Chapter 3 Flashcards

1
Q

Air

A

mix of nitrogen, oxygen, small amounts of solid/liquids

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2
Q

Atmospheric density

A

shallow atmosphere –> more than 50% of atmosphere below Mt Denali elevation

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3
Q

Permanent gases

A

Nitrogen (78%) and oxygen (21%) argon (1%)
nitrogen = added by decay/burning organic matter + volcanic eruptions, removed by nitrogen fixation + lightning
oxygen produced by vegetation + consumed by organisms

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4
Q

Variable gases

A

Water Vapor = abundant over warm, moist surfaces; very small amounts over polar regions/deserts –> hence variable; important role in storing latent heat

Carbon dioxide: significant effect on climate (like water vapor), uniform in lower layers of atmosphere, increasing bc of human activities

Ozone = 3 oxygen atoms, located in ozone layer (9-30 miles above Earth), absorbs UV rays

Other = methane, carbon monoxide, sulfur dioxide, nitrogen oxides, many harmful + caused by emissions

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5
Q

Aerosols/particulates

A

solid/liquid particles small enough to remain suspended in atmosphere
Sources = human activities, volcanic ash, windblown soil

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6
Q

Characteristic’s of aerosols

A

hygroscopic - many absorb water, so water vapor condenses around “condensation nuclei” –> important for cloud formation

absorb/reflect radiation –> influences temp

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7
Q

Layers of the atmosphere

A

Troposphere, stratosphere, mesosphere, thermosphere, exosphere

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8
Q

Troposphere (t for turbulent)

A

1) Depth varies depending on time/place, generally deepest over warm tropics, shallowest over cold poles
Characteristics:
1) temp decreases with increasing altitude (going farther away from heat of surface)
2) tropopause = upper limit of surface-initiated turbulence
3) 80% of atmospheric mass in troposphere
4) most clouds formed here

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9
Q

Stratosphere (s for stagnant)

A

1) Stagnant air
2) constant temperatures in lower half, after that it increases to max at bottom of Mesosphere
3) ozone layer here

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10
Q

Mesosphere

m for minimum

A

30 to 50 miles above sea level
temperature reaches minimum, lacks source of warmth, meteors burn up here

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11
Q

thermosphere

A

1) 50 miles +
2) temperature hot –> UV rays
3) no definite top, merges with exosphere (interplanetary space)

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12
Q

Pressure

A

Troposphere has most pressure –> most mass

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13
Q

Homosphere

A

up to 50 miles above sea level
zone of homogenous composition of gases

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14
Q

Heterosphere

A

Above homosphere –> no homogenous composition of gases
layered by atomic weight –> heaviest at bottom (N2), lightest at top (H)

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15
Q

Ozone layer

O ZONE (2nd)

The silly monkey takes eggs

A

in lower stratosphere, very small amount of ozone (not that concentrated)

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16
Q

ionosphere

3 syllables –> 3rd

the silly monkey takes eggs

A

full of ions –> mesosphere + lower thermosphere (40-250 miles)
aids in radio communication + causes northern lights

17
Q

Weather vs climate

A

Weather = constant state of change
Climate = aggregate of weather –> at least 30 years of data

18
Q

Six controls of weather/climate

lucas donates apples on alternating tuesdays

A

1) latitude
2) distribution of land/water
3) general circulation of atmosphere
4) general circulation of oceans
5) altitude
6) topographic barriers

19
Q

Weather control: latitude

A

different latitudes receive diff amounts of sunlight + energy –> warming/cooling of earth

20
Q

Weather control: Distribution of land and water

A

Areas w. more water = cooler, milder climates since water has high specific heat capacity

21
Q

Weather control: General circulation of atmosphere

A

varying circulation of atmosphere i.e. in tropics surface winds come from East but in middle latitudes they come from west
(different weather systems + winds)
Storms = some prominent + frequent enough to affect weather + climate

22
Q

Weather control: general circulation of oceans

A

1) broad general pattern of currents that move warm water to poles + cool water to equator
big effect on coastal climates

23
Q

Weather control: altitude

A

temperature, pressure, moisture decrease with increasing altitude
big effect in mountainous regions

24
Q

weather control: Topographic barriers

A

Large barriers i.e. mountains can cause rainshadow effects

25
Q

Coriolis Effect

A

deflection in path of free moving objects
BASICALLY winds + ocean currents in northern hemisphere go to right + winds in southern go to left

26
Q

Effects of coriolis effect

A

1) Northern hemisphere = deflect right
2) Southern hemisphere = deflect left
3) deflection strongest at poles
4) no deflection at equator
5) fast moving objects deflected more
6) only affects direction not speed of object
No effect on circulation of water draining

27
Q

What caused thinning of ozone

A

Use of CFCs (freon in refrigerating components)
CFCs broken down by UV radiation in ozone layer, react with ozone breaking the O3 apart
100K ozone molecules destroyed for every Cl atom released

28
Q

What was the Montreal Protocol?

A

196 countries banned use of CFC, eventually became a global ban

29
Q

Primary Air pollution gases

A

CO: most plentiful primary pollutant
NO: leads to acid rain + NO2 (gives yellow color to air)
Sulfur: rotten egg smell, leads to acid rain
Particulates: smoke + dust from industrial activities, smallest particles most dangerous for health

30
Q

Secondary pollutants

A

Primary - released directly into air
secondary - form as consequence of chemical reactions in atmosphere (i.e. photochemical smog)

31
Q

photochemical smog

A

smog made up of nitrogen dioxide + hydrocarbons –> reacts w. UV to form brown haze (caused bc an extra oxygen is released creating ozone which damages vegetation, body tissues, etc)

32
Q

temperature inversions

A

cooler air below, warmer air above
forms a lid over polluted area which inhibits updrafts + air movement

33
Q

effect of air pollution

A

cardiovascular disease, respiratory (1/5 of respiratory illness caused by ground level ozone)