The Earth's atmosphere is mostly made of nitrogen and oxygen
Crust: 0-70km
Mantle: ~80% of the Earth's volume
Outer core: ~5000K, made of liquid iron and some nickel, the charged particles that flow in the outer core are responsible for the Earth's magnetic field
Inner core: ~5500K, high pressure prevents iron and nickel from melting
Latitude is measured north or south of the equator
Longitude is measured east or west of the Prime Meridian
The Earth's polar axis is tilted at 23.5 degrees to the 'vertical'
Spring equinox is on March 21st, Autumn equinox is on September 23rd
The Summer solstice is on 21st June, the Winter solstice is on 21st December
Our atmosphere provides us with oxygen to breathe, absorbs harmful solar UV and X-radiation, regulates the planet's temperature to a mean of 15 degrees and protects us from most meteoroid strikes
Our atmosphere affects astronomers by:
the sky being blue which limits observations to nighttime
the air in the atmosphere is continuously in turbulent motion causing the stars to appear to twinkle
Light is scattered by oxygen and nitrogen molecules in our atmosphere; most scattering occurs at the shortest (blue) wavelengths, so the sky is predominantly blue
Turbulent motion: different densities of air rise and fall on a variety of scales, causing light to refract and change direction as it passes through the different layers
Light pollution:
Skyglow is a rusty orange haze cast by lights near urban areas
Local glare from things such as streetlight that ruin our eyes night vision (dark adaptation)
The Earth is the largest terrestrial planet with a mean diameter of 13000km
The Earth is an oblate spheroid, meaning it is slightly flattened at the poles.