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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. In _______ - the inversions are less frequent and weaker in the Arctic.
Albedo
Altimetry Pros
summer
Ozone Hole
2. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Absolute thresholds
Mass Budget
Accumulation
7%
3. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Carbon Dioxide
Inversion Layer Summer
What effects the density
Positive feedbacks both found in...
4. The amount of light reflected by an object.
Wetter; drier
1 m/yr; 10x
Albedo
winter
5. 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%
Radiative Forcing
Thermohaline Circulatoin
Strong
Albedos of Snow and Ice
6. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Surface Mass Balance
Heat wave
Hydrological Drought
Open talik
7. Ocean retains ____ CO2
Hydrological Drought
7%
Once every 4 years.
25%
8. Amount of light absorbed by surface
Energy Budget
Average radiative flux reaching the atmosphere
50%
Antarctica
9. Laser radar - H V - Long time series - high accuracy - Density
50%
Agricultural Drought
Infrared radiation
Altimetry (height)
10. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Sunspots
Why the Arctic climate is special
Ice in the Arctic
Sublimation
11. Set up in 1988 by WMO and UNEP.
IPCC
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
70%
air can warm dramatically
12. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Ocean water
In the troposphere that we live in.
Strong
13. Warming- positive feedback - Cooling- negative feedback.
Why Water Vapor is not a climate forcing
Cause of break of inversion layers or decrease in frequency
Calving
Ice-Albedo
14. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Altimetry
Mass Balance
In the stratosphere.
Monthly maximums and minimums
15. 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.
Precipitation and High Latitudes
Surface Mass Balance
Reduction in sea-ice extent
Change in vegetation generates a further feedback
16. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
.75OC/km-1
Hydrological Drought
Monthly maximums and minimums
17. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
More rain means no drought
Where rise in OC is greatest
Is precipitation around the world increasing?
18. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Warming; cooling
Negative Ice-Albedo Feedback
Mass Budget
Sea ice melt does not change sea level
19. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
doubles
Longwave Radiation
Carbon Dioxide
Thermohaline Circulation Effect
20. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Through talik
Open talik
Surface Mass Balance
How to define a heatwave
21. Summer increase in cloud cover - Winter decrease in cloud cover.
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22. Cooler water and drought conditions.
La Nia
Affect Floods and Droughts
Questions to think about
Grounding v Surface Melting
23. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Why ice-albedo feedback is a big deal in the Arctic
Grounding v Surface Melting
Rainy
Ocean water
24. Amount of light absorbed by atmosphere
Discontinuous Permafrosrt
20%
The cryosphere
Methane
25. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Deep tropics between 15O N and 15 O S are quite
Affect Floods and Droughts
Active Layer
Thermokarst Lake
26. 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
Types of Albedo
Thickness of the active layer and the permafrost depend on this
Thermokarst
Altimetry Pros
27. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Atmospheric Composition
Ozone Hole
Strong
El Nino
28. Antarctica - stratosphere - Sep-Oct
Ozone Hole
Severe coastal erosion
Atmospheric Structure
7%
29. Land Based Ecosystems retain ____ CO2.
30%
Archimedes' Principle
Negative Ice-Albedo Feedback
Black Carbon
30. ~10% of incident solar energy (albedo 90)
Surface Mass Balance
Mass Balance
Negative
Ice absorbs
31. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Positive feedbacks both found in...
Ice Sheets
IPCC
32. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
Methane
GHG
What happens with the Ozone Hole
Ice Sheets
33. Clouds 40~90% - Vegetation 10~15%
Atmospheric Structure
Hydrological Drought
Types of Albedo
30%
34. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Atmospheric Structure
air can warm dramatically
Thermohaline Circulation
Archimedes' Principle
35. 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
doubles
Changes in Arctic sea-ice Extent
The cryosphere
Thermohaline Circulation Effect
36. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Ice in the Arctic
El Nino
reduction in sea-ice
Why the Arctic climate is special
37. Total absorbed solar radiation
Altimetry Pros
70%
Monthly maximums and minimums
Ocean water
38. In average: +1% in respect to 100 years ago.
Threshold departures
Ice Motion
Why ice-albedo feedback is a big deal in the Arctic
Is precipitation around the world increasing?
39. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Indirect heat wave effect
Sunspots
Albedos of Snow and Ice
Today melting ice
40. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Active Layer
Sublimation
Mass Balance
% of Greenhouse Gases
41. Volcanic eruptions - Sunspots - Wobbly Earth
Monthly maximums and minimums
Radiative Flux
Natural Causes of Warming
Questions to think about
42. US is responsible for ___ of the total CO2
30%
Mass Change
Albedos of Snow and Ice
Warm
43. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Black Carbon
Discontinuous
Grounding Lines
44. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
50%
Earth's tilt
Greenland
45. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
How the cryosphere is affected by climate change
Ice Shelf
Troposphere
reduction in sea-ice
46. x7 smaller - 7m total sea level equivalent.
Ice Cap
Precipitation and High Latitudes
Greenland
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
47. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Ice loss
Normal condition for air
Radiative Forcing
Ocean-Ice-Atmosphere Interaction
48. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Thermohaline Circulation
Archimedes' Principle
Active Layer
Negative
49. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Atmospheric Structure
In the Arctic where the air is cooler
30%
50. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
Cause of break of inversion layers or decrease in frequency
Altimetry Cons
Depth v Surface
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