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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. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
1 m/yr; 10x
Indirect heat wave effect
Very small portion
Layers of Earth
2. Cooler water and drought conditions.
La Nia
Today melting ice
Accumulation
Types of Albedo
3. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Ice Discharge
Climate Change in the Arctic
GHG
Heat Source and Pressure
4. O Climate change in the Arctic is occurring now - Changes have been huge already
Black Carbon
Today melting ice
El Nino
Wetter; drier
5. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Ice-Ocean Interactions
Positive feedbacks both found in...
Normal condition for air
Ice Motion
6. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thermohaline Circulatoin
Black Carbon
Atmospheric Composition
7. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Thermohaline Circulation
Sea ice melt does not change sea level
What effects the density
Surface Mass Balance
8. 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.
Affect Floods and Droughts
Ice-Ocean Interactions
What happens with the Ozone Hole
Reduction in sea-ice extent
9. 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
Why ice-albedo feedback is a big deal in the Arctic
More rain means no drought
Melt
Thickness of the active layer and the permafrost depend on this
10. 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
Longwave Radiation
In the stratosphere.
Questions to think about
Natural Causes of Warming
11. Ice sheets have a very ____ Albedo
Deep tropics between 15O N and 15 O S are quite
Thermohaline Circulation Effect
Where rise in OC is greatest
Strong
12. 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
El Nio is in the coasts of...
Affect Floods and Droughts
Global warming and hot nights?
El Nino
13. Reduction of snow and ice cover - Changes in atmospheric circulation.
Ice Sheets
Cause of break of inversion layers or decrease in frequency
Time Variable Gravity
Thermokarst
14. 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.
Rainy
Warm
In the Arctic where the air is cooler
Negative Ice-Albedo Feedback
15. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Thermokarst
Methane
Grounding Lines
Altimetry Pros
16. 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
Wetter; drier
Infrared radiation
Warm
Where rise in OC is greatest
17. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Earth's tilt
20%
In the troposphere that we live in.
18. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
air can warm dramatically
All Greenhouse gases
Today melting ice
19. Antarctica - stratosphere - Sep-Oct
45%
Stronger
75-OC
Ozone Hole
20. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Absolute thresholds
Methane
50%
Deep tropics between 15O N and 15 O S are quite
21. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Mass Change
In the troposphere that we live in.
Warming; cooling
22. In average: +1% in respect to 100 years ago.
Through talik
Heat wave
Is precipitation around the world increasing?
El Nino
23. O Unfrozen soil that stays within the permafrost.
Talik
air can warm dramatically
Cloud Feedbacks
Snow and snow covered ice absorb
24. 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%
Open talik
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice shelf
Albedos of Snow and Ice
25. Really measures volume.
Mass Budget
Altimetry
Active Layer
50%
26. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Average radiative flux reaching the atmosphere
Arctic Atmosphere
Ice in the Arctic
Very small portion
27. 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.
Greenhouse Gases
Stratospheric Ozone Depletion
Precipitation and High Latitudes
7%
28. ~15% of incident solar energy (albedo 85)
Ice-Albedo
Permafrost
Snow and snow covered ice absorb
Agricultural Drought
29. Descending Air dry - Convection cells are wet.
45%
Monthly maximums and minimums
Atmospheric Circulation
Cause of break of inversion layers or decrease in frequency
30. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Sea ice melt does not change sea level
Layers of Earth
Ice shelf
Hydrological Drought
31. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
Through talik
70%
Normal condition for air
Wetter; drier
32. 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 to define a heatwave
summer
70%
How talik forms under lakes
33. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
75-OC
Radiative Forcing
Permafrost
34. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Inversion Layer Winter
air can warm dramatically
Heat wave
Time Variable Gravity
35. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Inversion Layer (feedback)
How talik forms under lakes
Cause of break of inversion layers or decrease in frequency
Dynamic thinning
36. The order of 1 m/year. Melting is ten times more.
Surface Mass Balance
In the Arctic where the air is cooler
El Nio is in the coasts of...
Arctic Atmosphere
37. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
Ice Sheets
Why the Arctic climate is special
Meteorological Drought
38. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Methane
Antarctica
Active Layer
Sublimation
39. Clouds 40~90% - Vegetation 10~15%
How a closed talik forms
Ocean water
Natural Causes of Warming
Types of Albedo
40. 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
What happens with the Ozone Hole
Altimetry Cons
Why the Arctic climate is special
30%
41. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Sea-Ice Albedo
Stratospheric Ozone Depletion
air can warm dramatically
42. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Permafrost
Surface Mass Balance
How a closed talik forms
Sea Ice Extent is Changing in Antarctica as well
43. Number of days when temperatures climb above average by a fixed amount.
reduction in sea-ice
Threshold departures
Ice loss
Carbon Dioxide
44. How often does El Nio occur?
Altimetry (height)
Active Layer
Altimetry
Once every 4 years.
45. Ocean retains ____ CO2
Depth v Surface
air can warm dramatically
Troposphere
25%
46. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Infrared radiation
How talik forms under lakes
Rainy
Sea Ice Extent is Changing in Antarctica as well
47. Greenhouse gases are mixed in the ____
Why ice-albedo feedback is a big deal in the Arctic
Troposphere
Absolute thresholds
How to define a heatwave
48. 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.
Some regions of the Earth have warmed faster than other regions.
reduction in sea-ice
Infrared radiation
Discontinuous
49. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Through talik
Thermokarst
How talik forms under lakes
Rainy
50. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Open talik
Why ice-albedo feedback is a big deal in the Arctic
Ice Discharge
Effect of Deforestation on CO-2