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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. CO2 - CH4 - O3 - H2O - N2O - CFCs
Albedos of Snow and Ice
Sea Ice
All Greenhouse gases
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
2. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Discharge
Natural Causes of Warming
Permafrost
Ocean water
3. 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
Is precipitation around the world increasing?
Ice Motion
Importance of ice sheets
Where rise in OC is greatest
4. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Ice Cap
Why the Arctic climate is special
Active Layer
Air pollution
5. 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.
Dynamic thinning
Severe coastal erosion
Greenhouse Gases
Grounding Lines
6. Ice sheets have a very ____ Albedo
Earth's tilt
Strong
Contributions to CO2 from different activities
Black Carbon
7. Radiation absorbed by atmospheric greenhouse gases?
Active Layer
In the stratosphere.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice loss
8. Number of days that exceed a given temperature
7%
More rain means no drought
Absolute thresholds
Climate Change in the Arctic
9. Warming- positive feedback - Cooling- negative feedback.
Calving
Precipitation and High Latitudes
Grounding Lines
Ice-Albedo
10. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Ozone Hole
Wetter; drier
Antarctica
Thermokarst Lake
11. Permafrost- A frozen soil
winter
Sea Ice
Frozen Soil
Precipitation and High Latitudes
12. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Longwave Radiation
Surface Mass Balance
Questions to think about
Indirect heat wave effect
13. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Climate Change in the Arctic
Active Layer
Percentile departures
Atmospheric Circulation
14. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
Thermohaline Circulatoin
Arctic Atmosphere
GHG
Stratospheric Ozone Depletion
15. Set up in 1988 by WMO and UNEP.
More rain means no drought
Greenland
IPCC
Talik
16. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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17. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Snow and snow covered ice absorb
Antarctica
Albedos of Snow and Ice
Carbon Dioxide
18. 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.
Dry
Ice Sheets
Methane
Amount of light actually reaching the Earth
19. Greenhouse gases are a ___ portion of the atmosphere
Ocean-Ice-Atmosphere Interaction
Greenhouse Gases
Percentile departures
Very small portion
20. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Altimetry (height)
Dynamic thinning
Snow and snow covered ice absorb
Once every 4 years.
21. Summer increase in cloud cover - Winter decrease in cloud cover.
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22. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Thermokarst
Atmospheric Composition
Altimetry Cons
IPCC
23. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Ice in the Arctic
Surface Mass Balance
Longwave Radiation
Sublimation
24. Melting Point decreases
Greenland
Ice/snow
Altimetry
.75OC/km-1
25. 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.
Frozen Soil
Cloud Feedbacks
70%
Change in vegetation generates a further feedback
26. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Cloud Feedbacks
Thermokarst
GHG
How the cryosphere is affected by climate change
27. Number of days when temperatures climb above average by a fixed amount.
Ice absorbs
Where rise in OC is greatest
Threshold departures
Frozen Soil
28. 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
How talik forms under lakes
Warm
doubles
Troposphere
29. Industrial product - 300 ppb (parts per billion)
Ice in the Arctic
Positive feedbacks both found in...
Nitrous Oxide (N2O)
Methane
30. 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.
Ice Shelf
Some parts of the planet are dry because of their location
Carbon Dioxide
Thickness of the active layer and the permafrost depend on this
31. 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%
Earth's tilt
Albedos of Snow and Ice
Carbon Dioxide
Surface Mass Balance
32. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Melt
Atmospheric Composition?
US and precipitation
75-OC
33. 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
Importance of ice sheets
Strong
Air pollution
Ice Sheets
34. 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
Inversion Layer Summer
In the stratosphere.
Dry
Thinner atmosphere
35. 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
Ozone Hole
Why the Arctic climate is special
Accumulation
Percentile departures
36. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Thickness of the active layer and the permafrost depend on this
Ice-Ocean Interactions
Ocean water
37. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
.7O Celsius over the past century.
Ice Cap
Ice Motion
Positive feedbacks both found in...
38. 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
Sea ice melt does not change sea level
Energy Budget
GHG
39. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Ice loss
Thinner atmosphere
El Nio is in the coasts of...
Hydrological Drought
40. Over the Northern Hemisphere than the tropics.
Importance of ice sheets
Surface Mass Balance
Stratospheric Ozone Depletion
Where rise in OC is greatest
41. 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:
Inversion Layer (feedback)
Warm
Thermohaline Circulation
Troposphere
42. A thick - floating slab of freshwater ice extending from coast to coast.
Ocean water
Ice shelf
Mass Budget
Some regions of the Earth have warmed faster than other regions.
43. The amount of light reflected by an object.
Mass Change
How a closed talik forms
Meteorological Drought
Albedo
44. 10 : 1 - grounding ; surface
In the troposphere that we live in.
Ocean-Ice-Atmosphere Interaction
Grounding v Surface Melting
Normal condition for air
45. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Ocean-Ice-Atmosphere Interaction
How we measure Mass Balance
Accumulation
Ice Discharge
46. Cooler water and drought conditions.
Ice Sheets
La Nia
El Nio is in the coasts of...
Sea-Ice Albedo
47. 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
Atmospheric Composition
How the cryosphere is affected by climate change
Ice-Ocean Interactions
Ozone Hole
48. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Active Layer
Melt
Some parts of the planet are dry because of their location
Through talik
49. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
reduction in sea-ice
Positive feedbacks both found in...
Strong
Dynamic thinning
50. Frozen +2 years - Few centimeters to 1500 m
Ocean-Ice-Atmosphere Interaction
Accumulation
Nitrous Oxide (N2O)
Permafrost
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