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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. Greenhouse gases are mixed in the ____
Troposphere
Calving
Albedos of Snow and Ice
Heat wave
2. 85%
Natural Causes of Warming
In the troposphere that we live in.
Sea-Ice Albedo
Discontinuous Permafrosrt
3. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Affect Floods and Droughts
Agricultural Drought
30%
In the troposphere that we live in.
4. x7 smaller - 7m total sea level equivalent.
Greenland
Surface Mass Balance
Average radiative flux reaching the atmosphere
The cryosphere
5. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Antarctica
Discontinuous Permafrosrt
Through talik
Climate Change in the Arctic
6. Number of days that exceed a given temperature
Cause of break of inversion layers or decrease in frequency
Some regions of the Earth have warmed faster than other regions.
Absolute thresholds
Types of Albedo
7. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Questions to think about
In the troposphere that we live in.
Grounding v Surface Melting
Inversion Layer Winter
8. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Dry
All Greenhouse gases
Thermokarst
Ozone Hole
9. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Nitrous Oxide (N2O)
Wetter; drier
Hydrological Drought
Why ice-albedo feedback is a big deal in the Arctic
10. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Talik
US and precipitation
Layers of Earth
Atmospheric Composition?
11. US is responsible for ___ of the total CO2
30%
Altimetry (height)
Stronger
Sea-Ice Albedo
12. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Mass Budget
Frozen Soil
Heat Source and Pressure
Global warming and hot nights?
13. 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.
Infrared radiation
.7O Celsius over the past century.
Ice Sheets
Ice Shelf
14. Carbon dioxide - Methane - Ozone - Water Vapor - Few others - Most ___________________ are mixed in the troposphere (Except water vapor) - Water vapor is concentrated closer to the ground.
Greenhouse Gases
The cryosphere
Warm
Altimetry
15. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
Cause of break of inversion layers or decrease in frequency
Average radiative flux reaching the atmosphere
Why Water Vapor is not a climate forcing
16. Industrial product - 300 ppb (parts per billion)
Ice Cap
Cause of break of inversion layers or decrease in frequency
Nitrous Oxide (N2O)
Grounding v Surface Melting
17. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Ice-Ocean Interactions
reduction in sea-ice
More rain means no drought
Atmospheric Composition
18. Rainy on yearly average. In these regions - rising air predominates.
Increases - decreases
Ocean water
What happens with the Ozone Hole
Deep tropics between 15O N and 15 O S are quite
19. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
The cryosphere
Thinner atmosphere
Discontinuous
20. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Stratospheric Ozone Depletion
Shortwave Length
Active Layer
Albedos of Snow and Ice
21. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Inversion Layer (feedback)
Hydrological Drought
Thermohaline Circulation
Atlantic Thermohaline Circulation
22. CO2 GHG forcing - H2O - dominant/major GHG
Rainy
GHG
Deep tropics between 15O N and 15 O S are quite
Troposphere
23. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
The cryosphere
Ocean water
Atlantic Thermohaline Circulation
24. Set up in 1988 by WMO and UNEP.
Ice Shelf
IPCC
20%
Warm
25. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Threshold departures
Mass Change
Sunspots
The cryosphere
26. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Sublimation
Cause of break of inversion layers or decrease in frequency
How we measure Mass Balance
US and precipitation
27. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Shortwave Length
How talik forms under lakes
Ice absorbs
Inversion Layer (feedback)
28. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Accumulation
Atmospheric Structure
30%
29. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Methane
How the cryosphere is affected by climate change
Shortwave Length
How we measure Mass Balance
30. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Carbon Dioxide
Dry
Permafrost Degradation
Increases - decreases
31. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Hydrological Drought
Altimetry Cons
Surface Mass Balance
Thickness of the active layer and the permafrost depend on this
32. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
What effects the density
In the troposphere that we live in.
Reduction in sea-ice extent
Severe coastal erosion
33. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Calving
Active Layer
Altimetry
Shortwave Length
34. How often does El Nio occur?
Why Water Vapor is not a climate forcing
Percentile departures
Talik
Once every 4 years.
35. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Major distinction between Kyoto Protocol and Convention
Thermokarst
% of Greenhouse Gases
Antarctica
36. Warming- positive feedback - Cooling- negative feedback.
Active Layer
7%
The Ozone Hole
Ice-Albedo
37. Total absorbed solar radiation
70%
Ice Shelf
Thermokarst
In the stratosphere.
38. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Ice Sheets
Atmospheric Circulation
Grounding Lines
39. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
Sublimation
Permafrost
70%
Radiative Flux
40. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Discharge
Through talik
Time Variable Gravity
Thermokarst
41. CO2 - CH4 - O3 - H2O - N2O - CFCs
doubles
All Greenhouse gases
Snow and snow covered ice absorb
Climate Change in the Arctic
42. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
1 m/yr; 10x
Albedos of Snow and Ice
In the Arctic where the air is cooler
Ice Sheets
43. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
30%
Hydrological Drought
Mass Balance
Arctic Atmosphere
44. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Sunspots
All Greenhouse gases
Mass Change
How to define a heatwave
45. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Is precipitation around the world increasing?
Changes in Arctic sea-ice Extent
Thermohaline Circulation
Arctic Atmosphere
46. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Indirect heat wave effect
Atmospheric Circulation
Earth's tilt
Permafrost Degradation
47. Where does the ozone protect us?
In the stratosphere.
Ice shelf
Altimetry Cons
Thermohaline Circulation Effect
48. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
45%
Greenhouse Gases
Snow and snow covered ice absorb
Discontinuous
49. Unfrozen ground that is found within a mass of permafrost
Closed talik
Troposphere
Heat wave
30%
50. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Sea Ice
Closed talik
Radiative Forcing
Ice loss