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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. The buoyant force is equal to the weight of the displaced water.
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2. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Contributions to CO2 from different activities
Reduction in sea-ice extent
winter
Some parts of the planet are dry because of their location
3. Like weighing oneself on the scale.
Rainy
Warming; cooling
Some regions of the Earth have warmed faster than other regions.
Time Variable Gravity
4. 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:
Melt
Thinner atmosphere
Thermohaline Circulation
How we measure Mass Balance
5. Set up in 1988 by WMO and UNEP.
Earth's tilt
Archimedes' Principle
IPCC
Change in vegetation generates a further feedback
6. Amount of light absorbed by atmosphere
20%
Amount of light actually reaching the Earth
1 m/yr; 10x
Positive
7. CO2 GHG forcing - H2O - dominant/major GHG
El Nino
GHG
Warming; cooling
75-OC
8. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
Meteorological Drought
Altimetry (height)
Global warming and hot nights?
9. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Thermohaline Circulation
Grounding Lines
In the Arctic where the air is cooler
Atmospheric Composition?
10. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Ozone Hole
Effect of Deforestation on CO-2
Shortwave Length
Methane
11. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Atmospheric Structure
Troposphere
What happens with the Ozone Hole
12. 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.
The cryosphere
Change in vegetation generates a further feedback
Affect Floods and Droughts
Methane
13. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Radiative Flux
Indirect heat wave effect
Wetter; drier
Negative
14. Radiation absorbed by atmospheric greenhouse gases?
Percentile departures
Deep tropics between 15O N and 15 O S are quite
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Why Water Vapor is not a climate forcing
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%
Albedos of Snow and Ice
Increases - decreases
Ice Sheets
Longwave Radiation
16. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
How to define a heatwave
Atmospheric Composition
Positive
Ice Cap
17. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
Permafrost Degradation
Some parts of the planet are dry because of their location
Atmospheric Structure
18. The past climate...for this reason - both keep good records of climate change.
Thickness of the active layer and the permafrost depend on this
Mass Budget
Monthly maximums and minimums
Altimetry Pros
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
7%
Mass Balance
Greenland
20. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Ice Discharge
GHG
Depth v Surface
Precipitation and High Latitudes
21. Where does the ozone protect us?
Discontinuous Permafrosrt
Infrared radiation
Some parts of the planet are dry because of their location
In the stratosphere.
22. A dome shaped cover of perennial ice and snow.
Ice Cap
Ice Sheets
The cryosphere
Albedo
23. 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
Melt
Infrared radiation
Ice shelf
Shortwave Length
24. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Ice shelf
Discontinuous
Radiative Flux
Sea Ice
25. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Ocean water
Some regions of the Earth have warmed faster than other regions.
Global warming and hot nights?
How to define a heatwave
26. How much is the planet really warming?
.7O Celsius over the past century.
Once every 4 years.
Contributions to CO2 from different activities
Atmospheric Structure
27. 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
Thickness of the active layer and the permafrost depend on this
Sea-Ice Albedo
Ice-Albedo
How the cryosphere is affected by climate change
28. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Radiative Forcing
Natural Causes of Warming
Hydrological Drought
Sunspots
29. Land Based Ecosystems retain ____ CO2.
Types of Albedo
Radiative Forcing
Importance of ice sheets
30%
30. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
Heat wave
How we measure Mass Balance
Reduction in sea-ice extent
doubles
31. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Contributions to CO2 from different activities
Radiative Forcing
Inversion Layer (feedback)
Sea ice melt does not change sea level
32. 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
The Ozone Hole
Stratospheric Ozone Depletion
Deep tropics between 15O N and 15 O S are quite
Questions to think about
33. Frozen +2 years - Few centimeters to 1500 m
Ice shelf
Thinner atmosphere
Cloud Feedbacks
Permafrost
34. Over the Northern Hemisphere than the tropics.
Negative
Surface Mass Balance
Stronger
Where rise in OC is greatest
35. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
% of Greenhouse Gases
Surface Mass Balance
Open talik
Altimetry (height)
36. 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
How the cryosphere is affected by climate change
Through talik
In the troposphere that we live in.
Thermohaline Circulation
37. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
30%
US and precipitation
Grounding Lines
38. 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.
El Nio is in the coasts of...
Thermohaline Circulation Effect
Negative
Atmospheric Composition?
39. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Melt
Grounding Lines
Ozone Hole
Hydrological Drought
40. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Absolute thresholds
Why Water Vapor is not a climate forcing
Shortwave Length
41. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
The Ozone Hole
Ocean water
Ice shelf
Active Layer
42. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Rainy
Altimetry
Change in vegetation generates a further feedback
43. he increase of ozone concentration in the atmosphere helps ____ our planet
Snow and snow covered ice absorb
.75OC/km-1
Warm
Sublimation
44. 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.
GHG
Surface Mass Balance
Precipitation and High Latitudes
Major distinction between Kyoto Protocol and Convention
45. 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
Altimetry (height)
Reduction in sea-ice extent
Stronger
US and precipitation
46. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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47. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Ice-Ocean Interactions
Ice Cap
Greenhouse Gases
Arctic Atmosphere
48. High cloud has a _____ effect and cool cloud has a ____ effect
Radiative Forcing
How a closed talik forms
Depth v Surface
Warming; cooling
49. Industrial product - 300 ppb (parts per billion)
Ice Cap
Nitrous Oxide (N2O)
Change in vegetation generates a further feedback
Carbon Dioxide
50. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Change in vegetation generates a further feedback
The Ozone Hole
Stratospheric Ozone Depletion
Why Water Vapor is not a climate forcing