Equator - passes through the center of the Earth with a latitude of 0 degrees. It divides the Earth into 2 Hemispheres, the Northern and Southern.
Prime Meridian - Perpendicular to the Equator, parallel to the axis. It has a longitude of 0 degrees and divides the world into 2 hemispheres, the Eastern and the Western.
Latitude (Parallels)- run from East to west. Starts at 0 degrees of the Equator to 90 degrees at the North and South poles.
The closer the latitude is to the Equator, the warmer the climate. The closer the latitude is to the poles, the colder the climate.
Resources - things that we can find in our environment that we use to meet our needs.
Renewable resources – those that can be replaced easily or have the potential to be replaced over time.
Nonrenewable resources – those that are in limited supply or once consumed, cannot be replaced easily
The Philippines is located at 14° 34' 59.99" N latitude and 121° 00' 0.00" E longitude.
Seasons
Divisions of the year marked by changes in weather and the amount of daylight
We have seasons because Earth's axis is tilted as it revolves around the sun
Seasons
Summer
Winter
Spring
Autumn
Summer
The hottest of the four temperate seasons
Winter
The coldest season of the year
Spring
The time when trees bloom
Autumn
Often called fall because leaves fall from the trees at this time
We have seasons because Earth's axis is tilted and the Earth revolves around the sun
There are times that the North Pole points to the Sun and there are times that it is pointing away
In June
It is summer in the Northern Hemisphere and winter in the Southern Hemisphere
In December
It is winter in the Northern Hemisphere and summer in the Southern Hemisphere
In March
It is spring in the Northern Hemisphere and autumn in the Southern Hemisphere
In September
It is spring in the Southern Hemisphere and autumn in the Northern Hemisphere.
Atmosphere
Body of Air or Gases that surround the world, protecting it and enabling life
Atmosphere
Temperature behavior is used to distinguish atmospheric layers
Composition of air: Nitrogen (78%), Oxygen (21%), Argon (0.93%), and Carbon Dioxide (0.04%)
Troposphere
Layer from 0-12km
Troposphere
Heated through energy transfer from the surface
Conventional aviation activity takes place
Only layer that can be accessed by propeller-driven aircraft
Contains 80% of the mass of the Earth's atmosphere, making it denser than all of its overlying layers
Stratosphere
Layer from 12-50km
Stratosphere
Atmospheric pressure is 1/1000 the pressure at sea level
The highest layer that can be accessed by jet-powered aircraft and weather balloons
No clouds and no forms of weather
Mesosphere
Layer from 50-80km
Mesosphere
Most meteors burn up in this layer
Lightning-induced discharges occasionally known form
Air too thin to breathe
Mainly accessed by sounding rockets and rocket-powered aircraft
Thermosphere
Layer from 80-600km
Thermosphere
Known as the upper atmosphere
The International Space Station orbits this layer
Aurora Borealis and Aurora Australis are occasionally seen
Exosphere
Layer from 600-10,000km
Exosphere
Merges into the solar wind
Composed of extremely low densities of hydrogen, helium and several heavier molecules including nitrogen, oxygen and carbon dioxide
Ozone Layer
Contained within the stratosphere
About 90% of the ozone in Earth's atmosphere is contained in the stratosphere
Ionosphere
It has practical importance because it influences radio propagation on Earth
Breeze - A light gentle wind caused by differences in air temperature.
When an area is of low pressure, the wind blows from high-pressure areas to equalize the pressure.
Sea Breeze - Occurs during the day when the land is warmer and has low pressure while the sea is cool and has high pressure.
Land Breeze - Occurs when the air over the land is cooler and has a higher pressure than the sea.