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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. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
What effects the density
Greenhouse Gases
Questions to think about
Atlantic Thermohaline Circulation
2. Unfrozen ground that is found within a mass of permafrost
Monthly maximums and minimums
All Greenhouse gases
Positive feedbacks both found in...
Closed talik
3. 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
Frozen Soil
Surface Mass Balance
Accumulation
What happens with the Ozone Hole
4. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
IN the last 2 decades what we've seen
Severe coastal erosion
In the stratosphere.
5. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
In the stratosphere.
Percentile departures
Negative
6. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Surface Mass Balance
Mass Balance
Change in vegetation generates a further feedback
7. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
How a closed talik forms
Climate Change in the Arctic
Active Layer
El Nio is in the coasts of...
8. 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
Average radiative flux reaching the atmosphere
Mass Balance
Mass Change
Is precipitation around the world increasing?
9. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
All Greenhouse gases
Negative
Sea ice melt does not change sea level
Positive feedbacks both found in...
10. 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
Global warming and hot nights?
Time Variable Gravity
Permafrost
Stronger
11. How much is the planet really warming?
25%
Ice-Albedo
.7O Celsius over the past century.
Inversion Layer Summer
12. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
winter
Today melting ice
How a closed talik forms
13. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Thinner atmosphere
Atlantic Thermohaline Circulation
Effect of Deforestation on CO-2
In the troposphere that we live in.
14. 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
Archimedes' Principle
El Nino
Reduction in sea-ice extent
Percentile departures
15. Industrial product - 300 ppb (parts per billion)
Thermokarst Lake
Time Variable Gravity
Sunspots
Nitrous Oxide (N2O)
16. US is responsible for ___ of the total CO2
What happens with the Ozone Hole
winter
30%
Why Water Vapor is not a climate forcing
17. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Methane
Shortwave Length
Altimetry Cons
Atmospheric Composition
18. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Sunspots
Ice Sheets
Dynamic thinning
Average radiative flux reaching the atmosphere
19. ~15% of incident solar energy (albedo 85)
Average radiative flux reaching the atmosphere
winter
Heat Source and Pressure
Snow and snow covered ice absorb
20. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
winter
Effect of Deforestation on CO-2
Active Layer
50%
21. The order of 1 m/year. Melting is ten times more.
Ice loss
Indirect heat wave effect
Cause of break of inversion layers or decrease in frequency
Surface Mass Balance
22. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Change in vegetation generates a further feedback
Ice loss
Air pollution
La Nia
23. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
Warming; cooling
Methane
Sea-Ice Albedo
24. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Why ice-albedo feedback is a big deal in the Arctic
Arctic Atmosphere
Some parts of the planet are dry because of their location
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
25. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Changes in Arctic sea-ice Extent
Methane
All Greenhouse gases
Albedos of Snow and Ice
26. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Methane
Altimetry (height)
summer
Surface Mass Balance
27. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Permafrost
Positive feedbacks both found in...
Changes in Arctic sea-ice Extent
Major distinction between Kyoto Protocol and Convention
28. Over the past century what has happened to the Earth's temperature?
El Nio is in the coasts of...
Negative
Some regions of the Earth have warmed faster than other regions.
Some parts of the planet are dry because of their location
29. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Permafrost Degradation
Time Variable Gravity
Discontinuous Permafrosrt
Dynamic thinning
30. In _______ - the inversions are less frequent and weaker in the Arctic.
30%
Stronger
summer
Cause of break of inversion layers or decrease in frequency
31. 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
El Nino
Ocean-Ice-Atmosphere Interaction
In the Arctic where the air is cooler
Calving
32. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Average radiative flux reaching the atmosphere
Atlantic Thermohaline Circulation
winter
33. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
How talik forms under lakes
Calving
Antarctica
34. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Heat Source and Pressure
How we measure Mass Balance
Warm
35. Where do greenhouse gases warm up the Earth?
Average radiative flux reaching the atmosphere
Some parts of the planet are dry because of their location
In the troposphere that we live in.
El Nino
36. 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
Accumulation
doubles
Ozone Hole
37. A dome shaped cover of perennial ice and snow.
Archimedes' Principle
Surface Mass Balance
Snow and snow covered ice absorb
Ice Cap
38. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Normal condition for air
In the Arctic where the air is cooler
Ocean-Ice-Atmosphere Interaction
El Nino
39. The amount of light reflected by an object.
Albedo
Affect Floods and Droughts
Change in vegetation generates a further feedback
Arctic Atmosphere
40. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Greenland
% of Greenhouse Gases
Monthly maximums and minimums
Thinner atmosphere
41. Amount of light absorbed by surface
50%
Archimedes' Principle
Heat Source and Pressure
Permafrost
42. 85%
Cause of break of inversion layers or decrease in frequency
IN the last 2 decades what we've seen
Major distinction between Kyoto Protocol and Convention
Sea-Ice Albedo
43. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Inversion Layer (feedback)
Atmospheric Composition
Permafrost Degradation
Ozone Hole
44. Total absorbed solar radiation
Inversion Layer Winter
70%
Reduction in sea-ice extent
Thermohaline Circulation Effect
45. Radiation absorbed by atmospheric greenhouse gases?
Meteorological Drought
Thickness of the active layer and the permafrost depend on this
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice shelf
46. 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%
25%
Depth v Surface
Albedos of Snow and Ice
Thermohaline Circulation
47. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Ocean water
Radiative Flux
Ice loss
Sea-Ice Albedo
48. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Mass Change
Grounding Lines
The cryosphere
Climate Change in the Arctic
49. Measures input and output.
75-OC
Mass Budget
Albedo
Ocean-Ice-Atmosphere Interaction
50. 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
Infrared radiation
70%
Ice Sheets
Carbon Dioxide