Second 22 cards Flashcards

GEOG

1
Q

Hotter objects radiate more energy and have shorter wavelengths.
Ex-sun and earth. Sun is more hot

A

Relationship between radiation and temperature

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2
Q

Type of radiation emitted by the sun

A

Electromagnetic radiation

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3
Q

A term most often used to describe the radiant energy emitted from the sun, in the visible and near ultraviolet wavelengths.

A

shortwave radiation

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4
Q

A term most often used to describe the infrared energy emitted by the earth and the atmosphere.

A

longwave radiation

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5
Q

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

A

Daily insolation

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6
Q

Average radiation total for year
Also depends on sun angle and length of day
*Latitude determines annual insolation

A

Annual insolation

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7
Q

movement of heat from equatorial and tropical regions toward the poles, occurring as latent and sensible heat transfer

A

Poleward heat transport

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8
Q

Snow and ice, light color objects
objects or surfaces reflect light leaving the temperature to be cooler.

A

High Albedo

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9
Q

Rocks and sand, darker colored objects
objects or surfaces absorb light which makes the temperature warmer.

A

Low Albedo

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10
Q

Energy from Sun-Absorbed by surface
Energy from surface-Absorbed by atmosphere
Energy from Atmosphere-Counter-radiation to surface

A

global energy budget

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11
Q

Substances that greatly impact cooling of the atmosphere

A

1-cloud changes range
2-aerosols

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12
Q

Sensible heat transferred by (for solids; ex: touching surface) transfer of thermal energy through direct contact.

A

Conduction

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13
Q

Sensible heat transferred by (for gases/liquids; ex: carried by rising air). Transfer of thermal energy through the movement of a liquid or gas.

A

Convection

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14
Q

Flattened near poles - bulging around Equator
Due to centripetal force of rotation

A

Why is the Earth an oblate spheroid?

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15
Q

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

A

June solstice

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16
Q

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

A

December solstice

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17
Q

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

A

Spring Equinox

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18
Q

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

A

Fall Equinox

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19
Q

What time of year does the equinox receive the maxi daily insolation?

A

June Solstice-15 hours

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20
Q

-massive poleward heat transport due to very cold poles
-More frequent weather systems; also larger & more intense
-Substantial change in climate throughout the world

A

Earths axis did not tilt?

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21
Q

What is the world latitude zone with the greatest seasonal variation?

A

Midlatitude

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22
Q

-Sun penetrates water deeper than land
-Heat capacity of water is greater
-Water allows mixing; land does not
-More evaporation over water versus land

A

Factors that make water heat and cool faster than land

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23
Q

*Latitude
*Surface type
*Coastal vs. Interior
*Elevation - temps decrease with altitude
*Atmospheric & oceanic circulation

A

Fundamental factors that influence local air temperatures

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24
Q

Warmer urban areas-Vegetation removed and more asphalt
Cooler rural areas- Evapotranspiration: combined water lose by plants/soils to atmosphere

A

Why are urban areas warmer while surrounding (rural) areas are more cool?

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25
Time of day when temperature is highest and lowest
Highest temp- mid afternoon (3pm ish) Lowest temp- immediately before or after sunrise
26
Greatest temp ranges in Siberia & NW N. America -Continental locations Smallest temp ranges in Equatorial oceans - Maritime influence
Regions with the greatest and smallest annual temp range in the world
27
Feel of temperature - based on: Actual temperature & windspeed -Higher windspeed creates colder wind-chill -Body emitting heat/perspiration creates "feel"
wind chill index
28
Feel of temperature on hot days -based on: Actual temperature & relative humidity -Higher relative humidity creates hotter conditions -Body emitting heat/inability to perspire creates "feel"
heat index
28
evaporation, melting, sublimation
latent heat absorbed
29
freezing, condensation, deposition
latent heat released
30
Where is most of Earth's freshwater found?
glaciers and ice caps
31
The cycle through which water in the hydrosphere moves; includes such processes as evaporation, precipitation, and surface and groundwater runoff -Evaporated from oceans: 430 cu km -Evaporated from land: 70 cu km
hydrologic cycle
32
Temperature at which air, when cooled, becomes saturated Provides measure of actual moisture in air
dew point temperature
33
Relative Humidity (RH) = 100 X (Specific Humidity / Saturation Specific Humidity) -RH is the actual amount of moisture / total amount of moisture the air can hold Adjustments to specific humidity and/or temperature can change relative humidity
Relationship between specific humidity and temperature
34
A process in which no heat is transferred to or from the system by its surroundings.
adiabatic process
35
Made up of water droplets or ice particles -Cloud particles form around Condensation Nuclei -Condensation nuclei include: *Tiny salt crystals *Dust *Other aerosols
How are clouds formed?
36
blanket-like, cover most of sky -Stratus - low, cover entire sky - can be thick -Altostratus - higher stratus clouds -Cirrostratus - very high stratus clouds, often thin
Types of clouds-Stratiform
37
vertically developed -Cumulus - globular cloud mass from rising air parcel -Altocumulus - mid-level, rounded clouds -Cirrocumulus - high-level rolls or ripples of clouds
Types of clouds- Cumuliform
38
Types of clouds- Nimbus
produce rainfall
39
thunderstorm clouds -Formed via thousands of rising air parcels
Types of clouds- Cumulonimbus
40
steady rain or snow
Types of clouds- Nimbostratus
41
high, thin, wispy clouds
Types of clouds- Cirrus
42
forms at night when air temp falls below dew point -Forms in valleys, esp. in winter where cooling is rapid
Radiation fog
43
forms when warm, moist air passes over cold surface -Happens in ocean where warm & cold currents pass -Famous San Francisco fog is what fog
Advection fog
44
1. in warm clouds -water droplets condense -Droplets collide and coalesce into larger droplets -At some point, gravity takes over and droplet falls to surface as rain 2. In cold clouds - ice crystals form & grow - May form by deposition or by freezing of super-cooled water -Ice may (or may not) melt on way down to Earth's surface
Two ways precipitation can form
45
Precipitation caused by winds blowing warm, moist air toward coastal mountains; results when warm air rises over the mountains and cools enough to form clouds that release rain and snow.
orographic precipitation
46
precipitation that is induced when warm, moist air is heated at the ground surface, rises, cools, and condenses to form water droplets, raindrops, and eventually rainfall
convective precipitation
47
rain snow sleet -rain falling through freezing air hail
Types of precipitation
48
The state of atmosphere at particular place & time -can change in minutes, but usually over a day or two
Weather
49
Is the average conditions of atmosphere in a region
Climate
50
51
eye model of Earth's surface. -Shows how phenomena are organized -3-D object represented on 2-D surface
Map-Birds
52
simplified (or idealized) version of reality
Model
53
change in temperature as one rises in atmosphere -(°C/1000m)
Lapse Rate
54
The boundary between the troposphere and the stratosphere.
Tropopause
55
60 - 400km in altitude -Contains electrically charged atoms & molecules -These particles called ions -Ions created by solar radiation -Creates global electrical and magnetic fields
Ionosphere
56
cannot be felt or measured Stored as molecular motion when water changes phase
Latent heat
57
can be felt & measured Transferred by conduction (for solids; ex: touching surface) Transferred by convection
Sensible heat
58
Difference between incoming and outgoing radiation
Net radiation
59
-Ice/snow reflect sunlight - Cool Earth (high albedo) -Dark material (rock/sand) absorb sunlight - Warm Earth (low albedo)
Albedo
60
The amount of water vapor in the air
Humidity
61
when air can hold no more H2O
Saturation
62
active during the day
Diurnal