Section 2.2 - Thermal Energy Transfer In The Atmosphere Flashcards
Thermal energy transfers in 3 ways:
Radiation, conduction, convection
______:
- the emission of energy as particles or ______
- this energy, when absorbed by an object, will increase the kinetic energy and therefore temperature of the particles that make up the object
Radiation
Waves
______:
- every atom is physically bonded to its neighbours
- if heat energy is supplied to one part of a solid, the atoms vibrate faster
- as they vibrate more, the bonds between atoms are shaken more
- this passes vibrations on to the next atom, and so on
- heat transferred through direct ______ of atoms
Conduction
Collision
______:
- the transfer of thermal energy through the ______ of particles from one ______ to another
- as the particles absorb ______, they move apart, decreasing the density
- the lower density air/water will move up, and the higher density air/water will fall down
Convection
Movement
Location
Energy
______ ______ is the pressure exerted by the air above any point on the Earth’s surface
Atmospheric pressure
Colder air exerts ______ ______ than warm air, since colder air is more dense
More pressure
This difference in air pressure and temperature between cold and hot air creates ______ ______ in the atmosphere
Convection currents
______ is the movement of air from regions of ______ pressure to regions of ______ pressure
Wind
High
Low
The ______ ______ if the bending of moving currents in response to Earth’s rotation
Coriolis effect
The ______ ______ causes winds in two hemispheres to move in opposite directions
Coriolis effect
______ and the ______ cause the global wind patterns
Convection currents
Coriolis effect
A ______ ______ is a narrow fast- flowing “river” of air in the stratosphere. These strong winds (480-640km/h) are typically thousands of kilometres long and hundreds of kilometres wide.
Jet stream
Changes in the jet stream are important in predicting ______ weather
Severe