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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. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Major distinction between Kyoto Protocol and Convention
50%
doubles
Active Layer
2. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Active Layer
Inversion Layer Summer
Antarctica
Ozone Hole
3. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
winter
Thermokarst
Ocean water
75-OC
4. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Altimetry Cons
Calving
Effect of Deforestation on CO-2
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
5. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Surface Mass Balance
1 m/yr; 10x
Open talik
Snow and snow covered ice absorb
6. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Energy Budget
Accumulation
Why ice-albedo feedback is a big deal in the Arctic
7. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Thermohaline Circulation
Sea Ice
Surface Mass Balance
Negative Ice-Albedo Feedback
8. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Methane
Open talik
Antarctica
9. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Cause of break of inversion layers or decrease in frequency
Atmospheric Composition?
Inversion Layer Summer
10. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Dry
Through talik
Ice Sheets
11. Total absorbed solar radiation
Antarctica
Nitrous Oxide (N2O)
20%
70%
12. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
In the troposphere that we live in.
Earth's tilt
Thermokarst Lake
Heat wave
13. 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
La Nia
What happens with the Ozone Hole
Some regions of the Earth have warmed faster than other regions.
Hydrological Drought
14. 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
Active Layer
Melt
doubles
The cryosphere
15. Atmospheric Cooling - Both negative (stabilizing) feedbacks - It is not happening now - but it has happened in the past - Ice-albedo feedback was the dominant feedback during the ice ages.
Thermokarst
How a closed talik forms
Negative Ice-Albedo Feedback
In the troposphere that we live in.
16. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Warm
Why the Arctic climate is special
The cryosphere
Deep tropics between 15O N and 15 O S are quite
17. 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
How the cryosphere is affected by climate change
reduction in sea-ice
Permafrost
Radiative Forcing
18. 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
Today melting ice
Ice Sheets
Thermokarst
Cause of break of inversion layers or decrease in frequency
19. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Carbon Dioxide
7%
Longwave Radiation
Ocean-Ice-Atmosphere Interaction
20. Rainy on yearly average. In these regions - rising air predominates.
Greenhouse Gases
Deep tropics between 15O N and 15 O S are quite
Contributions to CO2 from different activities
Once every 4 years.
21. LW - SW - 55% absorbed by surface
How talik forms under lakes
How we measure Mass Balance
In the stratosphere.
Energy Budget
22. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
1 m/yr; 10x
Reduction in sea-ice extent
winter
Atmospheric Composition
23. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Negative
Mass Budget
Grounding Lines
Dry
24. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Energy Budget
Snow and snow covered ice absorb
Mass Budget
25. In average: +1% in respect to 100 years ago.
Dry
Layers of Earth
Is precipitation around the world increasing?
Sublimation
26. 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
Importance of ice sheets
Where rise in OC is greatest
US and precipitation
20%
27. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Monthly maximums and minimums
El Nio is in the coasts of...
Thermohaline Circulation
IN the last 2 decades what we've seen
28. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Thermokarst Lake
Stronger
45%
29. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Severe coastal erosion
Layers of Earth
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Methane
30. Number of days when temperatures climb above average by a fixed amount.
IN the last 2 decades what we've seen
Open talik
Threshold departures
Earth's tilt
31. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Air pollution
Mass Balance
winter
Affect Floods and Droughts
32. Atmosphere retains ____ CO2
Why Water Vapor is not a climate forcing
What effects the density
45%
Infrared radiation
33. Clouds 40~90% - Vegetation 10~15%
Types of Albedo
Sea Ice Extent is Changing in Antarctica as well
Archimedes' Principle
Cause of break of inversion layers or decrease in frequency
34. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Open talik
Strong
Longwave Radiation
35. Amount of light absorbed by atmosphere
Inversion Layer (feedback)
Infrared radiation
Reduction in sea-ice extent
20%
36. CO2 - CH4 - O3 - H2O - N2O - CFCs
Deep tropics between 15O N and 15 O S are quite
Ice loss
Heat Source and Pressure
All Greenhouse gases
37. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Ice Shelf
Positive
Accumulation
Stratospheric Ozone Depletion
38. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Questions to think about
Atmospheric Composition
Black Carbon
Carbon Dioxide
39. Land Based Ecosystems retain ____ CO2.
Active Layer
30%
Ocean water
Frozen Soil
40. 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.
Natural Causes of Warming
Precipitation and High Latitudes
Ice Cap
Thermohaline Circulation Effect
41. The amount of light reflected by an object.
Nitrous Oxide (N2O)
Albedo
How the cryosphere is affected by climate change
Inversion Layer (feedback)
42. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
IPCC
Rainy
Threshold departures
Global warming and hot nights?
43. The Earth emits this.
Accumulation
Longwave Radiation
25%
Increases - decreases
44. Over the past century what has happened to the Earth's temperature?
Archimedes' Principle
Longwave Radiation
Negative
Some regions of the Earth have warmed faster than other regions.
45. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
Active Layer
Atmospheric Composition
Thinner atmosphere
How we measure Mass Balance
46. Reduction of snow and ice cover - Changes in atmospheric circulation.
How we measure Mass Balance
Wetter; drier
Cause of break of inversion layers or decrease in frequency
75-OC
47. 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
Heat Source and Pressure
Ozone
Global warming and hot nights?
Permafrost
48. 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
Very small portion
Mass Budget
Stratospheric Ozone Depletion
49. 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.
Normal condition for air
Troposphere
Ice Sheets
Ice Discharge
50. Radiation absorbed by atmospheric greenhouse gases?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Severe coastal erosion
Thermohaline Circulation
Active Layer