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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. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Absolute thresholds
Surface Mass Balance
Grounding v Surface Melting
2. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Archimedes' Principle
Ozone
Mass Change
3. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Dry
Mass Balance
Major distinction between Kyoto Protocol and Convention
50%
4. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
The Ozone Hole
Dynamic thinning
reduction in sea-ice
All Greenhouse gases
5. 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
More rain means no drought
Amount of light actually reaching the Earth
Ice loss
Why the Arctic climate is special
6. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Why Water Vapor is not a climate forcing
Thermohaline Circulation
doubles
Surface Mass Balance
7. How much is the planet really warming?
Ice Cap
Thermohaline Circulation
Monthly maximums and minimums
.7O Celsius over the past century.
8. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Snow and snow covered ice absorb
Talik
Ocean water
Effect of Deforestation on CO-2
9. 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
75-OC
Open talik
El Nino
Indirect heat wave effect
10. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Ozone Hole
Where rise in OC is greatest
Sea Ice Extent is Changing in Antarctica as well
Earth's tilt
11. How often does El Nio occur?
The Ozone Hole
Ozone
Once every 4 years.
More rain means no drought
12. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Contributions to CO2 from different activities
Methane
Ice shelf
The cryosphere
13. High vs low
Cloud Feedbacks
Layers of Earth
Sea Ice
Surface Mass Balance
14. Longwave radiation - any radiation with a long wave will heat up quickly.
Greenhouse Gases
Infrared radiation
Severe coastal erosion
Ice absorbs
15. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Ozone
Thermohaline Circulation
Depth v Surface
Grounding Lines
16. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Antarctica
La Nia
Thinner atmosphere
Calving
17. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Methane
Effect of Deforestation on CO-2
Greenland
Meteorological Drought
18. LW - SW - 55% absorbed by surface
Indirect heat wave effect
Altimetry
Energy Budget
Altimetry (height)
19. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Permafrost Degradation
Inversion Layer Winter
Severe coastal erosion
20. 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
Ice loss
75-OC
Atmospheric Structure
Dry
21. 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
Nitrous Oxide (N2O)
Ocean water
Thermohaline Circulation
IN the last 2 decades what we've seen
22. 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
Is precipitation around the world increasing?
Ice Sheets
Ice-Ocean Interactions
Atlantic Thermohaline Circulation
23. 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
Mass Change
Radiative Forcing
Reduction in sea-ice extent
24. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Deep tropics between 15O N and 15 O S are quite
Thermokarst
Nitrous Oxide (N2O)
Sunspots
25. Set up in 1988 by WMO and UNEP.
Depth v Surface
IPCC
Ice Discharge
Frozen Soil
26. 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
Why Water Vapor is not a climate forcing
How talik forms under lakes
Ocean-Ice-Atmosphere Interaction
27. A thick - floating slab of freshwater ice extending from coast to coast.
Surface Mass Balance
How a closed talik forms
In the troposphere that we live in.
Ice shelf
28. More common
Why Water Vapor is not a climate forcing
Permafrost Degradation
Inversion Layer Winter
Altimetry Cons
29. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Strong
Black Carbon
Very small portion
Thermokarst
30. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Closed talik
Is precipitation around the world increasing?
How we measure Mass Balance
Grounding Lines
31. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
El Nio is in the coasts of...
Atmospheric Structure
Stronger
Infrared radiation
32. CO2 GHG forcing - H2O - dominant/major GHG
The cryosphere
Antarctica
GHG
Global warming and hot nights?
33. Rainy on yearly average. In these regions - rising air predominates.
Deep tropics between 15O N and 15 O S are quite
Atmospheric Composition?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Melt
34. Permafrost- A frozen soil
Frozen Soil
Nitrous Oxide (N2O)
summer
Grounding v Surface Melting
35. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Indirect heat wave effect
Monthly maximums and minimums
Carbon Dioxide
36. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Where rise in OC is greatest
Ice-Ocean Interactions
Active Layer
How talik forms under lakes
37. Like weighing oneself on the scale.
Frozen Soil
Surface Mass Balance
Time Variable Gravity
Mass Budget
38. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Major distinction between Kyoto Protocol and Convention
Precipitation and High Latitudes
IPCC
Contributions to CO2 from different activities
39. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
20%
Effect of Deforestation on CO-2
Monthly maximums and minimums
40. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Ice Shelf
.75OC/km-1
How talik forms under lakes
Severe coastal erosion
41. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Active Layer
Ice loss
Ice Discharge
The Ozone Hole
42. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
Greenhouse Gases
Normal condition for air
Open talik
Ice Sheets
43. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
GHG
US and precipitation
Thermohaline Circulation Effect
44. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Contributions to CO2 from different activities
Atmospheric Structure
Wetter; drier
30%
45. Industrial product - 300 ppb (parts per billion)
.75OC/km-1
Earth's tilt
Dry
Nitrous Oxide (N2O)
46. Less frequent and weaker
Inversion Layer Summer
Shortwave Length
Active Layer
Calving
47. In _______ - the inversions are less frequent and weaker in the Arctic.
Negative Ice-Albedo Feedback
Ice Cap
Troposphere
summer
48. Where does the ozone protect us?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Surface Mass Balance
In the stratosphere.
Positive
49. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
7%
IN the last 2 decades what we've seen
Once every 4 years.
50. 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
Dry
30%
Sea ice melt does not change sea level