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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. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Open talik
reduction in sea-ice
Negative
2. ~15% of incident solar energy (albedo 85)
Altimetry Cons
Average radiative flux reaching the atmosphere
45%
Snow and snow covered ice absorb
3. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Normal condition for air
More rain means no drought
Thermohaline Circulation
4. Extent 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.
reduction in sea-ice
Hydrological Drought
Today melting ice
Warming; cooling
5. Ice sheets have a very ____ Albedo
Strong
Ozone
Through talik
Thickness of the active layer and the permafrost depend on this
6. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Normal condition for air
75-OC
Arctic Atmosphere
7. 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
Why the Arctic climate is special
Through talik
Time Variable Gravity
Ice Sheets
8. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Methane
Grounding Lines
reduction in sea-ice
The cryosphere
9. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
25%
Some regions of the Earth have warmed faster than other regions.
Heat Source and Pressure
summer
10. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Atmospheric Circulation
Rainy
Major distinction between Kyoto Protocol and Convention
11. 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
Greenland
El Nino
Effect of Deforestation on CO-2
How the cryosphere is affected by climate change
12. CO2 GHG forcing - H2O - dominant/major GHG
Thermohaline Circulation
GHG
Ice absorbs
Strong
13. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Active Layer
Ice Sheets
Negative
Calving
14. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Melt
Changes in Arctic sea-ice Extent
Atlantic Thermohaline Circulation
Ice Discharge
15. 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
Thermokarst
.75OC/km-1
50%
16. 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
Negative
doubles
Reduction in sea-ice extent
Greenland
17. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
winter
Where rise in OC is greatest
Rainy
18. Permafrost- A frozen soil
IN the last 2 decades what we've seen
Closed talik
Discontinuous Permafrosrt
Frozen Soil
19. Rainy on yearly average. In these regions - rising air predominates.
Active Layer
Increases - decreases
Ice/snow
Deep tropics between 15O N and 15 O S are quite
20. Laser radar - H V - Long time series - high accuracy - Density
25%
Altimetry (height)
Inversion Layer (feedback)
Surface Mass Balance
21. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Ice Sheets
Radiative Flux
50%
Methane
22. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
reduction in sea-ice
Increases - decreases
Sunspots
How talik forms under lakes
23. 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.
Some regions of the Earth have warmed faster than other regions.
Thermokarst
Radiative Forcing
What effects the density
24. 85%
Mass Budget
Indirect heat wave effect
Sea-Ice Albedo
Altimetry
25. Where does the ozone protect us?
In the stratosphere.
Some parts of the planet are dry because of their location
Mass Change
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
26. How much is the planet really warming?
Atmospheric Composition?
.7O Celsius over the past century.
Permafrost Degradation
20%
27. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Carbon Dioxide
Amount of light actually reaching the Earth
Thermokarst
Ozone
28. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Grounding v Surface Melting
Thermokarst Lake
Ice Sheets
Permafrost
29. LW - SW - 55% absorbed by surface
Thermohaline Circulation
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ozone
Energy Budget
30. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Permafrost
Changes in Arctic sea-ice Extent
How to define a heatwave
% of Greenhouse Gases
31. 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
GHG
.7O Celsius over the past century.
Altimetry Cons
32. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
El Nino
Calving
Positive feedbacks both found in...
Wetter; drier
33. Radiation absorbed by atmospheric greenhouse gases?
Dry
In the troposphere that we live in.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Threshold departures
34. Less frequent and weaker
Discontinuous Permafrosrt
Radiative Forcing
Global warming and hot nights?
Inversion Layer Summer
35. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Discontinuous
Atmospheric Composition
Normal condition for air
All Greenhouse gases
36. In _______ - the inversions are less frequent and weaker in the Arctic.
Ozone Hole
Active Layer
summer
45%
37. 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
Talik
Grounding Lines
Thermohaline Circulation
Ice absorbs
38. What can cause a change in the Earth's climate balance?
How the cryosphere is affected by climate change
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ozone Hole
How a closed talik forms
39. In average: +1% in respect to 100 years ago.
Accumulation
Ozone
La Nia
Is precipitation around the world increasing?
40. Atmosphere retains ____ CO2
Amount of light actually reaching the Earth
45%
Thermohaline Circulation
25%
41. 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
Negative Ice-Albedo Feedback
Mass Change
winter
Altimetry
42. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Cause of break of inversion layers or decrease in frequency
Atmospheric Circulation
Thermohaline Circulation
Ozone Hole
43. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
air can warm dramatically
Increases - decreases
Ice Shelf
Time Variable Gravity
44. Melting Point decreases
Open talik
50%
.75OC/km-1
Altimetry Cons
45. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Change in vegetation generates a further feedback
20%
Sea ice melt does not change sea level
Altimetry
46. 1.4 USA - 57 m total sea level equivalent
Ocean water
Mass Budget
Open talik
Antarctica
47. In ________- inversion layer is more common in the Arctic
75-OC
Rainy
winter
Stronger
48. 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.
The Ozone Hole
Greenhouse Gases
How talik forms under lakes
Atlantic Thermohaline Circulation
49. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Climate Change in the Arctic
Average radiative flux reaching the atmosphere
El Nio is in the coasts of...
Antarctica
50. High cloud has a _____ effect and cool cloud has a ____ effect
Some regions of the Earth have warmed faster than other regions.
Monthly maximums and minimums
Closed talik
Warming; cooling