Chapter 18-Global Climate Change Flashcards

You may prefer our related Brainscape-certified flashcards:
0
Q

The layer closest to the surface of the Earth. This layer extends from the Earth’s surface to 5-10 miles high (8-16 km). This layer contains practically all of the water vapor and clouds in the atmosphere and is the site and source of our weather. Temperature decreases as you go up in this layer

A

Troposphere

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

Caps the troposphere

A

Tropopause

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

Layer that extends from the top of the troposphere to about 40 miles high. This layer contains ozone (O3) which is a form of oxygen that absorbs high-energy radiation emitted by the sun. The temperature increases as you go up in this layer.

A

Stratosphere

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

The day-to-day variations in temperature, air pressure, wind, humidity, and precipitation

A

Weather

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

The long-term weather patterns in an area

A

Climate

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

The study of weather and climate

A

Meteorology

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

This brings us the day-to-day changes in our weather as it moves in a general pattern from west to east. Vertical air currents caused by warmer air from the surface rising, expanding, cooling, and then sinking again

A

Convection currents

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

Rivers of air high in the troposphere that flow eastward at speeds of more than 300 mph

A

Jet streams

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

Air masses of different temperatures and pressures meet at boundaries; regions of rapid weather change

A

Fronts

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

Major seasonal airflows which often represent a reversal of previous wind patterns; created by major differences in cooling and heating between oceans and continents

A

Monsoons

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Established in 1988, by the United Nations Environment Program and the World Meteorological Society; this panel, which consists of more than 2,000 unpaid workers from a hundred countries, gathers and examines scientific data in an attempt to gain a better understanding of whether humans are inducing climate change

A

Intergovernmental Panel on Climate Change

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Climate shifts due to variations in Earth’s orbit

A

Milankovitch cycles

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

The effects that temperature and salinity have on the density of seawater

A

Thermohaline

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

System that acts as a giant belt, moving water masses from the surface to deep oceans and back again, according to the density of the mass

A

Conveyor system

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

A phenomenon of one of the most impressive demonstrations of the oceans’ impact on climate

A

El Niño/La Niña Southern Oscillation (ENSO)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Occurs when a major shift in atmospheric pressure over the central equatorial Pacific Ocean leads to a reversal of the trade winds that normally blow from an easterly direction. Warm water spreads to the east, the jet streams strengthen and shift from their normal courses, patterns in precipitation and evaporation are affected, and the system is usually sustained for more than a year

A

El Niño

16
Q

The easterly trade winds are reestablished with even greater intensity, upwelling of colder ocean water in the eastern Pacific from the depths replaces the surface water blown westward, the jet streams are weakened, and weather patterns are again affected; encourages cooling

A

La Niña

17
Q

The influence a particular factor has on the energy balance of the atmosphere- ocean-land system

A

Radioactive forcing

18
Q

Contribute to atmospheric warming; include water vapor, carbon dioxide, and other gases in the atmosphere

A

Greenhouse gases

19
Q

Contributes to global cooling; clouds reflect 23% of solar radiation back to space before it ever reaches the planet. Low-lying, fluffy clouds have a negative forcing effect, while High-lying clouds have a positive forcing effect. Snow and ice (the cryosphere) also reflect sunlight. Soot originating from anthropogenic sources darkens the snow and ice. Therefore, the soot promotes the absorption of radiant energy rather than reflection

A

Planetary albedo

20
Q

Contribute to global cooling. Particles and aerosols enter into the atmosphere and spread around the world, causing solar radiation to be reflected back to space

A

Volcanoes

21
Q

From pollution can cause a haze to form in the atmosphere which reflects and scatters some sunlight and also contributes to the formation of clouds

A

Aerosols

22
Q

(From fires) has an overall warming effect

A

Sooty aerosols

23
Q

Oceans are experiencing a decrease in pH

A

Ocean acidification

24
Q

Where most of the ice on earth can be found

A

Antarctic

25
Q

Burning of fossil fuels and the burning of forest trees (deforestation)

A

Anthropogenic sources

26
Q

Carbon emissions are removed annually

A

Carbon sinks

27
Q

Absorbs infrared energy and is the most abundant greenhouse gas

A

Water vapor

28
Q

As temperatures rise, water vapor in the atmosphere increases and warming accelerates; one of the more disturbing features of future warming

A

Positive feedback

29
Q

The third-most important greenhouse gas; product of microbial fermentative reactions; its main natural source are wetlands and green plants

A

Methane

30
Q

Levels have increased some 19% during the last 200 years. Sources of the gas include agriculture, the oceans, and the burning of biomass; lesser quantities come from fossil-fuel burning and industry. Produced in agriculture via anaerobic denitrification processes, which occur wherever nitrogen is highly available in soils. This gas accelerates warming in the troposphere and also contributes to depletion of the ozone in the stratosphere. Has a long residence time of 114 years in the atmosphere

A

Nitrous oxide (N2O)

31
Q

A potent greenhouse gas which forms in the stratosphere and descends into the troposphere. Major sources contributing to increasing levels of ozone are automotive traffic, burning forests, and agricultural wastes

A

Ozone (O3)

32
Q

Entirely anthropogenic; long lived and contribute to both global warming in the troposphere and ozone destruction in the stratosphere. Used as refrigerants, solvents, and fire retardants, have a much greater capacity (10,000 times) for absorbing infrared radiation than does CO2

A

CFCs and other halocarbons

33
Q

Now called the Global Change Research Program (GCPR) places emphasis on the government’s approach to climate research; the focus of the plan is to address a number of issues in climate science especially climate change

A

Climate Change Science Program (CCSP)

34
Q

Refers to actions designed to reduce greenhouse gas emissions

A

Mitigation

35
Q

Agreement to stabilize greenhouse gas levels in the atmosphere to 1990 levels by the year 2000 which ended up failing

A

Framework Convention on Climate Change (FCCC)

36
Q

In 1997, nations met in Kyoto, Japan and agreed on ways to reduce greenhouse gas emissions; agreement is to reduce six types of greenhouse gas emissions to 5.2% below 1990 levels by 2012

A

Kyoto Protocol

37
Q

Reached an agreement on two principles once the Kyoto process expires in 2012. First, there would be future meetings aimed at producing a new, tougher set of binding limits on GHG emissions that would take effect after 2012. Second, there would be broader dialogues towards reaching nonbinding accords addressing global climate change

A

U.N. Climate Control Conference

38
Q

Accepting that climate change is happening and taking action to lessen the impact of this change

A

Adaptation