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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. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Greenhouse Gases
Positive feedbacks both found in...
Ice in the Arctic
Severe coastal erosion
2. Where do greenhouse gases warm up the Earth?
Ice-Albedo
In the troposphere that we live in.
Through talik
Warming; cooling
3. Permafrost- A frozen soil
Surface Mass Balance
Frozen Soil
Deep tropics between 15O N and 15 O S are quite
Positive feedbacks both found in...
4. 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
Reduction in sea-ice extent
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Importance of ice sheets
Very small portion
5. 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
Atmospheric Structure
Threshold departures
.75OC/km-1
Mass Change
6. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
Climate Change in the Arctic
Longwave Radiation
Average radiative flux reaching the atmosphere
7. Like weighing oneself on the scale.
Effect of Deforestation on CO-2
Time Variable Gravity
Mass Change
Types of Albedo
8. In average: +1% in respect to 100 years ago.
Surface Mass Balance
Is precipitation around the world increasing?
Deep tropics between 15O N and 15 O S are quite
Altimetry Pros
9. Number of days that exceed a given temperature
Albedo
Absolute thresholds
Shortwave Length
Ice Sheets
10. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
How a closed talik forms
Global warming and hot nights?
Ice in the Arctic
Hydrological Drought
11. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Strong
More rain means no drought
US and precipitation
Infrared radiation
12. Warming- positive feedback - Cooling- negative feedback.
Why ice-albedo feedback is a big deal in the Arctic
Altimetry
Radiative Forcing
Ice-Albedo
13. LW - SW - 55% absorbed by surface
Shortwave Length
Grounding Lines
Natural Causes of Warming
Energy Budget
14. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
7%
70%
Discontinuous Permafrosrt
15. Summer increase in cloud cover - Winter decrease in cloud cover.
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16. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Ice Motion
Greenhouse Gases
30%
% of Greenhouse Gases
17. The buoyant force is equal to the weight of the displaced water.
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18. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Albedo
Radiative Flux
Warm
19. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Thermohaline Circulation Effect
reduction in sea-ice
Methane
Sea-Ice Albedo
20. 240 w/m squared
Amount of light actually reaching the Earth
Thermohaline Circulation
Stratospheric Ozone Depletion
How a closed talik forms
21. 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.
Contributions to CO2 from different activities
Permafrost
Troposphere
Inversion Layer (feedback)
22. 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
Negative Ice-Albedo Feedback
Stronger
IN the last 2 decades what we've seen
Wetter; drier
23. ~10% of incident solar energy (albedo 90)
Ice absorbs
Cloud Feedbacks
Deep tropics between 15O N and 15 O S are quite
Permafrost Degradation
24. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Very small portion
Sea ice melt does not change sea level
Heat Source and Pressure
Carbon Dioxide
25. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Melt
Some regions of the Earth have warmed faster than other regions.
How the cryosphere is affected by climate change
26. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Reduction in sea-ice extent
Once every 4 years.
Energy Budget
27. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Atmospheric Composition
Surface Mass Balance
45%
Meteorological Drought
28. 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.
El Nio is in the coasts of...
Negative Ice-Albedo Feedback
Permafrost Degradation
Longwave Radiation
29. 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
Importance of ice sheets
Ice Sheets
Questions to think about
Average radiative flux reaching the atmosphere
30. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Sea ice melt does not change sea level
Melt
Heat Source and Pressure
Discontinuous Permafrosrt
31. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Effect of Deforestation on CO-2
Monthly maximums and minimums
Affect Floods and Droughts
Ice Motion
32. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Grounding v Surface Melting
Ice Motion
30%
Amount of light actually reaching the Earth
33. High cloud has a _____ effect and cool cloud has a ____ effect
Surface Mass Balance
Warming; cooling
Negative
Albedos of Snow and Ice
34. 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.
Thermohaline Circulatoin
doubles
Monthly maximums and minimums
Frozen Soil
35. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Arctic Atmosphere
Active Layer
Carbon Dioxide
Inversion Layer Summer
36. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Increases - decreases
Ice/snow
Albedos of Snow and Ice
Ocean-Ice-Atmosphere Interaction
37. 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.
Threshold departures
Active Layer
Ice Shelf
Ocean water
38. Ocean retains ____ CO2
Precipitation and High Latitudes
Dynamic thinning
Ice shelf
25%
39. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Ice shelf
Surface Mass Balance
Arctic Atmosphere
Types of Albedo
40. Descending Air dry - Convection cells are wet.
IN the last 2 decades what we've seen
Infrared radiation
Atmospheric Circulation
Sublimation
41. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Arctic Atmosphere
30%
Reduction in sea-ice extent
Air pollution
42. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Rainy
How talik forms under lakes
Depth v Surface
summer
43. Longwave radiation - any radiation with a long wave will heat up quickly.
Permafrost
Time Variable Gravity
Infrared radiation
Melt
44. 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.
Ice absorbs
IN the last 2 decades what we've seen
Indirect heat wave effect
In the stratosphere.
45. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Agricultural Drought
Surface Mass Balance
Longwave Radiation
Affect Floods and Droughts
46. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Inversion Layer Summer
Effect of Deforestation on CO-2
Average radiative flux reaching the atmosphere
Ice loss
47. O Climate change in the Arctic is occurring now - Changes have been huge already
Severe coastal erosion
How talik forms under lakes
Today melting ice
Ice Sheets
48. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Ice/snow
75-OC
winter
Discontinuous Permafrosrt
49. 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.
Positive feedbacks both found in...
Negative Ice-Albedo Feedback
Antarctica
Thermohaline Circulation
50. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
What effects the density
Ice Motion
Sea Ice Extent is Changing in Antarctica as well
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