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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. How often does El Nio occur?
Albedo
7%
Once every 4 years.
Strong
2. 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
Time Variable Gravity
doubles
Ozone Hole
El Nio is in the coasts of...
3. A thick - floating slab of freshwater ice extending from coast to coast.
Once every 4 years.
IPCC
Ice shelf
Radiative Flux
4. 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
Sublimation
What happens with the Ozone Hole
25%
Thermohaline Circulation
5. CO2 - CH4 - O3 - H2O - N2O - CFCs
The Ozone Hole
All Greenhouse gases
Meteorological Drought
How a closed talik forms
6. Clouds 40~90% - Vegetation 10~15%
Active Layer
50%
Types of Albedo
Once every 4 years.
7. 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.
Ice Cap
Thermohaline Circulatoin
Importance of ice sheets
Greenland
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
Mass Change
Meteorological Drought
Mass Budget
Very small portion
9. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Warming; cooling
Methane
Permafrost
Infrared radiation
10. The amount of light reflected by an object.
Absolute thresholds
Mass Budget
Albedo
Methane
11. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
In the Arctic where the air is cooler
Altimetry Cons
Open talik
winter
12. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
The Ozone Hole
Ice Motion
Radiative Flux
Surface Mass Balance
13. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Is precipitation around the world increasing?
Major distinction between Kyoto Protocol and Convention
Average radiative flux reaching the atmosphere
Thinner atmosphere
14. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Sunspots
Surface Mass Balance
Thermokarst
Why ice-albedo feedback is a big deal in the Arctic
15. Really measures volume.
Thinner atmosphere
Altimetry
1 m/yr; 10x
Changes in Arctic sea-ice Extent
16. Summer increase in cloud cover - Winter decrease in cloud cover.
17. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Grounding Lines
Atlantic Thermohaline Circulation
Altimetry
Ice Sheets
18. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Rainy
Thermokarst
Ice-Ocean Interactions
Increases - decreases
19. The Earth emits this.
Climate Change in the Arctic
Longwave Radiation
Ice Sheets
70%
20. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
21. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Through talik
Grounding Lines
In the Arctic where the air is cooler
22. Volcanic eruptions - Sunspots - Wobbly Earth
Warm
Thermohaline Circulation
Natural Causes of Warming
Nitrous Oxide (N2O)
23. Descending Air dry - Convection cells are wet.
Atmospheric Circulation
Permafrost
Negative Ice-Albedo Feedback
Antarctica
24. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Agricultural Drought
More rain means no drought
Global warming and hot nights?
Ice/snow
25. 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
IN the last 2 decades what we've seen
IPCC
Snow and snow covered ice absorb
26. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
How we measure Mass Balance
Heat Source and Pressure
What happens with the Ozone Hole
How to define a heatwave
27. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Ice Motion
Frozen Soil
Antarctica
Grounding Lines
28. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Strong
Snow and snow covered ice absorb
El Nio is in the coasts of...
Thickness of the active layer and the permafrost depend on this
29. Frozen +2 years - Few centimeters to 1500 m
Permafrost
air can warm dramatically
Ocean water
Climate Change in the Arctic
30. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Monthly maximums and minimums
Cloud Feedbacks
Archimedes' Principle
Stronger
31. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Melt
Mass Budget
Inversion Layer Winter
Black Carbon
32. 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.
Ocean water
75-OC
GHG
Greenhouse Gases
33. Land Based Ecosystems retain ____ CO2.
Open talik
Stronger
The Ozone Hole
30%
34. Amount of light absorbed by surface
50%
Major distinction between Kyoto Protocol and Convention
Antarctica
All Greenhouse gases
35. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
75-OC
Sea ice melt does not change sea level
Infrared radiation
Positive
36. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Accumulation
Stratospheric Ozone Depletion
Thermokarst
Methane
37. CO2 GHG forcing - H2O - dominant/major GHG
El Nio is in the coasts of...
Why ice-albedo feedback is a big deal in the Arctic
GHG
Frozen Soil
38. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Today melting ice
Altimetry Cons
Rainy
Methane
39. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Climate Change in the Arctic
Active Layer
Frozen Soil
Affect Floods and Droughts
40. Greenhouse gases are mixed in the ____
Snow and snow covered ice absorb
Natural Causes of Warming
Severe coastal erosion
Troposphere
41. Number of days that exceed a given temperature
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Absolute thresholds
Hydrological Drought
air can warm dramatically
42. The buoyant force is equal to the weight of the displaced water.
43. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
How to define a heatwave
More rain means no drought
Inversion Layer (feedback)
Ice-Albedo
44. Radiation absorbed by atmospheric greenhouse gases?
Frozen Soil
7%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Sunspots
45. 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
summer
Why the Arctic climate is special
Altimetry
Accumulation
46. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
In the troposphere that we live in.
Ocean water
Climate Change in the Arctic
47. 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
Permafrost Degradation
The cryosphere
Ice Sheets
GHG
48. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Mass Budget
Why ice-albedo feedback is a big deal in the Arctic
30%
49. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Ocean water
Positive feedbacks both found in...
Ice-Albedo
50. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Negative Ice-Albedo Feedback
Altimetry Cons
Thickness of the active layer and the permafrost depend on this
The cryosphere