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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. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Radiative Forcing
Warm
Altimetry Cons
Sea Ice
2. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
GHG
Through talik
Precipitation and High Latitudes
Once every 4 years.
3. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Is precipitation around the world increasing?
Talik
Air pollution
Amount of light actually reaching the Earth
4. O Climate change in the Arctic is occurring now - Changes have been huge already
Thermohaline Circulation Effect
Radiative Flux
Surface Mass Balance
Today melting ice
5. 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
Ice-Ocean Interactions
Agricultural Drought
Ocean-Ice-Atmosphere Interaction
6. Reduction of Summer Sea- 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 - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Normal condition for air
Reduction in sea-ice extent
Meteorological Drought
Shortwave Length
7. 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:
Thermohaline Circulation
Altimetry Cons
How a closed talik forms
Methane
8. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Thermohaline Circulation
Through talik
Ocean water
IN the last 2 decades what we've seen
9. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Cause of break of inversion layers or decrease in frequency
Ocean-Ice-Atmosphere Interaction
Sunspots
How we measure Mass Balance
10. 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
Ozone Hole
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
The cryosphere
How the cryosphere is affected by climate change
11. Number of days that land among the hottest of all days in that month's long-term record.
Mass Change
Percentile departures
Positive feedbacks both found in...
Albedo
12. The buoyant force is equal to the weight of the displaced water.
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13. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Once every 4 years.
Positive
Why Water Vapor is not a climate forcing
Greenland
14. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
air can warm dramatically
Active Layer
The Ozone Hole
All Greenhouse gases
15. 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
Thinner atmosphere
Ice Sheets
Active Layer
30%
16. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Increases - decreases
Types of Albedo
Contributions to CO2 from different activities
Positive feedbacks both found in...
17. x7 smaller - 7m total sea level equivalent.
Greenland
Thermohaline Circulation
Stratospheric Ozone Depletion
Ice Sheets
18. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Global warming and hot nights?
Archimedes' Principle
Carbon Dioxide
Increases - decreases
19. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
winter
Average radiative flux reaching the atmosphere
Meteorological Drought
30%
20. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Ice absorbs
Surface Mass Balance
Monthly maximums and minimums
21. Radiation absorbed by atmospheric greenhouse gases?
.75OC/km-1
Radiative Flux
Ice in the Arctic
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
22. 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.
Change in vegetation generates a further feedback
Thermokarst
Greenland
Snow and snow covered ice absorb
23. 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
Very small portion
Why Water Vapor is not a climate forcing
In the Arctic where the air is cooler
Warming; cooling
24. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Ice/snow
Thermokarst
Open talik
75-OC
25. Is not an externally imposed perturbation to the climate system.
Absolute thresholds
Why Water Vapor is not a climate forcing
Severe coastal erosion
Heat Source and Pressure
26. LW - SW - 55% absorbed by surface
In the stratosphere.
Black Carbon
Energy Budget
Hydrological Drought
27. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Positive feedbacks both found in...
Ice in the Arctic
Active Layer
Rainy
28. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
How to define a heatwave
All Greenhouse gases
Average radiative flux reaching the atmosphere
29. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Hydrological Drought
What effects the density
Radiative Flux
30. The past climate...for this reason - both keep good records of climate change.
Permafrost Degradation
In the stratosphere.
Thickness of the active layer and the permafrost depend on this
El Nio is in the coasts of...
31. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Normal condition for air
Ocean-Ice-Atmosphere Interaction
Permafrost Degradation
Archimedes' Principle
32. Precipitation intensity will rise ___ for every 1 OC of warming.
Thermokarst Lake
Surface Mass Balance
7%
Energy Budget
33. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
What effects the density
Atmospheric Circulation
Frozen Soil
34. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Today melting ice
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Discontinuous Permafrosrt
Thermokarst Lake
35. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Discontinuous
Through talik
Ice Shelf
75-OC
36. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Warm
reduction in sea-ice
Monthly maximums and minimums
Positive
37. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Earth's tilt
Grounding Lines
Greenhouse Gases
Ocean water
38. Atmosphere retains ____ CO2
Atmospheric Circulation
45%
50%
Surface Mass Balance
39. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Climate Change in the Arctic
Negative Ice-Albedo Feedback
Some regions of the Earth have warmed faster than other regions.
% of Greenhouse Gases
40. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
Thermokarst Lake
Atmospheric Structure
Precipitation and High Latitudes
41. CO2 GHG forcing - H2O - dominant/major GHG
Major distinction between Kyoto Protocol and Convention
Sea-Ice Albedo
30%
GHG
42. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Positive feedbacks both found in...
Ice Cap
Ice Motion
Sea ice melt does not change sea level
43. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Natural Causes of Warming
Absolute thresholds
Ice Motion
44. Melting Point decreases
Ozone Hole
Mass Budget
Thermokarst
.75OC/km-1
45. How much is the planet really warming?
.7O Celsius over the past century.
Earth's tilt
Infrared radiation
Thinner atmosphere
46. Frozen +2 years - Few centimeters to 1500 m
Methane
Precipitation and High Latitudes
Wetter; drier
Permafrost
47. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Wetter; drier
Positive
Deep tropics between 15O N and 15 O S are quite
Atmospheric Structure
48. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
GHG
Monthly maximums and minimums
Ice Discharge
Ozone Hole
49. 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
Meteorological Drought
Mass Change
Affect Floods and Droughts
doubles
50. Total absorbed solar radiation
Severe coastal erosion
Stronger
70%
Thermokarst