Geography CHAPTER 4 AIR Our Earth is surrounded

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Geography CHAPTER -4 AIR

Geography CHAPTER -4 AIR

Our Earth is surrounded by a huge blanket of air called atmosphere. All living

Our Earth is surrounded by a huge blanket of air called atmosphere. All living beings on this earth depend on the atmosphere for their survival. It provides us the air we breathe and protect us from the harmful effect of the Sun rays.

(1) TROPOSPHERE: THIS LAYER IS THE MOST IMPORTANT LAYER OF THE ATMOSPHERE. ITS AVERAGE

(1) TROPOSPHERE: THIS LAYER IS THE MOST IMPORTANT LAYER OF THE ATMOSPHERE. ITS AVERAGE HEIGHT 13. THE AIR WE BREATHE EXIST HERE. ALMOST ALL THE WEATHER PHENOMENA LIK RAINFALL, FOG AND STORM OCCUR IN THIS LAYER. (2) STRATOSPHERE : ABOVE THE TROPOSPHERE LIE THE STRATOSPHERE. IT EXTENDS UPTO A HEIGHT O 50 KM. THIS LAYER IS ALMOST FREE FROM CLOUDS AND ASSOCIATED WEATHER PHENOMENON, MAKING CONDITIONS MOST IDEAL FOR FLYING AEROPLANES CONTAINS A LAYER OF OZONE GAS.

(3) MESOSPHERE: IT LIES ABOVE THE STRATOSPHERE. IT EXTENDS UPTO THE HEIGHT OF 80

(3) MESOSPHERE: IT LIES ABOVE THE STRATOSPHERE. IT EXTENDS UPTO THE HEIGHT OF 80 KM. (4) THERMOSPHERE: IN THERMOSPHERE TEMPERATURE RISES VERY RAPIDLY WITH INCREASING HEIGHT. IT EXTENDS BETWEEN 80 TO 400 KM. THIS LAYER HELPS IN RADIO TRANSMISSION. (5) EXOSPHERE: THE UPPERMOST LAYER Of THE

WEATHER: - WEATHER IS THIS HOUR TO HOUR, DAY TO DAY CONDITION OF THE

WEATHER: - WEATHER IS THIS HOUR TO HOUR, DAY TO DAY CONDITION OF THE ATMOSPHERE. CLIMATE: - THE AVERAGE WEATHER CONDITION OF A PLACE FOR A LONGER PERIOD OF TIME REPRESENTS THE CLIMATE OF A PLACE. TEMPERATURE: - THE DEGREE OF HOTNESS AND COLDNESS OF THE AIR IS KNOWN AS TEMPERATURE. • AN IMPORTANT FACTOR THAT INFLUENCES THE

WIND: - THE MOVEMENT OF AIR FROM HIGH PRESSURE AREAS TO LOW PRESSURE AREAS

WIND: - THE MOVEMENT OF AIR FROM HIGH PRESSURE AREAS TO LOW PRESSURE AREAS IS CALLED

(1) PERMANENT WINDS: - THE TRADE WINDS, WESTERLIES AND EASTERLIES ARE THE PERMANENT WINDS.

(1) PERMANENT WINDS: - THE TRADE WINDS, WESTERLIES AND EASTERLIES ARE THE PERMANENT WINDS. THESE BLOW CONSTANTLY THROUGHOUT THE YEAR IN A PARTICULAR DIRECTION. (2) SEASONAL WINDS: - THESE WINDS CHANG THEIR DIRECTION IN DIFFERENT SEASONS. FOR EXAMPLE MONSOONS IN INDIA. (3) LOCAL WINDS: - THESE BELOW ONLY

ON THE BASIS OF MECHANISM THREE TYPES OF RAINFALL CYCLONIC RAINFALL

ON THE BASIS OF MECHANISM THREE TYPES OF RAINFALL CYCLONIC RAINFALL

RELIEF (OROGRAPHIC RAINFALL)

RELIEF (OROGRAPHIC RAINFALL)

THANK YOU

THANK YOU