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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. x7 smaller - 7m total sea level equivalent.
Greenland
How to define a heatwave
Indirect heat wave effect
Sea ice melt does not change sea level
2. 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.
Amount of light actually reaching the Earth
Affect Floods and Droughts
Ice/snow
Thermohaline Circulatoin
3. The Earth emits this.
Longwave Radiation
Where rise in OC is greatest
Strong
Atmospheric Circulation
4. 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
Time Variable Gravity
1 m/yr; 10x
Ice Sheets
Strong
5. Total absorbed solar radiation
Cloud Feedbacks
70%
Atlantic Thermohaline Circulation
Heat Source and Pressure
6. CO2 - CH4 - O3 - H2O - N2O - CFCs
Ice Motion
All Greenhouse gases
The Ozone Hole
Grounding Lines
7. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Greenland
Ice/snow
Contributions to CO2 from different activities
Natural Causes of Warming
8. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
Black Carbon
70%
Frozen Soil
9. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
7%
Snow and snow covered ice absorb
Carbon Dioxide
El Nino
10. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Ozone
Severe coastal erosion
Air pollution
In the stratosphere.
11. 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
Normal condition for air
Radiative Flux
Grounding v Surface Melting
Ice shelf
12. Over the past century what has happened to the Earth's temperature?
Grounding Lines
30%
Some regions of the Earth have warmed faster than other regions.
Strong
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
Thermohaline Circulation Effect
Ice-Ocean Interactions
Increases - decreases
Thermohaline Circulation
14. Reduction of snow and ice cover - Changes in atmospheric circulation.
Infrared radiation
Mass Change
Cause of break of inversion layers or decrease in frequency
Monthly maximums and minimums
15. High cloud has a _____ effect and cool cloud has a ____ effect
Ice Sheets
Rainy
Average radiative flux reaching the atmosphere
Warming; cooling
16. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Ice Cap
Dynamic thinning
Altimetry Cons
Warm
17. Amount of light absorbed by atmosphere
Inversion Layer (feedback)
20%
Frozen Soil
Permafrost
18. 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
Why ice-albedo feedback is a big deal in the Arctic
Mass Change
Thermokarst Lake
19. More common
Inversion Layer Winter
Strong
Positive feedbacks both found in...
Methane
20. Measures input and output.
Reduction in sea-ice extent
Ice-Ocean Interactions
Mass Budget
Change in vegetation generates a further feedback
21. Ice sheets have a very ____ Albedo
Stratospheric Ozone Depletion
Strong
Why ice-albedo feedback is a big deal in the Arctic
Time Variable Gravity
22. 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
Permafrost Degradation
Atmospheric Structure
Why the Arctic climate is special
23. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Ice-Albedo
Atmospheric Composition?
Effect of Deforestation on CO-2
Rainy
24. Ocean retains ____ CO2
25%
Carbon Dioxide
Accumulation
Affect Floods and Droughts
25. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
How talik forms under lakes
Permafrost
Strong
Heat Source and Pressure
26. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
IN the last 2 decades what we've seen
Permafrost
The Ozone Hole
Atmospheric Composition
27. Number of days that exceed a given temperature
Absolute thresholds
Melt
Stronger
Average radiative flux reaching the atmosphere
28. Number of days that land among the hottest of all days in that month's long-term record.
.75OC/km-1
Ocean-Ice-Atmosphere Interaction
Percentile departures
Positive feedbacks both found in...
29. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Accumulation
Active Layer
Threshold departures
30. In _______ - the inversions are less frequent and weaker in the Arctic.
summer
Dry
Mass Balance
Some parts of the planet are dry because of their location
31. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Where rise in OC is greatest
Ice Shelf
US and precipitation
30%
32. O Climate change in the Arctic is occurring now - Changes have been huge already
Atmospheric Circulation
.75OC/km-1
Today melting ice
Atmospheric Composition
33. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Ice absorbs
Altimetry Cons
Some parts of the planet are dry because of their location
Rainy
34. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
La Nia
Thermohaline Circulatoin
What effects the density
Methane
35. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
50%
Grounding Lines
IPCC
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
36. A dome shaped cover of perennial ice and snow.
Permafrost Degradation
Indirect heat wave effect
Ice Cap
More rain means no drought
37. The amount of light reflected by an object.
Changes in Arctic sea-ice Extent
Albedo
70%
Black Carbon
38. How often does El Nio occur?
Ice in the Arctic
30%
Once every 4 years.
Heat Source and Pressure
39. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
Antarctica
Radiative Flux
Agricultural Drought
40. 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.
Active Layer
Ice Cap
doubles
Ice-Ocean Interactions
41. 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
How the cryosphere is affected by climate change
Mass Budget
Permafrost Degradation
Affect Floods and Droughts
42. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Discontinuous Permafrosrt
Thinner atmosphere
Through talik
Sea Ice
43. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
30%
Layers of Earth
Surface Mass Balance
44. Amount of light absorbed by surface
50%
Thermohaline Circulatoin
Air pollution
Closed talik
45. 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.
Ice Sheets
Atmospheric Circulation
45%
Ice Shelf
46. 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.
Changes in Arctic sea-ice Extent
Severe coastal erosion
Reduction in sea-ice extent
Positive
47. How much is the planet really warming?
Ice Discharge
.7O Celsius over the past century.
Change in vegetation generates a further feedback
Why ice-albedo feedback is a big deal in the Arctic
48. 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
Thermohaline Circulation
Very small portion
25%
El Nino
49. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Snow and snow covered ice absorb
Sea ice melt does not change sea level
How a closed talik forms
Atmospheric Composition
50. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Ice Sheets
Types of Albedo
Ocean water
Shortwave Length