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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. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
In the stratosphere.
Mass Change
Altimetry
Carbon Dioxide
2. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Climate Change in the Arctic
Thermokarst
Types of Albedo
Cause of break of inversion layers or decrease in frequency
3. Rainy on yearly average. In these regions - rising air predominates.
Deep tropics between 15O N and 15 O S are quite
Air pollution
Arctic Atmosphere
Heat wave
4. Atmosphere retains ____ CO2
7%
Ice in the Arctic
Layers of Earth
45%
5. 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
Questions to think about
Longwave Radiation
20%
What happens with the Ozone Hole
6. 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.
Today melting ice
Thermohaline Circulatoin
Amount of light actually reaching the Earth
Ice Discharge
7. High cloud has a _____ effect and cool cloud has a ____ effect
Black Carbon
Antarctica
Warming; cooling
Grounding Lines
8. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
More rain means no drought
How we measure Mass Balance
30%
Thermokarst
9. 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.
Ice Shelf
Inversion Layer (feedback)
Thermohaline Circulatoin
Ice-Albedo
10. Warming- positive feedback - Cooling- negative feedback.
Radiative Flux
Stronger
Sea Ice Extent is Changing in Antarctica as well
Ice-Albedo
11. In average: +1% in respect to 100 years ago.
.75OC/km-1
Albedo
Is precipitation around the world increasing?
20%
12. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
IN the last 2 decades what we've seen
winter
Warming; cooling
13. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
How a closed talik forms
More rain means no drought
Positive feedbacks both found in...
Thermokarst
14. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
1 m/yr; 10x
Calving
Sunspots
Altimetry (height)
15. 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%
Talik
Earth's tilt
Albedos of Snow and Ice
Time Variable Gravity
16. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Grounding Lines
30%
In the Arctic where the air is cooler
How to define a heatwave
17. 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.
Ice Cap
Positive
reduction in sea-ice
What effects the density
18. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Archimedes' Principle
Wetter; drier
Average radiative flux reaching the atmosphere
Snow and snow covered ice absorb
19. Land Based Ecosystems retain ____ CO2.
Albedo
Thickness of the active layer and the permafrost depend on this
How to define a heatwave
30%
20. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
The cryosphere
Ice Sheets
Sea Ice
Heat wave
21. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Greenhouse Gases
In the stratosphere.
Affect Floods and Droughts
What effects the density
22. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
Infrared radiation
Some regions of the Earth have warmed faster than other regions.
Ice Cap
Thinner atmosphere
23. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Negative
Climate Change in the Arctic
Strong
24. 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
Threshold departures
Altimetry Pros
La Nia
El Nino
25. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Radiative Flux
Thermokarst Lake
Severe coastal erosion
More rain means no drought
26. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Reduction in sea-ice extent
Hydrological Drought
27. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
75-OC
Sea Ice
Positive
Thermokarst
28. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Sublimation
How we measure Mass Balance
Sea Ice Extent is Changing in Antarctica as well
Albedo
29. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
% of Greenhouse Gases
Global warming and hot nights?
Dry
30. 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.
Energy Budget
Percentile departures
Active Layer
Greenhouse Gases
31. O Climate change in the Arctic is occurring now - Changes have been huge already
Antarctica
Monthly maximums and minimums
Today melting ice
Energy Budget
32. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Thermohaline Circulation
Sea-Ice Albedo
Importance of ice sheets
Contributions to CO2 from different activities
33. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
70%
Earth's tilt
Reduction in sea-ice extent
34. The Earth emits this.
reduction in sea-ice
Longwave Radiation
Ice Cap
Grounding Lines
35. Tundra absorbs more energy than ice and snow but less than scrubs and forest - and with those plants migrating towards the north - they will further contribute ot absorb more energy.
Ice loss
Change in vegetation generates a further feedback
Melt
Mass Balance
36. Changes over time in the highest and lowest single temperature observed during a given month of the year.
1 m/yr; 10x
summer
25%
Monthly maximums and minimums
37. Greenhouse gases are mixed in the ____
Why ice-albedo feedback is a big deal in the Arctic
Troposphere
Melt
US and precipitation
38. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Radiative Flux
Some parts of the planet are dry because of their location
Mass Balance
Thickness of the active layer and the permafrost depend on this
39. 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
Depth v Surface
Arctic Atmosphere
doubles
Why the Arctic climate is special
40. 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
Discontinuous Permafrosrt
Wetter; drier
Ice loss
Active Layer
41. Amount of light absorbed by surface
Meteorological Drought
Inversion Layer Summer
50%
IPCC
42. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
30%
Greenland
The Ozone Hole
Altimetry (height)
43. A thick - floating slab of freshwater ice extending from coast to coast.
In the Arctic where the air is cooler
Hydrological Drought
Sea ice melt does not change sea level
Ice shelf
44. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
In the Arctic where the air is cooler
Monthly maximums and minimums
75-OC
45. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Ice Shelf
Closed talik
Precipitation and High Latitudes
46. US is responsible for ___ of the total CO2
1 m/yr; 10x
30%
How we measure Mass Balance
Ice Discharge
47. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Thinner atmosphere
Atlantic Thermohaline Circulation
Ice/snow
Through talik
48. Greenhouse gases are a ___ portion of the atmosphere
Radiative Flux
In the troposphere that we live in.
Very small portion
Severe coastal erosion
49. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Questions to think about
Very small portion
Greenhouse Gases
Accumulation
50. 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...
70%
Negative Ice-Albedo Feedback
Stronger