Imaginaryvertical lines - are called longitudes and are used to specify the East and West directions, sometimes called ”the meridians” they are starting point of zero called the PRIME MERIDIAN
Imaginaryhorizontal lines- are called Latitudes which specify the North and South, tjis starting point of the latitude is called the Equator - located between north and south pole
Non-renewable- it exists in a fixed quantity and be depleted much faster than they are formed
Metallic mineral resource- such as iron,copper and alumiwhich can be recycled
Most abundant gas in the atmosphere is nitrogen, 78% of the atmosphere is nitrogen
Layers of atmosphere
-exosphere
-thermosphere
-mesosphere
-stratosphere
-troposphere
Troposphere- closest to the earth’s surfac, weather occurs here because It contains most of the water vapor, may have bumpy ride (turbulenc)
altitude in km= 0-20
temp in °C = 15-60
Stratosphere- many jet aircraft flies in this layer because it is very stable, This OZONE layer absorbs the suns UV rays
altitude in km-= 10-50km,
temperature is -60 to -70 degrees
Mesosphere- meteor or rock, fragments burn up in this layer
80-100 km, temperature is 1000 degrees, it is mostly nitrogen and oxygen
Thermosphere- Space shuttle fly here, is also where AURORAS are found
AURORAS reffered to as northernlights
is caused when the solar wind strike gases in the atmosphere
-UV and X-ray radiation from the sun absorbs in this layer.
Exosphere- this layer merges into space, satellites are stationed in this area
The outermost layer of the atmosphere, extending from 500 to 1,000 kilometers above the Earth.
Winds- are called the “moving air” or the air that moves horizontally
when wind is blowing- the wind vane points intk the wind
Air molecules
HOT- expand when heated,less dense
COLD- contract when the temp is cold,more dense
Since the warm air become lighter, it rises, when the warm air is rising the colder air move when warm air is rising
-this process happens continuously and creates a cyle aka AIRCONVECTION
Air convection- is a process of air circulation wherein the warm air is risng giving way to cooler air to sink and replace rising warm air
Seabreeze- during the day, as the sun heats the earths surface, the land heats ul faster than the water in the sea
Land breeze- at night, the land and sea will cool down, the land will lose heatand cool down faster than the water in the sea
Lowpressure area- the area where the warm are rises
High-pressure area- the cool air sinks since it id denser than the warm air
Monsoons- are wind systems which are visually accompanied by heavy rainfall which greatly affects our country
Monsoons are known as Hanging AMIHAN at hanging HABAGAT
-AMIHAN aka the Northeastmonsoon- is a wind system experienced by filips during colder months | December-February | this wind blows from hinger-pressure area in the asian continent to the LPA south of Ph
HABAGAT aka Southwest monsoon- is a wind system which the wind system that will move from the higher pressure area in Australia to the Lpa,
-happens in warmer months | June-Nov
The intertropical convergence zone (ITCZ)- is the place where winds in the area near the equator meet or converge.