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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. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Ice loss
Depth v Surface
Thinner atmosphere
2. High cloud has a _____ effect and cool cloud has a ____ effect
Rainy
Warming; cooling
Troposphere
IPCC
3. O Climate change in the Arctic is occurring now - Changes have been huge already
Layers of Earth
Affect Floods and Droughts
Today melting ice
Atmospheric Circulation
4. 1.4 USA - 57 m total sea level equivalent
50%
Sea-Ice Albedo
Antarctica
Stronger
5. Land Based Ecosystems retain ____ CO2.
Ice Shelf
Discontinuous
30%
Rainy
6. Descending Air dry - Convection cells are wet.
Sea Ice Extent is Changing in Antarctica as well
Atmospheric Circulation
Thermokarst Lake
45%
7. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
How we measure Mass Balance
Reduction in sea-ice extent
Contributions to CO2 from different activities
8. 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.
All Greenhouse gases
Ice-Ocean Interactions
Why ice-albedo feedback is a big deal in the Arctic
Importance of ice sheets
9. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Ice Sheets
The cryosphere
Effect of Deforestation on CO-2
Time Variable Gravity
10. 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
In the Arctic where the air is cooler
Why the Arctic climate is special
Ice shelf
Thermokarst
11. 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
Heat wave
Ocean water
Dry
The Ozone Hole
12. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Greenhouse Gases
Sea-Ice Albedo
Percentile departures
13. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Mass Change
Altimetry Pros
Thermohaline Circulation Effect
Thermokarst
14. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Through talik
Thickness of the active layer and the permafrost depend on this
Climate Change in the Arctic
15. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
% of Greenhouse Gases
75-OC
Greenhouse Gases
Changes in Arctic sea-ice Extent
16. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Longwave Radiation
Ice Shelf
Atmospheric Composition?
All Greenhouse gases
17. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Sea Ice
Hydrological Drought
Cloud Feedbacks
Arctic Atmosphere
18. 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%
Increases - decreases
Albedos of Snow and Ice
Ozone Hole
Surface Mass Balance
19. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Indirect heat wave effect
El Nio is in the coasts of...
Ice Discharge
La Nia
20. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Air pollution
How a closed talik forms
What effects the density
Hydrological Drought
21. Measures input and output.
Ozone Hole
Thermokarst
Melt
Mass Budget
22. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
30%
The cryosphere
Surface Mass Balance
doubles
23. CO2 - CH4 - O3 - H2O - N2O - CFCs
Active Layer
Ice Cap
All Greenhouse gases
75-OC
24. Set up in 1988 by WMO and UNEP.
Ozone
How a closed talik forms
IPCC
7%
25. he increase of ozone concentration in the atmosphere helps ____ our planet
30%
Some parts of the planet are dry because of their location
How we measure Mass Balance
Warm
26. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Melt
70%
Positive
7%
27. How often does El Nio occur?
Thermohaline Circulation Effect
Active Layer
Once every 4 years.
45%
28. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Discontinuous Permafrosrt
Meteorological Drought
Thermohaline Circulation
Discontinuous
29. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Depth v Surface
Agricultural Drought
How to define a heatwave
Atmospheric Circulation
30. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Nitrous Oxide (N2O)
45%
Average radiative flux reaching the atmosphere
31. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Frozen Soil
Discontinuous Permafrosrt
In the Arctic where the air is cooler
32. 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
7%
Wetter; drier
Surface Mass Balance
Thermohaline Circulation
33. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
IPCC
Altimetry Cons
Thermohaline Circulation
34. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Cloud Feedbacks
Monthly maximums and minimums
Nitrous Oxide (N2O)
35. 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
Wetter; drier
In the Arctic where the air is cooler
Thermokarst
Natural Causes of Warming
36. Precipitation intensity will rise ___ for every 1 OC of warming.
Some regions of the Earth have warmed faster than other regions.
7%
Sea Ice Extent is Changing in Antarctica as well
Permafrost Degradation
37. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
25%
Ozone Hole
.75OC/km-1
38. 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
Agricultural Drought
Cloud Feedbacks
What effects the density
Permafrost
39. Extent 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.
reduction in sea-ice
75-OC
Natural Causes of Warming
50%
40. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Why Water Vapor is not a climate forcing
Atlantic Thermohaline Circulation
Why the Arctic climate is special
Surface Mass Balance
41. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Inversion Layer (feedback)
Grounding Lines
Time Variable Gravity
42. 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.
Thermokarst
Albedos of Snow and Ice
Natural Causes of Warming
Greenhouse Gases
43. Permafrost- A frozen soil
30%
Questions to think about
Mass Budget
Frozen Soil
44. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Carbon Dioxide
Active Layer
45%
Greenland
45. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
El Nio is in the coasts of...
Sublimation
Time Variable Gravity
Warm
46. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Monthly maximums and minimums
Ice in the Arctic
Cloud Feedbacks
Absolute thresholds
47. 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.
Some parts of the planet are dry because of their location
Ice Sheets
Indirect heat wave effect
Archimedes' Principle
48. 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
Surface Mass Balance
Ice Sheets
Sea Ice
Wetter; drier
49. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
The cryosphere
Permafrost
Arctic Atmosphere
50. 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.
Importance of ice sheets
In the troposphere that we live in.
More rain means no drought
Ice Shelf