Unit 4 Flashcards

You may prefer our related Brainscape-certified flashcards:
1
Q

The atmosphere

A
– Thin, shell-like envelope of life 
sustaining air that surrounds the 
Earth
– Consists of gases, liquids, and solids
– Reactions occur throughout the 
atmosphere
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

atmospheric elements

A
  • Temperature
  • Humidity
  • Cloudiness
  • Precipitation
  • Pressure
  • Wind speed/direction
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

atmospheric pressure

A

the weight of the air above
– At sea level, the average
atmospheric pressure (MSLP) is close to 1000 millibars
-DECREASES EXPONENTIALLY WITH HEIGHT

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Relationship between mass and height

A

inverse; atmospheric mass decreases with height

it is caused by_____

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

origin of the atmosphere

A

• Formed through a combination of volcanic outgassing and material
from outer reaches of solar system
• Early on mostly consisted of water vapor and carbon dioxide
• Planet eventually cooled allowing water vapor to condense and fall as
rain
– Falling rain drops carried carbon dioxide from the atmosphere to the ocean
– Could combine with other materials forming carbon bearing rocks and organisms
• Photosynthesis increased oxygen amounts

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

physical atmospheric processes

A

– Change in the appearance of a substance in which it can change
back to its original state
• Ex: Phase changes of water

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

chemical atmospheric processes

A

– Change of a substance into a new one that has a different chemical identity
•Ex: Lightning

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

biological atmospheric processes

A

– With life involved, change a
substance into a new one with a different chemical identity
• Ex: Photosynthesis

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

homosphere

A
Lower region of the 
atmosphere
• Uniform chemical composition
• Almost all of the atmospheric 
mass is found in this region
• Homosphere contains:
– Constant gases
– Trace gases
– Particulates
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

constant gases

A
– Found in same percentages all over world
– Little yearly or seasonal variation
– Constant gases include:
• Nitrogen
• Oxygen
• Argon
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

nitrogen

A

– 78 percent
– Nearly inert
– Residence time = 13 million years

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

oxygen

A
– 21 percent
– Crucial for life
– 3 forms of Oxygen
• O
• O2
• O3*
– Residence time = 5,000 years
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

argon

A

– 0.9 percent
– Inert gas
– Residence time = infinite

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

trace gases (variable gases)

A
– Constitute only a tiny proportion of the air 
– Present in varying quantities
– Trace gases include:  
• Carbon dioxide
• Water Vapor
• Ozone (O3)
• Methane
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

carbon dioxide (trace gases)

A
– 0.04 percent or 390 ppm
– Most important for climate change
• Absorbs and emits longwave 
(terrestrial) radiation
– Residence time = around 40 years
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

water vapor (trace gases)

A

– 1 to 4 percent
• Deserts and cold regions vs. oceans and warm areas
– Crucial for clouds and rainfall
– Residence time = less than two weeks

17
Q

ozone (o3)

A
– Rarer type of oxygen molecule
– 2 to 10 ppm
– Good absorber/transmitter of 
longwave (terrestrial) radiation
– Absorbs UV (solar) radiation
18
Q

methane (CH4)

A
– 1.8 ppm
– Better absorber of longwave 
(terrestrial) radiation than carbon 
dioxide
– Residence time = 10 years
19
Q

Particulates

A
– Any suspended or falling liquid or 
solid
• Clouds
• Sea salts
• Fine soils
• Smoke
• Soot
• Pollen
• Ash
• Nongaseous components
20
Q

heterosphere

A
• Extends beyond the 
homosphere in the upper 
region where the chemical 
composition changes 
• Gases start to settle according 
to molecular weigh
21
Q

arrangement of atmosphere

A

– Altitude has a major influence on
temperature
• Divided into 4 spheres
• Separated by 3 pauses

22
Q

troposphere

A
– Troposphere
• Lowest 15 km (9 mi) 
• All life and weather occurs here
• Temperature decreases with height
– Average lapse rate = 6.5 C/km 
(3.5F/1000ft)
– Lapse rate?
23
Q

tropopause

A

• Boundary between troposphere and
stratosphere
• Height varies with latitude

24
Q

stratosphere

A
– Stratosphere
• 15 to 50 km (9 to 32 mi)
• Thinner, clear air than troposphere 
• Jets fly here
• Ozone layer
– Temperature inversion
25
Q

stratopause

A

• Boundary between stratosphere and

mesosphere

26
Q

mesosphere

A
  • 50 to 95 km (31 to 60 mi)
  • Temperature decreases with height
  • Coldest temperatures on Earth
27
Q

mesopause

A

• Boundary between mesosphere and

thermosphere

28
Q

thermosphere

A
• 95 to 1000 km (60 to 620 mi)
• Temperature increases with height 
due to the absorption of very 
shortwave, high energy solar radiation 
by atoms of oxygen and nitrogen.
• Auroras
29
Q

ideal gas law

A

A basic relation between pressure, density, and temperature of air