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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. Summer increase in cloud cover - Winter decrease in cloud cover.
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2. 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 Nino
More rain means no drought
Ice Motion
Greenland
3. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Heat wave
Snow and snow covered ice absorb
Active Layer
Earth's tilt
4. 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
.7O Celsius over the past century.
Contributions to CO2 from different activities
In the Arctic where the air is cooler
Permafrost
5. Greenhouse gases are mixed in the ____
How to define a heatwave
More rain means no drought
Troposphere
winter
6. Atmosphere retains ____ CO2
45%
Antarctica
Altimetry Cons
Air pollution
7. Total absorbed solar radiation
70%
Ocean water
Change in vegetation generates a further feedback
More rain means no drought
8. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
US and precipitation
Sea-Ice Albedo
Active Layer
Infrared radiation
9. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Negative Ice-Albedo Feedback
Agricultural Drought
In the stratosphere.
10. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Methane
What happens with the Ozone Hole
Infrared radiation
Ice in the Arctic
11. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Surface Mass Balance
Thermokarst
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
All Greenhouse gases
12. 10 : 1 - grounding ; surface
Melt
Once every 4 years.
Grounding v Surface Melting
20%
13. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
In the stratosphere.
Discontinuous
Ocean-Ice-Atmosphere Interaction
Heat wave
14. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Surface Mass Balance
Stratospheric Ozone Depletion
Ice/snow
Monthly maximums and minimums
15. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Types of Albedo
Permafrost Degradation
Atmospheric Structure
16. Ice sheets have a very ____ Albedo
Strong
Albedo
Talik
Some regions of the Earth have warmed faster than other regions.
17. 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.
Cause of break of inversion layers or decrease in frequency
Thermohaline Circulation Effect
Accumulation
IN the last 2 decades what we've seen
18. 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
Thermokarst
Snow and snow covered ice absorb
Black Carbon
Permafrost
19. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Cause of break of inversion layers or decrease in frequency
Why the Arctic climate is special
Thermokarst
Thermokarst Lake
20. Volcanic eruptions - Sunspots - Wobbly Earth
Global warming and hot nights?
Grounding v Surface Melting
Natural Causes of Warming
The Ozone Hole
21. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Stratospheric Ozone Depletion
Through talik
El Nino
GHG
22. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Once every 4 years.
Contributions to CO2 from different activities
Inversion Layer Summer
30%
23. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
The Ozone Hole
Nitrous Oxide (N2O)
Black Carbon
Ice-Albedo
24. 85%
Thermohaline Circulation
Sea-Ice Albedo
Effect of Deforestation on CO-2
The cryosphere
25. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Is precipitation around the world increasing?
Natural Causes of Warming
Ice Discharge
What effects the density
26. 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 Sheets
Inversion Layer (feedback)
Through talik
Ice Motion
27. 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.
Wetter; drier
Hydrological Drought
How talik forms under lakes
What effects the density
28. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
Inversion Layer Winter
Positive feedbacks both found in...
Energy Budget
29. Clouds 40~90% - Vegetation 10~15%
Ice in the Arctic
Once every 4 years.
summer
Types of Albedo
30. The amount of light reflected by an object.
Ocean-Ice-Atmosphere Interaction
Ozone Hole
Albedo
Once every 4 years.
31. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Snow and snow covered ice absorb
US and precipitation
Surface Mass Balance
El Nio is in the coasts of...
32. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Cloud Feedbacks
Layers of Earth
1 m/yr; 10x
33. The Earth emits this.
Ozone
Longwave Radiation
Carbon Dioxide
IPCC
34. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
The Ozone Hole
Surface Mass Balance
Questions to think about
Thinner atmosphere
35. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Major distinction between Kyoto Protocol and Convention
Active Layer
El Nio is in the coasts of...
Greenland
36. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Talik
Amount of light actually reaching the Earth
Effect of Deforestation on CO-2
Very small portion
37. High vs low
Ocean-Ice-Atmosphere Interaction
Troposphere
Cloud Feedbacks
Precipitation and High Latitudes
38. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Thickness of the active layer and the permafrost depend on this
Thermohaline Circulatoin
Positive feedbacks both found in...
Change in vegetation generates a further feedback
39. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Amount of light actually reaching the Earth
Normal condition for air
Strong
How to define a heatwave
40. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Thermohaline Circulation
winter
air can warm dramatically
41. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Talik
Dry
Inversion Layer Summer
Radiative Forcing
42. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
IPCC
Archimedes' Principle
Increases - decreases
43. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Severe coastal erosion
Layers of Earth
Grounding Lines
Discontinuous
44. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Why Water Vapor is not a climate forcing
Increases - decreases
Changes in Arctic sea-ice Extent
Cloud Feedbacks
45. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Infrared radiation
Ice/snow
Effect of Deforestation on CO-2
30%
46. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Archimedes' Principle
Ocean water
70%
Active Layer
47. Permafrost- A frozen soil
Thermokarst
Frozen Soil
7%
Discontinuous Permafrosrt
48. Ocean retains ____ CO2
25%
Time Variable Gravity
Stratospheric Ozone Depletion
Effect of Deforestation on CO-2
49. Longwave radiation - any radiation with a long wave will heat up quickly.
Atmospheric Composition?
Deep tropics between 15O N and 15 O S are quite
Infrared radiation
Discontinuous Permafrosrt
50. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Atmospheric Structure
Positive
Ice Sheets
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