Different periods of the year that are distinguished by special weather and climate conditions
Seasons
Spring
Summer
Autumn
Winter
Seasons
Different amount of light received from the sun
Different temperatures
Different weather conditions that repeat
Axis
An imaginary line passing through the center of the earth that goes through both the north pole and the south pole
Rotation
The spinning motion of earth around its axis
Revolution
The movement of the earth around the sun
It takes 24 hours or one day for the earth to completely rotate around on its axis
It takes 365 and 1/4 days or one year for the earth to move around the sun
Tilt of the earth's axis
Tilted at an angle of 23.5 degrees
Reason behind the occurrence of seasons
Solstice
When the axis of the earth points forward or away from the sun
The first day of summer is marked by the summer solstice which occurred during June 21 or June 22
The first day of winter is marked by the winter solstice which occurred during December 21 or 22
When the north pole is tilted toward the sun in June
The northern hemisphere receives more direct rays from the sun and experiences longer daytime than nighttime
When the south pole is tilted toward the sun in December
The southern hemisphere receives more direct rays from the sun and experiences summer
Equinox
When the axis of the earth does not point either toward or away from the sun, resulting in equal day and night
The first day of spring is marked by the vernal equinox which happens on March 21 or 22
The first day of the autumn season is marked by the autumnal equinox which happens on September 21 or 22
Wet and dry seasons
The two main seasons experienced in the Philippines due to its location near the equator
The rainy season in the Philippines is from June to November, and the dry season is from December to May
The dry season in the Philippines can be subdivided into cold dry season and hot dry season
Seasonal change is caused by the tilt of the earth's axis, the revolution of the earth around the sun, the direct rays of the sun, and the length of daytime
There are a number of unique combinations of atmospheric phenomena experienced by people in all parts of the world
Common atmospheric phenomena
Breezes
Monsoons
Intertropical Convergence Zone
How air behaves when heated
1. Air molecules move faster and spread out
2. Makes the air less dense or light
3. Warm air rises
Warm air rises
Surrounding air moves toward it to replace the rising warm air
Wind
Air that is moving horizontally
Land surface heats up faster than bodies of water during the day, but loses heat faster at night
Breezes
Localized winds near bodies of water
Experienced by those living in coastal areas
Sea breeze
1. Land warms up faster than bodies of water during the day
2. Warm air on land rises
3. Cooler air above the sea moves toward the land and replaces the warm air
Land breeze
1. Land cools faster than the sea at night
2. Warm air over the sea rises
3. Cooler air from the land moves toward the sea
Monsoons
Wind systems that involve bigger masses of air moving horizontally
Bring abundant rainfall
Types of monsoons
East monsoon
Southwest monsoon
How monsoons occur
1. Air moves toward the place where warm air is rising (low pressure area)
2. Air sinks in the high pressure area
3. Wind moves from high pressure to low pressure area
Northeast monsoon
High pressure in China and Siberia, low pressure in South Indian Ocean/Australia
Brings dry, cold wind
Southwest monsoon
High pressure in South Indian Ocean/Australia, low pressure in China and Siberia
Brings warm, moist wind
Intertropical Convergence Zone (ITCZ)
Place where trade winds from Northern and Southern hemispheres meet at the equator
Warm, humid air masses form, resulting in heavy precipitation and thunderstorms
Breeding zone of low pressure areas
There are a number of unique combinations of atmospheric phenomena experienced by people in all parts of the world
Common atmospheric phenomena
Breezes
Monsoons
Intertropical Convergence Zone
How air behaves when heated
1. Air molecules move faster and spread out
2. Makes the air less dense or light
3. Warm air rises
Warm air rises
Surrounding air moves toward it to replace the rising warm air