLAR
ENERGY RECEIVED VARIES ACCORDING TO LATITUDE
• TEMPERATURE DECREASES FROM EQUATOR TO POLAR REGION
• TROPICAL REGION-HOT
• POLAR REGION –COLD
• TEMPERATE REGION –MODERATE
LATITUDE
TROPIC OF CANCER PASSES THROUGH THE CENTRE OF INDIA
SOUTH INDIA EXPERIENCES TROPICAL CLIMATE
NORTH INDIA EXPERIENCES TEMPERATE CLIMATE
GREEN LAND –POLAR CLIMATE
ALTITUDE
• AS WE GO FROM SURFACE OF THE EARTH TO HIGHER
ELEVATIONS ATMOSPHERIC TEMPERATURE DECREASES.
• NORMAL LAPSE RATE -1O C /165m HEIGHT
• ATMOSPHERE GET HEATED FROM BELOW
ALTITUDE
• HILLY AREAS ARE COOLER THAN PLAIN AREAS
• OOTY IS COOLER THAN COIM BATORE
• BANGALORE IS COOLER THAN CHENNAI
DISTANCE FROM
THE SEA
• SEA EXERTS A MODERATING INFLUENCE ON CLIMATE
• IF THE PLACE IS LOCATED AWAY FROM THE SEA THEN THE
MODERATING INFLUENCE OF THE SEA DECREASES
DISTANCE FROM THE SEA
• PLACES IN THE INTERIOR LOCATION
EXPERIENCES EXTREME CLIMATE
• COASTAL AREAS EXPERIENCES EQUABLE
CLIMATE
RELIEF
•

•
•
•

HEIGHT AND ASPECT OF THE RELIEF INFLUENCES THE
CLIMATE OF A REGION
MOUNTAINS ACT AS A CLIMATIC BARRIER
IT PREVENTS THE COLD/HOT WIND AND PROTECT THE
REGION
HIMALAYAS ACTS AS A CLIMATIC BARRIER
RELIEF
•

•
•
•

IF THE MOSTURE LADEN WINDS BLOW PERPENDICULAR TO A
MOUNTAINIT CAUSES OROGRAPHIC RAINFALL
WINDWARD SIDE RECEIVES MORE RAINFALL WHERE AS LEEWARD
SIDE REMAINS AS A RAINSHADOW REGION
WESTERN GHATS CAUSES OROGRAPHIC RAINFALL
PRESSURE AND
WIND SYSTEM
•
•
•
•
•

AIR PRESSURE AFFECTS THE WIND SYSTEM
WIND AFFECTS THE RAINFALL OF A REGION
HUMID AIR GIVES RAINFALL
WIND FROM CONTINENT –DRY
WIND FROM OCEANS- WET
OCEAN CURRENTS•MASS MOVEMENTS OF OCEAN WATER FROM ONE PART
OF THE OCEAN TO ANOTHER PART.
•TWO TYPES:
•WARM CURRENT
•COLD CURRENT
OCEAN CURRENTSWARM CURRENT INCREASES THE TEMPERATURE
COLD CURRENT –DECREASES THE TEMPERATURE
GULF STREAM INCREASES THE TEMPERATURE OF THE
WESTERN COAST OF EUROPE

Factors affecting climate

  • 1.
  • 2.
    FACTORS 1. 2. 3. 4. 5. 6. LATITUDE ALTITUDE DISTANCE FROM THESEA PRESSUR AND WIND SYSTEM RELIEF OCEAN CURRENTS
  • 3.
    LATITUDE • DUE TOTHE CURVATURE OF HE EARTH THE AMOUNT OF SOLAR ENERGY RECEIVED VARIES ACCORDING TO LATITUDE • TEMPERATURE DECREASES FROM EQUATOR TO POLAR REGION • TROPICAL REGION-HOT • POLAR REGION –COLD • TEMPERATE REGION –MODERATE
  • 4.
    LATITUDE TROPIC OF CANCERPASSES THROUGH THE CENTRE OF INDIA SOUTH INDIA EXPERIENCES TROPICAL CLIMATE NORTH INDIA EXPERIENCES TEMPERATE CLIMATE GREEN LAND –POLAR CLIMATE
  • 5.
    ALTITUDE • AS WEGO FROM SURFACE OF THE EARTH TO HIGHER ELEVATIONS ATMOSPHERIC TEMPERATURE DECREASES. • NORMAL LAPSE RATE -1O C /165m HEIGHT • ATMOSPHERE GET HEATED FROM BELOW
  • 6.
    ALTITUDE • HILLY AREASARE COOLER THAN PLAIN AREAS • OOTY IS COOLER THAN COIM BATORE • BANGALORE IS COOLER THAN CHENNAI
  • 7.
    DISTANCE FROM THE SEA •SEA EXERTS A MODERATING INFLUENCE ON CLIMATE • IF THE PLACE IS LOCATED AWAY FROM THE SEA THEN THE MODERATING INFLUENCE OF THE SEA DECREASES
  • 8.
    DISTANCE FROM THESEA • PLACES IN THE INTERIOR LOCATION EXPERIENCES EXTREME CLIMATE • COASTAL AREAS EXPERIENCES EQUABLE CLIMATE
  • 9.
    RELIEF • • • • HEIGHT AND ASPECTOF THE RELIEF INFLUENCES THE CLIMATE OF A REGION MOUNTAINS ACT AS A CLIMATIC BARRIER IT PREVENTS THE COLD/HOT WIND AND PROTECT THE REGION HIMALAYAS ACTS AS A CLIMATIC BARRIER
  • 10.
    RELIEF • • • • IF THE MOSTURELADEN WINDS BLOW PERPENDICULAR TO A MOUNTAINIT CAUSES OROGRAPHIC RAINFALL WINDWARD SIDE RECEIVES MORE RAINFALL WHERE AS LEEWARD SIDE REMAINS AS A RAINSHADOW REGION WESTERN GHATS CAUSES OROGRAPHIC RAINFALL
  • 11.
    PRESSURE AND WIND SYSTEM • • • • • AIRPRESSURE AFFECTS THE WIND SYSTEM WIND AFFECTS THE RAINFALL OF A REGION HUMID AIR GIVES RAINFALL WIND FROM CONTINENT –DRY WIND FROM OCEANS- WET
  • 12.
    OCEAN CURRENTS•MASS MOVEMENTSOF OCEAN WATER FROM ONE PART OF THE OCEAN TO ANOTHER PART. •TWO TYPES: •WARM CURRENT •COLD CURRENT
  • 13.
    OCEAN CURRENTSWARM CURRENTINCREASES THE TEMPERATURE COLD CURRENT –DECREASES THE TEMPERATURE GULF STREAM INCREASES THE TEMPERATURE OF THE WESTERN COAST OF EUROPE