The air that surrounds us and makes up the environment we live in. It is composed of a mixture of gases, primarily nitrogen and oxygen, and is made up of layers with different temperatures, pressure, and chemicalcomposition.
Layers of the atmosphere
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Troposphere
Closest to the Earth's surface, layer in which we live, extends from the surface up to around 10-15km, characterized by temperaturesthat decrease with altitude
Stratosphere
Extends from the top of the troposphere up to around 50km, characterized by temperatures that increase with altitude due to the presence of ozone
Mesosphere
Extends from the top of the stratosphere up to around 85km, characterized by temperatures that decrease with altitude and is the coldest layer in the atmosphere
Thermosphere
Characterized by temperatures that increase with altitude due to the presence of chargedparticles that absorbenergy from the sun
Exosphere
Outermostlayer of Earth'satmosphere, provides protection from harmfulradiation
Troposphere
HotAirBalloon
Airplane
Stratosphere
Radiosonde
Mesosphere
Meteors
Meteorological Rocket
Thermosphere
AuroraLights
Exosphere
Spaceship
Satellite
Seabreeze
Happens when landheatsfaster than waterduringtheday, making the airabovewarmer.Warmairrises, drawingcoolerair from the ocean to replaceit.
Land breeze
At night, landcoolsfasterthan the sea. A low-pressurearea forms over the sea as it stayswarmer.Airflows from landtosea, creating a landbreeze.
Monsoon
Windsystem that involve biggermasses of air that move horizontally, bring abundant rainfall to the country.
Monsoon types
NortheastMonsoon (Amihan)
SouthwestMonsoon (Habagat)
Northeast Monsoon
Dry and coolwind, slight to moderaterainfall, November - March
Southwest Monsoon
Warm and moistwind, moderate to heavytorrentialrainfall, June - October
Monsoon formation
Occurs when the airmovestowardstheplace where warmair is rising (lowpressure area), away from the highpressure area
IntertropicalConvergenceZone
The place where the trade winds from the NorthernHemisphere and the SouthernHemisphere meet at, or near, the equator. Where warm and humidairmasses form, breeding zones of low-pressure areas.