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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. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Ocean water
Indirect heat wave effect
75-OC
Thermokarst
2. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
What effects the density
Dry
Stratospheric Ozone Depletion
Why Water Vapor is not a climate forcing
3. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
air can warm dramatically
Negative
Contributions to CO2 from different activities
Albedos of Snow and Ice
4. 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.
Thermokarst Lake
Ocean water
Negative Ice-Albedo Feedback
Increases - decreases
5. 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
air can warm dramatically
Ozone Hole
Thermokarst Lake
El Nino
6. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ice loss
Ocean water
75-OC
Ozone Hole
7. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
Contributions to CO2 from different activities
Today melting ice
Archimedes' Principle
8. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sublimation
Calving
Ice Sheets
Snow and snow covered ice absorb
9. 85%
Carbon Dioxide
Sea-Ice Albedo
Thinner atmosphere
Why Water Vapor is not a climate forcing
10. Laser radar - H V - Long time series - high accuracy - Density
Importance of ice sheets
Very small portion
Why ice-albedo feedback is a big deal in the Arctic
Altimetry (height)
11. 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
Time Variable Gravity
Longwave Radiation
Inversion Layer Summer
Wetter; drier
12. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Surface Mass Balance
Ice Shelf
Heat Source and Pressure
Questions to think about
13. Clouds 40~90% - Vegetation 10~15%
Strong
Mass Budget
Types of Albedo
Stronger
14. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
How we measure Mass Balance
Earth's tilt
45%
15. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Questions to think about
Longwave Radiation
Changes in Arctic sea-ice Extent
Heat Source and Pressure
16. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Greenland
Albedos of Snow and Ice
Mass Balance
Is precipitation around the world increasing?
17. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
El Nino
Wetter; drier
Grounding v Surface Melting
Depth v Surface
18. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Effect of Deforestation on CO-2
Ice in the Arctic
Absolute thresholds
19. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice in the Arctic
The Ozone Hole
Discontinuous
20. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Antarctica
Ocean water
Earth's tilt
Once every 4 years.
21. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
How a closed talik forms
Surface Mass Balance
Monthly maximums and minimums
Closed talik
22. Less frequent and weaker
Climate Change in the Arctic
Dynamic thinning
Inversion Layer Summer
Very small portion
23. ~15% of incident solar energy (albedo 85)
Permafrost Degradation
El Nino
Snow and snow covered ice absorb
Average radiative flux reaching the atmosphere
24. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Altimetry Pros
Air pollution
Permafrost Degradation
Albedos of Snow and Ice
25. 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
Greenland
Wetter; drier
The cryosphere
26. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Normal condition for air
winter
Inversion Layer (feedback)
Thickness of the active layer and the permafrost depend on this
27. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Grounding Lines
Affect Floods and Droughts
Snow and snow covered ice absorb
28. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
.75OC/km-1
Cloud Feedbacks
Ice loss
29. 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
Radiative Flux
Types of Albedo
How we measure Mass Balance
Absolute thresholds
30. Set up in 1988 by WMO and UNEP.
The Ozone Hole
Grounding Lines
IPCC
Changes in Arctic sea-ice Extent
31. 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
Air pollution
Sea-Ice Albedo
Thinner atmosphere
Importance of ice sheets
32. Water vapor means more water up in the clouds and less in the ground!
Importance of ice sheets
Ice Sheets
More rain means no drought
Earth's tilt
33. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
US and precipitation
70%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Positive feedbacks both found in...
34. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
Active Layer
Climate Change in the Arctic
What happens with the Ozone Hole
Ice/snow
35. 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.
Today melting ice
Rainy
Inversion Layer Winter
Changes in Arctic sea-ice Extent
36. Forms in a mosaic of favoured locations.
25%
Frozen Soil
Discontinuous Permafrosrt
Inversion Layer Summer
37. Ice sheets have a very ____ Albedo
Thermohaline Circulation
1 m/yr; 10x
Strong
75-OC
38. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Is precipitation around the world increasing?
Thermokarst Lake
Reduction in sea-ice extent
How we measure Mass Balance
39. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Sea ice melt does not change sea level
Through talik
Thermohaline Circulation
Ocean-Ice-Atmosphere Interaction
40. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Snow and snow covered ice absorb
How the cryosphere is affected by climate change
Normal condition for air
41. Amount of light absorbed by surface
Carbon Dioxide
50%
Cloud Feedbacks
El Nino
42. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
In the stratosphere.
Meteorological Drought
Thermohaline Circulation Effect
Hydrological Drought
43. O Climate change in the Arctic is occurring now - Changes have been huge already
Thermohaline Circulatoin
Discontinuous Permafrosrt
Today melting ice
Methane
44. Number of days that exceed a given temperature
Average radiative flux reaching the atmosphere
Albedos of Snow and Ice
Threshold departures
Absolute thresholds
45. 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
20%
Ice loss
Ice in the Arctic
46. 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.
Ice-Ocean Interactions
Ice Motion
The cryosphere
reduction in sea-ice
47. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
How we measure Mass Balance
Black Carbon
IN the last 2 decades what we've seen
Negative Ice-Albedo Feedback
48. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Positive feedbacks both found in...
Warm
Thermohaline Circulation
49. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Ozone
% of Greenhouse Gases
Methane
Ice Cap
50. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
GHG
Thermokarst
Ocean water
Carbon Dioxide