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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. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Negative
Negative Ice-Albedo Feedback
Ice loss
2. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Greenhouse Gases
What effects the density
Ozone
Greenland
3. Clouds 40~90% - Vegetation 10~15%
Global warming and hot nights?
How we measure Mass Balance
Types of Albedo
Positive
4. ~15% of incident solar energy (albedo 85)
Where rise in OC is greatest
Snow and snow covered ice absorb
30%
Earth's tilt
5. CO2 GHG forcing - H2O - dominant/major GHG
Earth's tilt
GHG
How a closed talik forms
Increases - decreases
6. Melting Point decreases
More rain means no drought
Surface Mass Balance
.75OC/km-1
Is precipitation around the world increasing?
7. Number of days that exceed a given temperature
Absolute thresholds
Threshold departures
Agricultural Drought
Thinner atmosphere
8. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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9. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Negative Ice-Albedo Feedback
Ocean-Ice-Atmosphere Interaction
Time Variable Gravity
Ice loss
10. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
.7O Celsius over the past century.
How talik forms under lakes
25%
11. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
Deep tropics between 15O N and 15 O S are quite
Thermohaline Circulation Effect
Why the Arctic climate is special
12. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Very small portion
.7O Celsius over the past century.
Ice Motion
Rainy
13. 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
Altimetry
Thermohaline Circulation
Permafrost
Affect Floods and Droughts
14. Number of days that land among the hottest of all days in that month's long-term record.
The cryosphere
In the stratosphere.
Percentile departures
Discontinuous
15. 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.
Earth's tilt
Thermohaline Circulatoin
Surface Mass Balance
Types of Albedo
16. A thick - floating slab of freshwater ice extending from coast to coast.
Questions to think about
Ice shelf
Ice Sheets
Methane
17. Reduction of snow and ice cover - Changes in atmospheric circulation.
Albedos of Snow and Ice
Radiative Forcing
Cause of break of inversion layers or decrease in frequency
Hydrological Drought
18. The Earth emits this.
Longwave Radiation
Amount of light actually reaching the Earth
Wetter; drier
In the stratosphere.
19. 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
Ice shelf
Ocean water
Wetter; drier
Agricultural Drought
20. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Calving
Wetter; drier
Ozone Hole
Shortwave Length
21. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Positive
Altimetry Cons
El Nio is in the coasts of...
22. 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.
In the stratosphere.
Accumulation
Increases - decreases
Indirect heat wave effect
23. High vs low
Sea ice melt does not change sea level
doubles
Cloud Feedbacks
Ice Motion
24. 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.
Negative Ice-Albedo Feedback
% of Greenhouse Gases
Antarctica
Thermohaline Circulation
25. CO2 - CH4 - O3 - H2O - N2O - CFCs
Permafrost
All Greenhouse gases
Ice Discharge
30%
26. Greenhouse gases are mixed in the ____
Mass Balance
Cloud Feedbacks
Troposphere
More rain means no drought
27. 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.
Meteorological Drought
50%
Ice-Ocean Interactions
Albedo
28. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Thermohaline Circulation Effect
30%
Average radiative flux reaching the atmosphere
Sea Ice
29. 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
Today melting ice
Sea Ice
Why the Arctic climate is special
Agricultural Drought
30. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ice absorbs
air can warm dramatically
Ozone
Rainy
31. In _______ - the inversions are less frequent and weaker in the Arctic.
Nitrous Oxide (N2O)
50%
summer
Why ice-albedo feedback is a big deal in the Arctic
32. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Monthly maximums and minimums
Stronger
Carbon Dioxide
33. 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
Thermohaline Circulation Effect
Radiative Flux
Thermokarst Lake
Surface Mass Balance
34. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
What happens with the Ozone Hole
Reduction in sea-ice extent
Types of Albedo
35. 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
Closed talik
Wetter; drier
Inversion Layer (feedback)
Earth's tilt
36. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Absolute thresholds
Mass Balance
How we measure Mass Balance
Increases - decreases
37. Measures input and output.
Some regions of the Earth have warmed faster than other regions.
El Nio is in the coasts of...
Major distinction between Kyoto Protocol and Convention
Mass Budget
38. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
Hydrological Drought
How to define a heatwave
Very small portion
39. 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.
Permafrost Degradation
Altimetry
La Nia
Major distinction between Kyoto Protocol and Convention
40. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Climate Change in the Arctic
Ice Sheets
Heat wave
41. 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
Contributions to CO2 from different activities
Ice Shelf
Ice Sheets
Ocean water
42. 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.
Change in vegetation generates a further feedback
Major distinction between Kyoto Protocol and Convention
30%
Severe coastal erosion
43. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Atmospheric Circulation
Cause of break of inversion layers or decrease in frequency
Antarctica
Depth v Surface
44. x7 smaller - 7m total sea level equivalent.
Strong
Ice-Ocean Interactions
Greenland
doubles
45. Rainy on yearly average. In these regions - rising air predominates.
Thermohaline Circulation Effect
All Greenhouse gases
Discontinuous
Deep tropics between 15O N and 15 O S are quite
46. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Discharge
How a closed talik forms
Ocean-Ice-Atmosphere Interaction
Altimetry
47. The order of 1 m/year. Melting is ten times more.
Permafrost Degradation
Thermohaline Circulation
Surface Mass Balance
El Nio is in the coasts of...
48. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Albedos of Snow and Ice
Frozen Soil
Sunspots
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
49. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
What effects the density
Thinner atmosphere
Average radiative flux reaching the atmosphere
Layers of Earth
50. 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
Troposphere
Discontinuous Permafrosrt
Affect Floods and Droughts