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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. 85%
Ozone Hole
Severe coastal erosion
Sea-Ice Albedo
IPCC
2. 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
Mass Balance
Ice shelf
Energy Budget
Thinner atmosphere
3. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Monthly maximums and minimums
% of Greenhouse Gases
Importance of ice sheets
45%
4. The order of 1 m/year. Melting is ten times more.
Average radiative flux reaching the atmosphere
Ice Motion
Surface Mass Balance
Once every 4 years.
5. ~10% of incident solar energy (albedo 90)
Ice absorbs
Ice Cap
Through talik
75-OC
6. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Calving
El Nio is in the coasts of...
Cause of break of inversion layers or decrease in frequency
30%
7. In average: +1% in respect to 100 years ago.
air can warm dramatically
How to define a heatwave
Is precipitation around the world increasing?
Natural Causes of Warming
8. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Meteorological Drought
Thermokarst
How to define a heatwave
9. Rainy on yearly average. In these regions - rising air predominates.
Deep tropics between 15O N and 15 O S are quite
Positive
Ice-Ocean Interactions
Indirect heat wave effect
10. How often does El Nio occur?
Normal condition for air
Ozone
Arctic Atmosphere
Once every 4 years.
11. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Permafrost Degradation
Negative Ice-Albedo Feedback
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Air pollution
12. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
How we measure Mass Balance
Earth's tilt
Amount of light actually reaching the Earth
13. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Ocean water
Atlantic Thermohaline Circulation
Longwave Radiation
14. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
What effects the density
Sea-Ice Albedo
Thermohaline Circulation
Ice/snow
15. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Greenland
Contributions to CO2 from different activities
Ozone Hole
Where rise in OC is greatest
16. US is responsible for ___ of the total CO2
Monthly maximums and minimums
70%
Talik
30%
17. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Altimetry Cons
Earth's tilt
Some parts of the planet are dry because of their location
Energy Budget
18. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Thermokarst
Surface Mass Balance
Active Layer
Talik
19. High cloud has a _____ effect and cool cloud has a ____ effect
Warming; cooling
Warm
25%
Amount of light actually reaching the Earth
20. Number of days that exceed a given temperature
Absolute thresholds
Thermohaline Circulation
45%
Ozone Hole
21. 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) -
US and precipitation
Methane
Normal condition for air
Contributions to CO2 from different activities
22. 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.
50%
Contributions to CO2 from different activities
Why Water Vapor is not a climate forcing
Thermohaline Circulation Effect
23. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
reduction in sea-ice
Climate Change in the Arctic
Changes in Arctic sea-ice Extent
24. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Mass Budget
doubles
Sublimation
The Ozone Hole
25. How much is the planet really warming?
Rainy
Archimedes' Principle
Thermokarst Lake
.7O Celsius over the past century.
26. Cooler water and drought conditions.
Once every 4 years.
Grounding Lines
La Nia
reduction in sea-ice
27. Over the past century what has happened to the Earth's temperature?
Once every 4 years.
In the troposphere that we live in.
Troposphere
Some regions of the Earth have warmed faster than other regions.
28. 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.
Indirect heat wave effect
Altimetry Pros
Deep tropics between 15O N and 15 O S are quite
Ice Sheets
29. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Ocean-Ice-Atmosphere Interaction
How to define a heatwave
Increases - decreases
Radiative Forcing
30. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Black Carbon
Precipitation and High Latitudes
Greenland
Atmospheric Structure
31. The Earth emits this.
Ice Shelf
Longwave Radiation
Today melting ice
Surface Mass Balance
32. 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
Positive
doubles
Precipitation and High Latitudes
Ocean water
33. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
In the Arctic where the air is cooler
air can warm dramatically
Ice Sheets
Ozone
34. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Atlantic Thermohaline Circulation
Depth v Surface
Ozone Hole
Greenland
35. Summer increase in cloud cover - Winter decrease in cloud cover.
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36. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
air can warm dramatically
Increases - decreases
Permafrost
Why Water Vapor is not a climate forcing
37. High vs low
Cloud Feedbacks
Talik
Precipitation and High Latitudes
Nitrous Oxide (N2O)
38. Melting Point decreases
winter
50%
Average radiative flux reaching the atmosphere
.75OC/km-1
39. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Sea Ice
Meteorological Drought
Thickness of the active layer and the permafrost depend on this
Carbon Dioxide
40. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
Stronger
Permafrost Degradation
Ozone Hole
41. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Today melting ice
Ice in the Arctic
Layers of Earth
Reduction in sea-ice extent
42. 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%
Altimetry Cons
Albedos of Snow and Ice
Ice Shelf
20%
43. Amount of light absorbed by atmosphere
Earth's tilt
20%
Thermohaline Circulation Effect
Black Carbon
44. The past climate...for this reason - both keep good records of climate change.
Thickness of the active layer and the permafrost depend on this
Ozone Hole
Ice in the Arctic
Is precipitation around the world increasing?
45. 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.
IPCC
Major distinction between Kyoto Protocol and Convention
50%
In the troposphere that we live in.
46. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Antarctica
Depth v Surface
Questions to think about
47. 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
How we measure Mass Balance
Greenhouse Gases
What happens with the Ozone Hole
What effects the density
48. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
El Nio is in the coasts of...
More rain means no drought
Effect of Deforestation on CO-2
49. Over the Northern Hemisphere than the tropics.
Grounding Lines
Thermokarst Lake
Where rise in OC is greatest
IPCC
50. Number of days when temperatures climb above average by a fixed amount.
Monthly maximums and minimums
Positive
Sublimation
Threshold departures