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Test your basic knowledge |
Global Warming
Start Test
Study First
Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
.
Match each statement with the correct term.
Don't refresh. All questions and answers are randomly picked and ordered every time you load a test.
This is a study tool. The 3 wrong answers for each question are randomly chosen from answers to other questions. So, you might find at times the answers obvious, but you will see it re-enforces your understanding as you take the test each time.
1. Number of days when temperatures climb above average by a fixed amount.
Air pollution
Threshold departures
Surface Mass Balance
45%
2. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
GHG
Why Water Vapor is not a climate forcing
75-OC
Black Carbon
3. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
Normal condition for air
Surface Mass Balance
How the cryosphere is affected by climate change
Questions to think about
4. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Ice Discharge
Discontinuous
Antarctica
Ice/snow
5. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Strong
Talik
Greenland
6. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Wetter; drier
Grounding Lines
45%
Monthly maximums and minimums
7. A thick - floating slab of freshwater ice extending from coast to coast.
Carbon Dioxide
Thermokarst
Dry
Ice shelf
8. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Cloud Feedbacks
Positive
1 m/yr; 10x
.7O Celsius over the past century.
9. Reduction of snow and ice cover - Changes in atmospheric circulation.
Ice/snow
Cause of break of inversion layers or decrease in frequency
Surface Mass Balance
Climate Change in the Arctic
10. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Cause of break of inversion layers or decrease in frequency
% of Greenhouse Gases
Atmospheric Composition
11. Rainy on yearly average. In these regions - rising air predominates.
Sea ice melt does not change sea level
Greenland
Deep tropics between 15O N and 15 O S are quite
Ozone
12. Measures input and output.
Climate Change in the Arctic
Ice Shelf
Mass Budget
30%
13. The order of 1 m/year. Melting is ten times more.
Sea-Ice Albedo
Surface Mass Balance
Mass Change
50%
14. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Importance of ice sheets
Indirect heat wave effect
Methane
Negative Ice-Albedo Feedback
15. Longwave radiation - any radiation with a long wave will heat up quickly.
reduction in sea-ice
Ice Sheets
Infrared radiation
In the Arctic where the air is cooler
16. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Active Layer
Through talik
Thermokarst Lake
70%
17. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
In the Arctic where the air is cooler
Surface Mass Balance
Thickness of the active layer and the permafrost depend on this
The Ozone Hole
18. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
IN the last 2 decades what we've seen
Climate Change in the Arctic
Melt
Affect Floods and Droughts
19. Warming- positive feedback - Cooling- negative feedback.
20%
Precipitation and High Latitudes
Ice-Albedo
Ice Discharge
20. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
25%
Positive feedbacks both found in...
Through talik
21. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Global warming and hot nights?
El Nio is in the coasts of...
How to define a heatwave
Why ice-albedo feedback is a big deal in the Arctic
22. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Methane
Inversion Layer Winter
Effect of Deforestation on CO-2
23. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
% of Greenhouse Gases
Thinner atmosphere
Warming; cooling
Earth's tilt
24. The past climate...for this reason - both keep good records of climate change.
Very small portion
Permafrost
Ice absorbs
Thickness of the active layer and the permafrost depend on this
25. Set up in 1988 by WMO and UNEP.
Warming; cooling
Grounding Lines
Effect of Deforestation on CO-2
IPCC
26. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Ice-Ocean Interactions
Greenhouse Gases
air can warm dramatically
Albedos of Snow and Ice
27. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
50%
% of Greenhouse Gases
Radiative Forcing
Ice Discharge
28. Ice sheets have a very ____ Albedo
How a closed talik forms
In the Arctic where the air is cooler
Strong
The Ozone Hole
29. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
In the Arctic where the air is cooler
How a closed talik forms
Active Layer
Increases - decreases
30. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Changes in Arctic sea-ice Extent
Ice Sheets
Precipitation and High Latitudes
% of Greenhouse Gases
31. 85%
Sea-Ice Albedo
Today melting ice
Ice Motion
Thermohaline Circulation
32. Reduction of Summer Sea- will increase the warming because less energy will be reflected back to the atmosphere by the ice and more will be absorbed by the ocean - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Layers of Earth
Reduction in sea-ice extent
Thinner atmosphere
Hydrological Drought
33. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Greenland
El Nio is in the coasts of...
Earth's tilt
Ozone Hole
34. High vs low
Thermohaline Circulatoin
Stronger
In the troposphere that we live in.
Cloud Feedbacks
35. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Atmospheric Circulation
Positive feedbacks both found in...
Wetter; drier
36. Where does the ozone protect us?
Positive feedbacks both found in...
In the stratosphere.
Types of Albedo
Thickness of the active layer and the permafrost depend on this
37. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
30%
Ice absorbs
7%
Black Carbon
38. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
Antarctica
Thermohaline Circulation
Albedo
39. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
Absolute thresholds
Ice-Ocean Interactions
Altimetry Cons
40. 1.4 USA - 57 m total sea level equivalent
Through talik
Ocean water
Albedos of Snow and Ice
Antarctica
41. The Earth emits this.
Layers of Earth
Why ice-albedo feedback is a big deal in the Arctic
Longwave Radiation
Cloud Feedbacks
42. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Layers of Earth
Permafrost Degradation
Stronger
Albedo
43. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Where rise in OC is greatest
Accumulation
Atmospheric Structure
Ocean water
44. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
In the Arctic where the air is cooler
Permafrost
The cryosphere
45. Antarctica - stratosphere - Sep-Oct
Ozone Hole
30%
Permafrost
Average radiative flux reaching the atmosphere
46. In ________- inversion layer is more common in the Arctic
winter
Rainy
Energy Budget
Where rise in OC is greatest
47. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Atmospheric Composition?
La Nia
Ice Motion
Antarctica
48. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Why the Arctic climate is special
Accumulation
Black Carbon
Ice Shelf
49. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
75-OC
Why the Arctic climate is special
Layers of Earth
Thermohaline Circulation Effect
50. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Permafrost Degradation
Atmospheric Composition?
Today melting ice
How we measure Mass Balance