Second 22 cards Flashcards
GEOG
Hotter objects radiate more energy and have shorter wavelengths.
Ex-sun and earth. Sun is more hot
Relationship between radiation and temperature
Type of radiation emitted by the sun
Electromagnetic radiation
A term most often used to describe the radiant energy emitted from the sun, in the visible and near ultraviolet wavelengths.
shortwave radiation
A term most often used to describe the infrared energy emitted by the earth and the atmosphere.
longwave radiation
Average radiation total in 24 hours
Depends on:Sun angle - higher sun angle results in greater insolation
Length of day - *higher latitudes result in long summer days
Daily insolation
Average radiation total for year
Also depends on sun angle and length of day
*Latitude determines annual insolation
Annual insolation
movement of heat from equatorial and tropical regions toward the poles, occurring as latent and sensible heat transfer
Poleward heat transport
Snow and ice, light color objects
objects or surfaces reflect light leaving the temperature to be cooler.
High Albedo
Rocks and sand, darker colored objects
objects or surfaces absorb light which makes the temperature warmer.
Low Albedo
Energy from Sun-Absorbed by surface
Energy from surface-Absorbed by atmosphere
Energy from Atmosphere-Counter-radiation to surface
global energy budget
Substances that greatly impact cooling of the atmosphere
1-cloud changes range
2-aerosols
Sensible heat transferred by (for solids; ex: touching surface) transfer of thermal energy through direct contact.
Conduction
Sensible heat transferred by (for gases/liquids; ex: carried by rising air). Transfer of thermal energy through the movement of a liquid or gas.
Convection
Flattened near poles - bulging around Equator
Due to centripetal force of rotation
Why is the Earth an oblate spheroid?
Summer - North Pole directed 23.5° toward Sun
*Subsolar point 23.5° N (sun directly overhead)
*Circle of illumination touches Arctic & Antarctic circles
*June 21, beginning of summer in northern hemisphere
*Longest day of year in northern hemisphere
June solstice
Winter - North Pole directed 23.5° away from Sun
*Subsolar point 23.5° S (sun directly overhead)
*Circle of illumination touches Arctic & Antarctic circles
*December 22, beginning of winter in northern hemisphere
*Shortest day of year in northern hemisphere
December solstice
Spring (Vernal) - no tilt toward or away from Sun
*Subsolar point at Equator, passing into northern hemisphere
*Circle of illumination passes through poles
*March 21, beginning of spring in northern hemisphere
Spring Equinox
Fall (Autumnal) - no tilt toward or away from Sun
*Subsolar point at Equator, passing into southern hemisphere
*Circle of illumination passes through poles
*September 22, beginning of fall in northern hemisphere
Fall Equinox
What time of year does the equinox receive the maxi daily insolation?
June Solstice-15 hours
-massive poleward heat transport due to very cold poles
-More frequent weather systems; also larger & more intense
-Substantial change in climate throughout the world
Earths axis did not tilt?
What is the world latitude zone with the greatest seasonal variation?
Midlatitude
-Sun penetrates water deeper than land
-Heat capacity of water is greater
-Water allows mixing; land does not
-More evaporation over water versus land
Factors that make water heat and cool faster than land
*Latitude
*Surface type
*Coastal vs. Interior
*Elevation - temps decrease with altitude
*Atmospheric & oceanic circulation
Fundamental factors that influence local air temperatures
Warmer urban areas-Vegetation removed and more asphalt
Cooler rural areas- Evapotranspiration: combined water lose by plants/soils to atmosphere
Why are urban areas warmer while surrounding (rural) areas are more cool?