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Test your basic knowledge |
Global Warming
Start Test
Study First
Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
50%
IN the last 2 decades what we've seen
Inversion Layer Winter
75-OC
2. The order of 1 m/year. Melting is ten times more.
Agricultural Drought
Ice Sheets
Surface Mass Balance
How a closed talik forms
3. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
US and precipitation
Black Carbon
Sunspots
Meteorological Drought
4. Clouds 40~90% - Vegetation 10~15%
winter
In the troposphere that we live in.
Average radiative flux reaching the atmosphere
Types of Albedo
5. 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
Ice-Ocean Interactions
Surface Mass Balance
Altimetry (height)
Why ice-albedo feedback is a big deal in the Arctic
6. Really measures volume.
Precipitation and High Latitudes
Contributions to CO2 from different activities
Altimetry
Antarctica
7. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Normal condition for air
50%
Monthly maximums and minimums
Positive
8. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Is precipitation around the world increasing?
Active Layer
Normal condition for air
Effect of Deforestation on CO-2
9. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Thermohaline Circulation
air can warm dramatically
Sea Ice
Stratospheric Ozone Depletion
10. 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
Depth v Surface
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Reduction in sea-ice extent
What effects the density
11. 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
What happens with the Ozone Hole
Heat Source and Pressure
Thermohaline Circulation
Ocean water
12. 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
How the cryosphere is affected by climate change
Mass Change
The Ozone Hole
Accumulation
13. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Grounding Lines
How a closed talik forms
Ice Sheets
Greenland
14. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Grounding Lines
Sea ice melt does not change sea level
Sublimation
Sea Ice
15. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
El Nino
Ice in the Arctic
Snow and snow covered ice absorb
16. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Amount of light actually reaching the Earth
Frozen Soil
Ice Sheets
Ozone
17. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Thinner atmosphere
Methane
Warming; cooling
Thermohaline Circulatoin
18. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
Methane
Atmospheric Circulation
Meteorological Drought
19. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Time Variable Gravity
Meteorological Drought
Questions to think about
Ice-Albedo
20. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
1 m/yr; 10x
Talik
Negative
In the Arctic where the air is cooler
21. Amount of light absorbed by surface
How to define a heatwave
50%
Changes in Arctic sea-ice Extent
Rainy
22. ~10% of incident solar energy (albedo 90)
Average radiative flux reaching the atmosphere
Ice absorbs
Thickness of the active layer and the permafrost depend on this
Depth v Surface
23. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
US and precipitation
How we measure Mass Balance
1 m/yr; 10x
Discontinuous
24. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Grounding Lines
air can warm dramatically
Atmospheric Composition
25. A thick - floating slab of freshwater ice extending from coast to coast.
Open talik
Percentile departures
Meteorological Drought
Ice shelf
26. 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.
Ice loss
GHG
Natural Causes of Warming
Atmospheric Structure
27. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Ice in the Arctic
Antarctica
Inversion Layer Summer
28. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Change in vegetation generates a further feedback
Greenland
Ice Discharge
Thermokarst Lake
29. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Energy Budget
Surface Mass Balance
How talik forms under lakes
Greenland
30. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Time Variable Gravity
Precipitation and High Latitudes
Ice Discharge
Negative
31. Laser radar - H V - Long time series - high accuracy - Density
Wetter; drier
Altimetry (height)
Inversion Layer Winter
More rain means no drought
32. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
Inversion Layer (feedback)
Ice loss
Thermokarst Lake
33. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
Shortwave Length
Ice Shelf
Air pollution
Thermohaline Circulation
34. 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
Mass Budget
Snow and snow covered ice absorb
Calving
Radiative Flux
35. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Some regions of the Earth have warmed faster than other regions.
45%
Dynamic thinning
Natural Causes of Warming
36. Frozen +2 years - Few centimeters to 1500 m
Importance of ice sheets
In the Arctic where the air is cooler
Radiative Forcing
Permafrost
37. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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38. 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
30%
Effect of Deforestation on CO-2
How talik forms under lakes
39. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
winter
Mass Change
Ice Discharge
40. How often does El Nio occur?
Once every 4 years.
Talik
Sea-Ice Albedo
Negative Ice-Albedo Feedback
41. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Permafrost Degradation
What happens with the Ozone Hole
Thermohaline Circulatoin
42. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Mass Change
In the stratosphere.
Talik
Radiative Forcing
43. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Through talik
Some parts of the planet are dry because of their location
Active Layer
Why the Arctic climate is special
44. 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.
Very small portion
Time Variable Gravity
Thermohaline Circulatoin
Discontinuous Permafrosrt
45. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Thermohaline Circulation Effect
Hydrological Drought
Ozone
Dry
46. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Rainy
Sunspots
Ice Discharge
IN the last 2 decades what we've seen
47. Number of days that exceed a given temperature
Absolute thresholds
Energy Budget
Thermokarst
Questions to think about
48. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Black Carbon
Altimetry Cons
Negative Ice-Albedo Feedback
Air pollution
49. High vs low
Contributions to CO2 from different activities
Antarctica
Cloud Feedbacks
Infrared radiation
50. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Absolute thresholds
Major distinction between Kyoto Protocol and Convention
Atmospheric Circulation
Accumulation
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