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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. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Hydrological Drought
Amount of light actually reaching the Earth
Why Water Vapor is not a climate forcing
Altimetry Pros
2. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
1 m/yr; 10x
Inversion Layer (feedback)
Depth v Surface
3. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Sea ice melt does not change sea level
Energy Budget
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
What effects the density
4. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Thinner atmosphere
Mass Change
Active Layer
Discontinuous Permafrosrt
5. x7 smaller - 7m total sea level equivalent.
Greenland
Ice in the Arctic
IN the last 2 decades what we've seen
Contributions to CO2 from different activities
6. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Atmospheric Composition?
1 m/yr; 10x
Atlantic Thermohaline Circulation
Altimetry Cons
7. The amount of light reflected by an object.
summer
Why Water Vapor is not a climate forcing
Albedo
Severe coastal erosion
8. ~10% of incident solar energy (albedo 90)
Earth's tilt
Ice absorbs
Atlantic Thermohaline Circulation
How to define a heatwave
9. 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
In the Arctic where the air is cooler
30%
Ocean water
summer
10. 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
Radiative Forcing
Wetter; drier
Snow and snow covered ice absorb
11. How often does El Nio occur?
Mass Balance
Ice in the Arctic
Thermokarst
Once every 4 years.
12. O Climate change in the Arctic is occurring now - Changes have been huge already
% of Greenhouse Gases
Mass Change
Today melting ice
Cause of break of inversion layers or decrease in frequency
13. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Surface Mass Balance
Ice Shelf
Hydrological Drought
14. Over the Northern Hemisphere than the tropics.
In the troposphere that we live in.
Grounding Lines
Where rise in OC is greatest
Surface Mass Balance
15. High cloud has a _____ effect and cool cloud has a ____ effect
Snow and snow covered ice absorb
Air pollution
7%
Warming; cooling
16. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Agricultural Drought
Atlantic Thermohaline Circulation
Grounding Lines
Sea ice melt does not change sea level
17. 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
Sublimation
Indirect heat wave effect
Closed talik
18. Water vapor means more water up in the clouds and less in the ground!
Change in vegetation generates a further feedback
More rain means no drought
Warm
Atmospheric Composition
19. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Thermokarst Lake
Surface Mass Balance
Inversion Layer (feedback)
75-OC
20. 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.
Shortwave Length
Atlantic Thermohaline Circulation
Altimetry (height)
Negative Ice-Albedo Feedback
21. Forms in a mosaic of favoured locations.
Ocean-Ice-Atmosphere Interaction
Sea-Ice Albedo
Discontinuous Permafrosrt
Negative Ice-Albedo Feedback
22. 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
doubles
Sea ice melt does not change sea level
Inversion Layer Summer
Once every 4 years.
23. 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.
Thermohaline Circulation Effect
Longwave Radiation
Positive feedbacks both found in...
75-OC
24. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Inversion Layer Summer
Sea Ice Extent is Changing in Antarctica as well
Mass Budget
Thermokarst
25. 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%
Ocean-Ice-Atmosphere Interaction
Albedos of Snow and Ice
Ice Sheets
El Nio is in the coasts of...
26. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Sea-Ice Albedo
Ice Discharge
Change in vegetation generates a further feedback
Ice/snow
27. ~15% of incident solar energy (albedo 85)
Ozone Hole
Snow and snow covered ice absorb
Positive feedbacks both found in...
Threshold departures
28. Where do greenhouse gases warm up the Earth?
Albedo
Threshold departures
Effect of Deforestation on CO-2
In the troposphere that we live in.
29. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Archimedes' Principle
Stratospheric Ozone Depletion
Some regions of the Earth have warmed faster than other regions.
30. Melting Point decreases
.75OC/km-1
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Affect Floods and Droughts
Layers of Earth
31. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Mass Budget
What effects the density
How we measure Mass Balance
Grounding v Surface Melting
32. The past climate...for this reason - both keep good records of climate change.
Agricultural Drought
Time Variable Gravity
Thickness of the active layer and the permafrost depend on this
Surface Mass Balance
33. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Types of Albedo
Sea-Ice Albedo
Surface Mass Balance
1 m/yr; 10x
34. 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
How we measure Mass Balance
El Nino
Major distinction between Kyoto Protocol and Convention
Some parts of the planet are dry because of their location
35. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Once every 4 years.
Atmospheric Structure
Global warming and hot nights?
Natural Causes of Warming
36. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Greenland
Very small portion
GHG
37. 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
More rain means no drought
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Through talik
38. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Inversion Layer (feedback)
Carbon Dioxide
The cryosphere
39. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Radiative Forcing
Deep tropics between 15O N and 15 O S are quite
Open talik
Ice Motion
40. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
El Nino
In the Arctic where the air is cooler
Atmospheric Composition?
41. The buoyant force is equal to the weight of the displaced water.
42. 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
Major distinction between Kyoto Protocol and Convention
Talik
.7O Celsius over the past century.
Dry
43. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Permafrost Degradation
Dry
Methane
Rainy
44. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
How talik forms under lakes
45%
Snow and snow covered ice absorb
45. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Some parts of the planet are dry because of their location
Sea-Ice Albedo
doubles
46. Set up in 1988 by WMO and UNEP.
Permafrost Degradation
IPCC
Permafrost
Atmospheric Circulation
47. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
1 m/yr; 10x
Greenhouse Gases
Cause of break of inversion layers or decrease in frequency
48. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Altimetry (height)
Climate Change in the Arctic
Average radiative flux reaching the atmosphere
El Nio is in the coasts of...
49. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Permafrost Degradation
1 m/yr; 10x
Effect of Deforestation on CO-2
What happens with the Ozone Hole
50. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Albedos of Snow and Ice
70%
Average radiative flux reaching the atmosphere
Mass Balance