3. General Circulation Flashcards

1
Q

What is the ozone hole?

A

depletion of O3 related to the atmospheric chemistry, exacerbated by bromine, chlorine, and chlorofluorocarbons (CFCs), Montreal Protocol, as it thins more UV rays come through - burn easier, annual minimum during the spring months

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2
Q

What is the Montreal Protocol?

A

1987: phased out the productions of numerous substance related to ozone depletion

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3
Q

What is latent heat flux?

A

energy that is stored in water vapor as it evaporates, strongest where there’s surface moisture and a strong gradient between surface and air temp and humidity

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4
Q

what is sensible heat flux?

A

dry air convection, strongest where there’s gradient in temp between the surface and air temp, conduction and advection, and radiation

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5
Q

What is specific heat?

A

amount of hear per unit mass required to raise temps by 1C

  • high = object warms and cools slowly (ocean, rivers, lakes)
  • low = object warms and cools fast (land)
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6
Q

What is the Coriolis effect?

A

describes the apparent deflection of objects moving in a straight path relative to earth’s surface - northern hemisphere objects are deflected to the right from place of origin; southern hemisphere objects are deflected to the left from place of origin

  • earth rotates west to east (counter-clockwise)
  • 839km/hr at poles & 1674km/hr at equator
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7
Q

What is convergence?

A

hot air rising is associated with low pressure, involves low pressure and high pressure areas, law of mass continuity

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8
Q

Explain a low-pressure area.

A
  • low/depression; a region where atmospheric pressure is lower than that of surrounding locations.
  • rising air; cools area, makes clouds and brings rain
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9
Q

What is the law of mass continuity?

A

empty spaces aren’t tolerated, air always moves to fill them in causing rotational cycles

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10
Q

Explain high-pressure areas.

A
  • high/anticyclone; region where atmospheric pressure at the surface is greater than its surrounding environment.
  • sinking air; warms area, clear sky, brings drier air
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11
Q

Why do large storms spin?

A
  • Coriolis effect, low pressure at the middle of the storm - high pressure comes rushing back pulling is to the right (counter clockwise) - northern hemisphere
  • tropopause is more dense because air is cooler causing molecules to condense making it shrink - still same size in mass
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12
Q

Draw general circulation of Earth.

A

*

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13
Q

What is the ITCZ?

A
  • InterTropical Convergence Zone

- relatively little wind (equator), storms are built upwards and not in fronts like other parts of the world

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14
Q

Explain the preferential pressure patterns.

A
  • the Hadley cell moves N&S depending on the time of the year
  • south - July: Aleutian low (Alaska), Pacific high (Cali), Azores high (Golf last > Africa), Icelandic low (Iceland), & Siberian high (Asia)
  • north - January: Pacific high (Cali), Azores high (Golf last > Africa), Icelandic low (Iceland), & Tiberian low (Asia)
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15
Q

What is the polar jet stream?

A

current of fast moving air in the upper troposphere at boundary of polar front

  • may be thousands of miles long but only 10s of miles wide
  • develops aloft and leaders above high pressure anticyclones (ridges) and below low pressure cyclones (troughs)
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16
Q

what is a gyre?

A

large system of rotating ocean currents with dynamics determined by presence of coastlines

17
Q

Explain the western boundary currents.

A

warm, deep, narrow, and fast flown currents that flow from the west side of ocean basins - tropics > poles (gulf stream)

18
Q

Explain the eastern boundary currents.

A

shallow, broad, and slow currents from eastern side of ocean basins - west coasts > equator-ward
-promotes upwelling

19
Q

What is upwelling?

A

mechanism that involves alone shore currents and Coriolis effect that brings cover, nutrient rich water from the depths of the cease to the surface
-some of the most biologically productive areas