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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. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Thickness of the active layer and the permafrost depend on this
Depth v Surface
IN the last 2 decades what we've seen
2. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice Discharge
GHG
Permafrost
3. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Types of Albedo
75-OC
Altimetry Cons
.75OC/km-1
4. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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5. Really measures volume.
Inversion Layer (feedback)
Atmospheric Composition
Altimetry
Why Water Vapor is not a climate forcing
6. Reduction of snow and ice cover - Changes in atmospheric circulation.
Cause of break of inversion layers or decrease in frequency
Atmospheric Composition
Albedo
Affect Floods and Droughts
7. 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
Dry
Thermohaline Circulatoin
Sunspots
Ice-Ocean Interactions
8. Set up in 1988 by WMO and UNEP.
Questions to think about
IPCC
Indirect heat wave effect
Snow and snow covered ice absorb
9. Volcanic eruptions - Sunspots - Wobbly Earth
doubles
Natural Causes of Warming
Methane
Rainy
10. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Meteorological Drought
Accumulation
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Strong
11. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
Change in vegetation generates a further feedback
Agricultural Drought
Thermohaline Circulatoin
12. x7 smaller - 7m total sea level equivalent.
Greenland
Albedo
El Nio is in the coasts of...
Today melting ice
13. US is responsible for ___ of the total CO2
Ice Shelf
reduction in sea-ice
Severe coastal erosion
30%
14. CO2 GHG forcing - H2O - dominant/major GHG
Affect Floods and Droughts
GHG
The Ozone Hole
Inversion Layer (feedback)
15. The past climate...for this reason - both keep good records of climate change.
Ice Motion
Troposphere
Thickness of the active layer and the permafrost depend on this
Methane
16. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Energy Budget
Closed talik
Inversion Layer (feedback)
The Ozone Hole
17. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
Earth's tilt
Frozen Soil
Ice-Ocean Interactions
18. A thick - floating slab of freshwater ice extending from coast to coast.
Atmospheric Circulation
Ice shelf
.75OC/km-1
Importance of ice sheets
19. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
Calving
doubles
Archimedes' Principle
Radiative Forcing
20. ~15% of incident solar energy (albedo 85)
Layers of Earth
Surface Mass Balance
In the stratosphere.
Snow and snow covered ice absorb
21. 1.4 USA - 57 m total sea level equivalent
Altimetry Cons
Antarctica
Amount of light actually reaching the Earth
Where rise in OC is greatest
22. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Atmospheric Circulation
Hydrological Drought
How we measure Mass Balance
Negative Ice-Albedo Feedback
23. 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
Ice Motion
Sunspots
Agricultural Drought
20%
24. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
25%
Why ice-albedo feedback is a big deal in the Arctic
Ice Motion
Ozone
25. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
75-OC
Altimetry (height)
Permafrost
26. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Shortwave Length
Types of Albedo
45%
27. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Natural Causes of Warming
Methane
Snow and snow covered ice absorb
Ice Motion
28. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
US and precipitation
Average radiative flux reaching the atmosphere
Talik
El Nio is in the coasts of...
29. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Heat wave
Ice absorbs
Discontinuous
Thermokarst Lake
30. In average: +1% in respect to 100 years ago.
Heat Source and Pressure
Sea ice melt does not change sea level
Thermohaline Circulation Effect
Is precipitation around the world increasing?
31. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sublimation
50%
Ocean water
Nitrous Oxide (N2O)
32. Number of days that exceed a given temperature
IN the last 2 decades what we've seen
Absolute thresholds
Ice Motion
How to define a heatwave
33. Tundra absorbs more energy than ice and snow but less than scrubs and forest - and with those plants migrating towards the north - they will further contribute ot absorb more energy.
Ice shelf
Albedos of Snow and Ice
7%
Change in vegetation generates a further feedback
34. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Permafrost
Dry
Shortwave Length
35. Warming- positive feedback - Cooling- negative feedback.
In the troposphere that we live in.
Agricultural Drought
Ice-Albedo
Heat Source and Pressure
36. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Dry
Why ice-albedo feedback is a big deal in the Arctic
Natural Causes of Warming
Severe coastal erosion
37. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Antarctica
Inversion Layer Summer
70%
Atmospheric Composition
38. How much is the planet really warming?
.7O Celsius over the past century.
Today melting ice
Methane
Permafrost
39. Unfrozen ground that is found within a mass of permafrost
Radiative Flux
Energy Budget
Through talik
Closed talik
40. Is not an externally imposed perturbation to the climate system.
La Nia
Why Water Vapor is not a climate forcing
Negative Ice-Albedo Feedback
Ice Shelf
41. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Altimetry Pros
Types of Albedo
Strong
Talik
42. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Depth v Surface
In the stratosphere.
Severe coastal erosion
43. Clouds 40~90% - Vegetation 10~15%
Thermohaline Circulation Effect
Ocean-Ice-Atmosphere Interaction
Types of Albedo
Albedo
44. More common
Inversion Layer Winter
Types of Albedo
What effects the density
Heat Source and Pressure
45. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Atmospheric Circulation
Grounding Lines
Cloud Feedbacks
Surface Mass Balance
46. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Why ice-albedo feedback is a big deal in the Arctic
Ocean-Ice-Atmosphere Interaction
How a closed talik forms
Questions to think about
47. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ice Sheets
air can warm dramatically
Ozone Hole
The cryosphere
48. 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.
Some regions of the Earth have warmed faster than other regions.
Thermohaline Circulation
Greenhouse Gases
Albedo
49. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Calving
Questions to think about
Methane
50. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
Grounding v Surface Melting
What happens with the Ozone Hole
Severe coastal erosion
Calving