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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. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
50%
Depth v Surface
Monthly maximums and minimums
Active Layer
2. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Ice-Albedo
Arctic Atmosphere
Sublimation
Shortwave Length
3. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Arctic Atmosphere
Today melting ice
Ice Motion
4. Total absorbed solar radiation
70%
Ice-Albedo
Indirect heat wave effect
Thinner atmosphere
5. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
70%
How the cryosphere is affected by climate change
In the stratosphere.
6. 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.
Precipitation and High Latitudes
Thermohaline Circulatoin
Altimetry Pros
Today melting ice
7. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Atmospheric Structure
Inversion Layer Summer
Closed talik
8. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
.75OC/km-1
Mass Balance
GHG
doubles
9. Permafrost- A frozen soil
Thickness of the active layer and the permafrost depend on this
air can warm dramatically
Frozen Soil
45%
10. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Altimetry Cons
Ozone Hole
Discontinuous
Inversion Layer Summer
11. he increase of ozone concentration in the atmosphere helps ____ our planet
Shortwave Length
Heat Source and Pressure
Dry
Warm
12. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
winter
Radiative Forcing
Surface Mass Balance
Contributions to CO2 from different activities
13. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Infrared radiation
Radiative Forcing
Average radiative flux reaching the atmosphere
El Nino
14. 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.
Methane
Thermokarst
Sunspots
Ice loss
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
7%
Warming; cooling
Very small portion
16. 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
Threshold departures
Ozone Hole
Talik
17. 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
Mass Budget
Importance of ice sheets
Ozone
Contributions to CO2 from different activities
18. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Normal condition for air
In the Arctic where the air is cooler
IN the last 2 decades what we've seen
Calving
19. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
air can warm dramatically
IPCC
Greenland
20. 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.
In the Arctic where the air is cooler
Greenhouse Gases
Inversion Layer Winter
Absolute thresholds
21. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Open talik
Ice Motion
Normal condition for air
Active Layer
22. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
Layers of Earth
Why Water Vapor is not a climate forcing
Ocean water
23. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
Positive feedbacks both found in...
Rainy
What effects the density
24. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Atmospheric Composition?
Some parts of the planet are dry because of their location
Heat wave
Sunspots
25. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Permafrost Degradation
Grounding Lines
Thermohaline Circulation
Stratospheric Ozone Depletion
26. O Climate change in the Arctic is occurring now - Changes have been huge already
Ice-Albedo
Heat Source and Pressure
Today melting ice
Mass Balance
27. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Earth's tilt
Thermohaline Circulation
Open talik
28. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Amount of light actually reaching the Earth
Atmospheric Composition
Ice Sheets
Global warming and hot nights?
29. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Energy Budget
Changes in Arctic sea-ice Extent
Questions to think about
Infrared radiation
30. LW - SW - 55% absorbed by surface
Some parts of the planet are dry because of their location
Ice loss
Normal condition for air
Energy Budget
31. 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
Ozone Hole
doubles
Discontinuous Permafrosrt
Warm
32. Radiation absorbed by atmospheric greenhouse gases?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Greenhouse Gases
Thermokarst Lake
Inversion Layer Summer
33. 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
70%
Permafrost
Reduction in sea-ice extent
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
34. More common
Ocean water
Threshold departures
All Greenhouse gases
Inversion Layer Winter
35. The amount of light reflected by an object.
7%
Albedo
Ice Motion
reduction in sea-ice
36. Set up in 1988 by WMO and UNEP.
IPCC
Deep tropics between 15O N and 15 O S are quite
Altimetry Pros
Longwave Radiation
37. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Once every 4 years.
Why the Arctic climate is special
Permafrost Degradation
Greenland
38. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Albedos of Snow and Ice
Cloud Feedbacks
Thermohaline Circulation
39. 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.
El Nio is in the coasts of...
Ice-Ocean Interactions
Ocean-Ice-Atmosphere Interaction
Surface Mass Balance
40. High vs low
The Ozone Hole
Ice absorbs
Cloud Feedbacks
Black Carbon
41. 1.4 USA - 57 m total sea level equivalent
Why the Arctic climate is special
Antarctica
Discontinuous Permafrosrt
Mass Budget
42. CO2 - CH4 - O3 - H2O - N2O - CFCs
Why Water Vapor is not a climate forcing
Some regions of the Earth have warmed faster than other regions.
La Nia
All Greenhouse gases
43. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Warming; cooling
How we measure Mass Balance
reduction in sea-ice
44. Tundra absorbs more energy than ice and snow but less than scrubs and forest - and with those plants migrating towards the north - they will further contribute ot absorb more energy.
50%
Percentile departures
Change in vegetation generates a further feedback
Today melting ice
45. The past climate...for this reason - both keep good records of climate change.
Surface Mass Balance
Energy Budget
Contributions to CO2 from different activities
Thickness of the active layer and the permafrost depend on this
46. Melting Point decreases
All Greenhouse gases
Mass Change
.75OC/km-1
US and precipitation
47. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
What effects the density
Atmospheric Composition
Ice loss
Antarctica
48. 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
Ice Sheets
Altimetry Pros
El Nino
Some parts of the planet are dry because of their location
49. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
Closed talik
Ice in the Arctic
.7O Celsius over the past century.
How the cryosphere is affected by climate change
50. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Amount of light actually reaching the Earth
Discontinuous Permafrosrt
7%
Methane