ATMOSPHERE IS MADE UP OF NITROGEN(78%) AND OXYGEN(21%) IN MAJOR.
OTHER GASES THAT INCLUDE IS THE HELIUM.HYDROGEN,ARGON,OZONE,CARBON DI OXIDE.
ARGON IS THE THIRD MAJOR GASES THAT IS FOUND IN THE ATMOSPHERE.
CARBON DI OXIDE IS THE GREEN HOUSE GASES.
STRUCTURE OF ATMOSPHERE::::
THERE ARE FIVE LAYER OF ATMOSPHERE WHICH ARE
1)TROPOSPHERE
2)STRATOS[HERE
3)MESOSPHERE
4)THERMOSPHERE
5)EXOSPHERE
TROPOSPHERE::::AVERAGE HEIGHT IS 13 KM
ALL THE AIR WE BREATHE,EXIST HERE.
AND ALL THE NATURAL PHENOMENON THAT OCCUR IS FROM HERE.
LIKE RAINFALL,HAILSTORM,
STRATOSPHERE::::THIS LAYER GOES TILL 50 KM.
THIS LAYER IS FREE FROM CLOUDS AND ITS RELATED ACTIVITY.
THIS LAYER IS MOST IDEAL FOR FLYING AIRPLANES.
THIS LAYER ALSO CONTAINS OZONE LAYER.
MESOSPHRE::::THIS LAYER IS THE THIRD LAYER OF THE ATMOSPHERE AND IT EXTENDS TILL THE 80 KM.
THIS LAYER IS THE LAYER WHERE METEROITES ENTER IN THE ATMOSPHERE FROM SPACE AND ARE BURNT HERE.
THERMOSPHERE:::::THIS IS THE FOUTH LAYER OF THE ATMOSPHERE AND IT EXTENDS FROM 80-400 KM.
THIS IS THE VERY HOT LAYER .
THIS LAYER IS USED FOR RADIO TRANSMISSION.
THIS IS THE LAYER FROM WHERE THE RADIO WAVES ARE REFLECTED BACK TO THE EARTH WHICH WERE SENT FROM THE EARTH.
EXOSPHERE::::THIS IS THE TOP MOST LAYER OF ATMOSPHERE.
TEMPERATURE:::::
TEMPERATURE OF A PLACE IS DETERMINED BY INSOLATION.
INSOLATION IS THE AMOUNT OF HEAT THAT IS INTERCEPTED IN EARTH BY SUN.
THE INSOLATION IS HIGHEST AT THE EQUATOR AND IT DECREASES AS WE GO TOWARD THE POLE.
THE TEMPERATURE IS MEASURED IN CELCIUS AND IT WAS INVENTED BY ANDER CELCIUS.
AIR PRESSURE::::
THE PRESSURE EXCERTED BY THE WEIGHT OF THE AIR IS CALLED AS AIR PRESSURE.
THE AIR PRESSURE DECREASES WITH HEIGHT AND HENCE MAXIMUM AIR PRESSURE IS ON THE SEA LEVEL AND IT DECREASES RAPIDLY.
HORIZONTALLY,AIR PRESSURE IS DEPENDENT ON TEMPERATURE
HORIZONTALLY,ON THE PLACES WHERE THERE IS HIGH TEMPERATURE,THE AIR PRESSURE IS LOW AND WHERE THERE IS COLD,THE AIR PRESSURE IS VERY HIGH.
WINDS::::
WINDS BLOW FROM HIGH PRESSURE TO LOW PRESSURE.
THERE ARE VARIOUS TYPES OF WINDS::::
1)PERMANENT WINDS::::THESE ARE THE WINDS THAT BLOWS PERMANENTLY THROUGHOUT THE YEAR AND BLOW IN A PARTICULAR DIRECTION.
FOR EXAMPLE::::TRADE WINDS,EASTERLIES,WESTERLIES.
2)SEASONAL WINDS::::THESE WIND BLOW IN THE PARTICULAR SEASON AND ARE DEPENDENT ON THE SEASONS.
THE EXAMPLE OF THE SEASONAL WINDS ARE MONSOONS.
LOCAL WINDS::::THESE WIND BLOW FOR SMALL PERIOD OF THE YEAR AND THEY BLOW IN A PARTICULAR REGIONS.
THE EXAMPLE ARE LOO.
MOISTURE:::::WHEN THE WATER EVAPORATES FROM THE WATER BODIES,IT BECOME WATER VAPOUR.
WHEN THEY MIX UP WITH THE AIR,IT IS CALLED MOISTURE. OR HUMIDITY.
WHEN THE AIR IS FULL OF WATER VAPOUR,WE CALL IT A HUMID DAY.
WHEN THE WATER VAPOUR RISES,IT START COOLING.
THE VAPOUR CONDENSES AND FORM AN DROPLET.WHEN THE DROPLET IS VERY HIGH IN BULK SIZE,IT IS CALLED AS CLOUD.
WHEN THESE WATER DROPLET IS TOO HEAVY,IT PRECIPITATES AND WATER COMES DOWN TO THE EARTH IN FORM OF RAINFALL.
OTHER GASES THAT INCLUDE IS THE HELIUM.HYDROGEN,ARGON,OZONE,CARBON DI OXIDE.
ARGON IS THE THIRD MAJOR GASES THAT IS FOUND IN THE ATMOSPHERE.
CARBON DI OXIDE IS THE GREEN HOUSE GASES.
STRUCTURE OF ATMOSPHERE::::
THERE ARE FIVE LAYER OF ATMOSPHERE WHICH ARE
1)TROPOSPHERE
2)STRATOS[HERE
3)MESOSPHERE
4)THERMOSPHERE
5)EXOSPHERE
TROPOSPHERE::::AVERAGE HEIGHT IS 13 KM
ALL THE AIR WE BREATHE,EXIST HERE.
AND ALL THE NATURAL PHENOMENON THAT OCCUR IS FROM HERE.
LIKE RAINFALL,HAILSTORM,
STRATOSPHERE::::THIS LAYER GOES TILL 50 KM.
THIS LAYER IS FREE FROM CLOUDS AND ITS RELATED ACTIVITY.
THIS LAYER IS MOST IDEAL FOR FLYING AIRPLANES.
THIS LAYER ALSO CONTAINS OZONE LAYER.
MESOSPHRE::::THIS LAYER IS THE THIRD LAYER OF THE ATMOSPHERE AND IT EXTENDS TILL THE 80 KM.
THIS LAYER IS THE LAYER WHERE METEROITES ENTER IN THE ATMOSPHERE FROM SPACE AND ARE BURNT HERE.
THERMOSPHERE:::::THIS IS THE FOUTH LAYER OF THE ATMOSPHERE AND IT EXTENDS FROM 80-400 KM.
THIS IS THE VERY HOT LAYER .
THIS LAYER IS USED FOR RADIO TRANSMISSION.
THIS IS THE LAYER FROM WHERE THE RADIO WAVES ARE REFLECTED BACK TO THE EARTH WHICH WERE SENT FROM THE EARTH.
EXOSPHERE::::THIS IS THE TOP MOST LAYER OF ATMOSPHERE.
TEMPERATURE:::::
TEMPERATURE OF A PLACE IS DETERMINED BY INSOLATION.
INSOLATION IS THE AMOUNT OF HEAT THAT IS INTERCEPTED IN EARTH BY SUN.
THE INSOLATION IS HIGHEST AT THE EQUATOR AND IT DECREASES AS WE GO TOWARD THE POLE.
THE TEMPERATURE IS MEASURED IN CELCIUS AND IT WAS INVENTED BY ANDER CELCIUS.
AIR PRESSURE::::
THE PRESSURE EXCERTED BY THE WEIGHT OF THE AIR IS CALLED AS AIR PRESSURE.
THE AIR PRESSURE DECREASES WITH HEIGHT AND HENCE MAXIMUM AIR PRESSURE IS ON THE SEA LEVEL AND IT DECREASES RAPIDLY.
HORIZONTALLY,AIR PRESSURE IS DEPENDENT ON TEMPERATURE
HORIZONTALLY,ON THE PLACES WHERE THERE IS HIGH TEMPERATURE,THE AIR PRESSURE IS LOW AND WHERE THERE IS COLD,THE AIR PRESSURE IS VERY HIGH.
WINDS::::
WINDS BLOW FROM HIGH PRESSURE TO LOW PRESSURE.
THERE ARE VARIOUS TYPES OF WINDS::::
1)PERMANENT WINDS::::THESE ARE THE WINDS THAT BLOWS PERMANENTLY THROUGHOUT THE YEAR AND BLOW IN A PARTICULAR DIRECTION.
FOR EXAMPLE::::TRADE WINDS,EASTERLIES,WESTERLIES.
2)SEASONAL WINDS::::THESE WIND BLOW IN THE PARTICULAR SEASON AND ARE DEPENDENT ON THE SEASONS.
THE EXAMPLE OF THE SEASONAL WINDS ARE MONSOONS.
LOCAL WINDS::::THESE WIND BLOW FOR SMALL PERIOD OF THE YEAR AND THEY BLOW IN A PARTICULAR REGIONS.
THE EXAMPLE ARE LOO.
MOISTURE:::::WHEN THE WATER EVAPORATES FROM THE WATER BODIES,IT BECOME WATER VAPOUR.
WHEN THEY MIX UP WITH THE AIR,IT IS CALLED MOISTURE. OR HUMIDITY.
WHEN THE AIR IS FULL OF WATER VAPOUR,WE CALL IT A HUMID DAY.
WHEN THE WATER VAPOUR RISES,IT START COOLING.
THE VAPOUR CONDENSES AND FORM AN DROPLET.WHEN THE DROPLET IS VERY HIGH IN BULK SIZE,IT IS CALLED AS CLOUD.
WHEN THESE WATER DROPLET IS TOO HEAVY,IT PRECIPITATES AND WATER COMES DOWN TO THE EARTH IN FORM OF RAINFALL.
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