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Insolation Practice

AB
terrestrial radiationlow-wave infrared radiation is reradiated by land
insolationthe incoming radiation from the Sun
short-wave radiationmakes up 88% of radiation received on Earth
ultraviolet, visible, near-infrared radiationexamples of short-wave radiation
heat capacityability of a substance to absorb, hold or release heat and change its temperature
reradiategive back energy into the environment
albedoreflectivity of objects in space
angle of insolationangle at which the sun'd rays strike the Earth
duration of insolationamount of time that the sun is shining in any one place
90 degreesmaximum angle of insolation
winter solsticeshortest day of the year (Dec 21st in northern hemi)
amount of insolation that is absorbed by land51%
reflectoran object that easily reflects electromagnetic waves ex. mirror, still lake
radiatoran object that gives off energy as heat
equatorplace on earth that receives most insolation year round
summer solsticelongest day of the year
spring/fall equinoxwhen day and night are equal length
conductiona way things are heated when molecules touch
convectiona way of spreading energy by the movement of molecules
radio wavea type of long-wave radiation
gamma raya type of short-wave radiation
ozone layerblocks most of deadly ultraviolet radiation


Teacher
Northview HS
CA

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