Weather and climate Flashcards

1
Q

physical condition of the atmosphere (particularly the troposhere) at a specific time and place with regard to wind, temperature, cloud cover, fog and precipitation

A

Weather

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2
Q

collective word for rain, hail, snow, etc.

A

precipitation

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3
Q

longer term view of the weather patterns of a particular locality

A

Climate

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4
Q

The energy that drives processes in the atmosphere

A

Solar energy

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5
Q

fraction of the incident radiation that is reflected

A

Reflectivity

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6
Q

fraction of the incident radiation that is absorbed

A

Absorptivity

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7
Q

fraction of the incident radiation that is transmitted

A

Transmissivity

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8
Q

A body that absorbs all electromagnetic radiation that falls on

A

black body

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9
Q

“perfect absorber”

A

idealization

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10
Q

a perfect radiator (emitter), i.e., the relative intensities of the different frequencies that it radiates are dependent only on its temperature

A

black body

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11
Q

the ratio of the amount of radiative
power emitted by a non-black body to that of a blackbody at the same temperature.

A

Emissivity

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12
Q

distribution of the emitted spectrum

A

Solar spectrum

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13
Q

considered to behave as a black body having a surface temperature of ca. 6000 K.

A

Sun

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14
Q

not smooth unlike that of a black body of the same temperature. There are deep throughs.

A

Terrestrial spectrum

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15
Q

portion of the incoming radiation that is reflected and scattered back to space. A function of the angle of incidence

A

Albedo

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16
Q

*associated with temperature change, without phase change
*associated with a phase change

A
  • sensible heat
    *Latent heat
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17
Q

The water of the oceans is in perpetual state of circulatory motion driven by

A

convection

18
Q

*water sinks because of its relatively high density (due to low temperature and high salinity)
* water is warmed by the sun > becomes warmer > rises to the surface

A
  • North Atlantic
  • Indian and Pacific Ocean
19
Q

primary circulation, large-scale movements

A

Tropospheric airflow

20
Q

Horizontal movements

A

 Pressure gradient
 Coriolis
 Friction

21
Q

Vertical movement

A

 Cooling, heating (changes in density; changes
in pressure with altitude)

22
Q

A fluid tends to move from high pressure region to low pressure region

A

Pressure Gradient Force

23
Q

Deflection, depending on which hemisphere you are: north, right; south, left

A

Coriolis force

24
Q

a force that tends to dissipate the energy of a moving body
it acts in the direction opposite the direction of surface air movement

A

Frictional Forces

25
Warm air rises at the equator
Atmospheric convection cell
26
not necessarily continuous ; Two essentially circumpolar jet streams within the mid-latitude region
Jet streams ;  Subtropical jet stream  Polar front jet stream
27
an area of strong winds ranging from 120-250 mph that can be thousands of miles long, a couple of hundred miles across and a few miles deep. Jet streams usually sit at the boundary between the troposphere and the stratosphere at a level called the tropopause
Jet streams
28
driven by a strong horizontal temperature contrast
Jet formation
29
part of the atmosphere that has relatively little variation in temperature. Develops over several days under relatively calm condition.
Air mass
30
formed where two masses of different temperature meet.
Front
31
formed where two masses of different temperature meet.
Front
32
When two air masses with different temperature, humidity, and maybe also pressure, collide, it is created.
Front
33
are areas of low pressures that develop at fronts.
Extratropical cyclones
34
are areas of high pressure.Divergent surface air flow. Lower wind speed (smaller pressure gradient) than that in extratropical cyclone
Anticyclones
35
are separated by a certain distance the closer they are the more wind will be.
Isobars
36
depends on its ability to resist vertical motion.
stability
37
makes vertical movement difficult, and small vertical disturbances dampen out and disappear.
stable atmosphere
38
coastal breeze blowing from sea to land caused by the temperature difference
Sea breeze
39
coastal breeze flowing from land to sea caused by the temperature difference when the sea surface is warmer than the adjacent land.
Land breeze
40
bathed in moist maritime and continental air
East coast of Asia
41
The wind flow is reversed in the summer months, brining moist maritime winds and greater rain
Eurasian interior
42
Essentially same climatic influences as those in the north
Southern hemisphere