wind
heat
radiation
sea breeze
convection
jet stream
land breeze
conduction
greenhouse effect
Coriolis Effect
transfer of energy by the movement of particles in a gas or a liquid
thermal energy transferred from a warmer object to a cooler object
narrow belt of strong winds that blow near the top of the troposphere
movement of air from sea to land during the day
transfer of thermal energy by direct contact
causes moving air and water to curve due to earth's rotation
energy transferred by waves or rays
natural heating that occurs when certain gases in earth's atmosphere trap heat
the movement of air from an area of high pressure to an area of low pressure
movement of air from land to sea at night