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Energy in Earth Syst

Unit 10

TermDefinition
Earth systems is all of the matter , energy , and processes within Earth's boundary.
geosphere is the mostly solid, rocky part of Earth.
hydrosphere is the part of the Earth that is liquid water.
cryosphere is made up of all of the frozen water on Earth.
atmosphere is mostly made of invisible gases that surround Earth.
biosphere is made up of living things and areas of Earth.
energy budget is a way to keep track of energy transfers into and out of the Earth system.
air pressure is the measure of the force with which air molecules push on an area of a surface.
thermosphere is the uppermost layer of the atmosphere.
mesosphere is between the thermosphere and stratosphere.
stratosphere is between the mesosphere and troposphere.
troposphere is the lowest layer of the atmosphere.
ozone layer is an area in the stratosphere, 15 km to 40 km above Earth surface, where ozone is highly concentrated.
greenhouse effect is the process by which gases in the atmosphere , such as water vapor and carbon dioxide, absorb and give off infrared radiation.
temperature is a measure of the average kinetic energy of particles.
thermal energy is the total kinetic energy of particles.
thermal expansion the increase in volume that result from an increase in temperature.
heat is the energy that is transferred between objects that are at difference temperatures.
radiation is the transfer of energy as electromagnetic waves.
convection is the transfer of energy due to the movement of matter.
conduction is the transfer of energy from one object to another object through direct conitact.
wind the movement of air caused by difference in air pressure .
Coriolis effect the apparent curving of the path of a moving object from an otherwise straight path due to Earth's rotation .
global wind these wind systems occur at or near Earth's surface.
jet streams are narrow belts of high speed winds that blow from west to eat, between 7 km and 16 km above Earth's surface.
local wind are movements of air over short distances.
ocean current the oceans contain stemlike movements of water.
surface current ocean currents that occur at or near the surface of the ocean caused by wind.
deep current movements of ocean water far below the surface .
convection current is a movement of water that result from density differences.
upwelling the warm surface is then replaced by cold nutrient rich water from the deep ocean in a process.
Created by: Rhiley Dunston
 

 



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