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Weather
The condition of the atmosphere at a specific time and place
short term energy interactions
Climate
Long term average of weather
Meteorology
Study of weather
focus on physics of the atmosphere and short term weather forecasting
Climatology
Study of long term weather (climate)
focus on average regional conditions and predict long range changes
4 Spheres of Earth System
Atmosphere - Air
Lithosphere - Land
Hydrosphere - Water
Biosphere - Life
Geography
Description, or exploration, of Earth using a spatial perspective
Subfields of Geography
Physical, Human, Geotechnology
Geographic Grid
Latitude and Logitude
Latitude
Parallels based on angular measurements from the equator
horizontal
range from 0 degrees to 90 degrees N/S
Longitude
Based on angular measurements east/west of the prime meridian
vertical
0 degrees - 180 degrees E/W
Expanding Universe Theory
Describes how, since the Big Bang Theory, space is stretching causing galaxies to move further apart
Formation of Stars and Galaxies
As expanding universe cools, dark matter and interstellar gases accumulate into oddly shaped masses (nebula)
Evolution of Earth’s atmosphere
1) Primordial Altmosphere: Nebula of Hydrogen, Helium, Methane, and Ammonia - Photodissociation
2) Secondary Primitive Atmosphere: Earth cooling and degassing- 85% water vapor, 10% Carbon Dioxide, 1-2% Nitrogen
3) Heavy Precipitation Period: Water vapor turns liquid causing ocean formation. Carbon Dioxide dwindles and Nitrogen increases
4) Oxygen Period: Water molecules split and the ozone forms. Photosynthesis begins.
Fusion
Extreme heat and pressure combines light atomic nuclei (Hydrogen) into heavier ones (Helium) and releases an immense amount of energy
powers the Sun
Environmental Role of Earth’s Atmosphere
Provides essential gases: Oxygen and Carbon Dixoide
Traps heat through greenhouse gases
Ozone layer sheilds radiation
Regulates temperature
Enables water cycle
Terrestial Planets
Small, dense and made primarily of rocky and metallic material
Mercury: very little atmosphere; closely resembles the Earth’s moon
Venus: Earth’s sister planet; cloud-shrouded atmosphere; rotates opposite direction from Earth; dense, toxic atmosphere
Mars: leading candidate for past or present life-support system; surface features carved by water; evidence of water and strong winded atmosphere
Jovian Planets
Large, thick, low density, primarily gas giants
Neptune
Uranus
Jupiter
Composition of Earth’s Atmosphere
Mixture of solids (dust and ice), liquids (water), and gases
Non-variable gases: Nitrogen (78%), Oxygen (21%), Argon (0.93%)
Variable gases: Carbon Dioxide (0.036%), Water Vapor (0-4%), Ozone (varies)
Vertical Zonation
Thermal layers of the Earth’s atmosphere
Layers of Earth’s atmosphere
Trophosphere, Stratosphere, Mesosphere, and Thermosphere
Trophosphere
closest to Earth’s surface
thinnest layer
contains 80% of the total mass of the atmosphere
air is vertically and horizontally mixed
weather
Stratosphere
ozone layer
absorbs UV radiation from the sun
very little mixing of air
temperature increases with altitude
Mesosphere
temperature decreases to lowest levels in atmosphere
negative lapse rate
Thermosphere
furthest from Earth’s surface
temperature increases with altitude due to ultraviolet radiation (EUV) from the sun
thin air comtaining little heat energy
ionization occurs (electrons become ionized casuing auroras
Environmental Lapse Rate
Decrease in temperature as the altitude increases
occurs in the trophosphere and mesosphere
Greenhouse Effect
Atmospheric gases trap heat from the sun that warms the Earth
Temperature Inversion
Layer of warm air gets trapped above a layer of cool air
prevents vertical air mixing
Equinox
Sun is pointed at the equator
Experiences 12 hour light and 12 hour dark
September 21/22
March 20/21
Solstice
Sun rays are pointed on teh Tropic of Cancer: Summer solstice
June 21/22
Sun rays are pointed on the Tropic of Capricorn: Winter solstice
December 21/22
Solar Declination
The angular distance of the sun north or south of the equator varying throughout the year due to the Earth’s axial tilt
Temperature
Measure of the average kinetic energy in a substance
Heat Conduction
the transfer of thermal energy between substances in direct contact
Heat Convection
Heat transfer occurs in liquids and gases when there is physical movement carrying thermal energy from one location to another
Wind Chill
Temperature measure accounting for effect of wind speed on rate of heat loss from the body
Heat Index
Measure incorperating both surface temperature and relative humidity
Sun Spots
Areas of intense magnetic activity on solar photosphere
Calculating Sun Angle
1) Find latitudinal distance between observer and vertical rays of sun
2) Subtract value from 90 degrees