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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. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Threshold departures
Nitrous Oxide (N2O)
How the cryosphere is affected by climate change
2. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Albedo
Some parts of the planet are dry because of their location
% of Greenhouse Gases
Is precipitation around the world increasing?
3. 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
Ice Cap
25%
Radiative Flux
Archimedes' Principle
4. 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
Where rise in OC is greatest
What happens with the Ozone Hole
Some regions of the Earth have warmed faster than other regions.
70%
5. Number of days that exceed a given temperature
30%
Absolute thresholds
Ice loss
70%
6. Number of days when temperatures climb above average by a fixed amount.
El Nio is in the coasts of...
Threshold departures
All Greenhouse gases
25%
7. Longwave radiation - any radiation with a long wave will heat up quickly.
Active Layer
Infrared radiation
Earth's tilt
In the stratosphere.
8. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
How a closed talik forms
In the stratosphere.
Stronger
Cloud Feedbacks
9. Descending Air dry - Convection cells are wet.
Mass Balance
Thermokarst
Accumulation
Atmospheric Circulation
10. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
How to define a heatwave
Surface Mass Balance
Thermokarst
Ozone
11. Over the past century what has happened to the Earth's temperature?
Why Water Vapor is not a climate forcing
Ice Sheets
Some regions of the Earth have warmed faster than other regions.
Sublimation
12. Unfrozen ground that is found within a mass of permafrost
Thickness of the active layer and the permafrost depend on this
.75OC/km-1
Closed talik
Accumulation
13. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Layers of Earth
Hydrological Drought
Stronger
20%
14. 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
20%
Stronger
Through talik
Wetter; drier
15. 1.4 USA - 57 m total sea level equivalent
Antarctica
Permafrost
30%
Deep tropics between 15O N and 15 O S are quite
16. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
IPCC
Atmospheric Composition?
Thermohaline Circulatoin
La Nia
17. Is not an externally imposed perturbation to the climate system.
Absolute thresholds
Ice-Ocean Interactions
Why Water Vapor is not a climate forcing
Stronger
18. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Thermohaline Circulation
Positive feedbacks both found in...
Very small portion
19. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Ice Discharge
Atlantic Thermohaline Circulation
Change in vegetation generates a further feedback
20. Laser radar - H V - Long time series - high accuracy - Density
Greenland
Positive
Altimetry (height)
Deep tropics between 15O N and 15 O S are quite
21. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Why the Arctic climate is special
Cloud Feedbacks
Ice Shelf
% of Greenhouse Gases
22. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Why the Arctic climate is special
Ocean water
Atmospheric Composition
23. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Very small portion
Atmospheric Composition
summer
Atlantic Thermohaline Circulation
24. How often does El Nio occur?
GHG
What effects the density
Depth v Surface
Once every 4 years.
25. he increase of ozone concentration in the atmosphere helps ____ our planet
Thermokarst
Radiative Forcing
Ocean water
Warm
26. LW - SW - 55% absorbed by surface
Energy Budget
Thermohaline Circulation
% of Greenhouse Gases
Thermokarst
27. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
Thinner atmosphere
Agricultural Drought
Climate Change in the Arctic
28. In _______ - the inversions are less frequent and weaker in the Arctic.
.75OC/km-1
summer
25%
Energy Budget
29. Where do greenhouse gases warm up the Earth?
Grounding Lines
In the troposphere that we live in.
Rainy
Sublimation
30. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
75-OC
Precipitation and High Latitudes
Permafrost
31. 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.
Major distinction between Kyoto Protocol and Convention
Ice Motion
Positive
Sea-Ice Albedo
32. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
How talik forms under lakes
Negative Ice-Albedo Feedback
Stronger
33. 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.
Severe coastal erosion
Surface Mass Balance
Climate Change in the Arctic
Grounding Lines
34. CO2 GHG forcing - H2O - dominant/major GHG
Infrared radiation
Ozone Hole
GHG
Amount of light actually reaching the Earth
35. In ________- inversion layer is more common in the Arctic
Altimetry
How to define a heatwave
Sea Ice Extent is Changing in Antarctica as well
winter
36. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
air can warm dramatically
Heat Source and Pressure
Ice Motion
Thermohaline Circulatoin
37. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Radiative Flux
How talik forms under lakes
Black Carbon
38. Atmosphere retains ____ CO2
Dry
45%
In the Arctic where the air is cooler
Permafrost
39. 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.
Thermohaline Circulation Effect
Stratospheric Ozone Depletion
Permafrost
Ice-Ocean Interactions
40. Frozen +2 years - Few centimeters to 1500 m
doubles
25%
Permafrost
In the Arctic where the air is cooler
41. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Climate Change in the Arctic
Black Carbon
Questions to think about
Mass Budget
42. 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.
Radiative Flux
% of Greenhouse Gases
Changes in Arctic sea-ice Extent
Change in vegetation generates a further feedback
43. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Ocean water
The cryosphere
50%
Sea Ice
44. Ice sheets have a very ____ Albedo
summer
Albedos of Snow and Ice
Strong
Closed talik
45. 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.
Dry
Negative Ice-Albedo Feedback
reduction in sea-ice
In the troposphere that we live in.
46. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Deep tropics between 15O N and 15 O S are quite
Wetter; drier
Sublimation
Major distinction between Kyoto Protocol and Convention
47. 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
How to define a heatwave
Why the Arctic climate is special
Increases - decreases
48. A dome shaped cover of perennial ice and snow.
Ice Cap
El Nio is in the coasts of...
Antarctica
Ozone Hole
49. 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
Monthly maximums and minimums
.75OC/km-1
Thermohaline Circulation
How the cryosphere is affected by climate change
50. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Thinner atmosphere
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ozone Hole
Radiative Forcing