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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. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Nitrous Oxide (N2O)
Average radiative flux reaching the atmosphere
Atmospheric Structure
2. 10 : 1 - grounding ; surface
The cryosphere
Cloud Feedbacks
Permafrost Degradation
Grounding v Surface Melting
3. Number of days when temperatures climb above average by a fixed amount.
Accumulation
Methane
Snow and snow covered ice absorb
Threshold departures
4. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
La Nia
Active Layer
Thermokarst
Altimetry Pros
5. 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.
30%
Permafrost Degradation
Accumulation
Ice-Ocean Interactions
6. 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 talik forms under lakes
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Deep tropics between 15O N and 15 O S are quite
What happens with the Ozone Hole
7. Ocean retains ____ CO2
Inversion Layer Winter
25%
Atmospheric Composition
Ocean water
8. The buoyant force is equal to the weight of the displaced water.
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9. 1.4 USA - 57 m total sea level equivalent
Ice/snow
Methane
Wetter; drier
Antarctica
10. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Ice/snow
Grounding Lines
Thermohaline Circulatoin
Effect of Deforestation on CO-2
11. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Thinner atmosphere
The Ozone Hole
Why ice-albedo feedback is a big deal in the Arctic
Ice Discharge
12. 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
Sublimation
Atmospheric Composition
Thermohaline Circulation
Importance of ice sheets
13. 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
Surface Mass Balance
Negative Ice-Albedo Feedback
El Nino
Once every 4 years.
14. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Radiative Flux
Antarctica
Sunspots
El Nino
15. 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
How talik forms under lakes
Sublimation
Radiative Flux
Thermohaline Circulatoin
16. ~10% of incident solar energy (albedo 90)
Severe coastal erosion
.75OC/km-1
Amount of light actually reaching the Earth
Ice absorbs
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.
Ozone Hole
What effects the density
Closed talik
.7O Celsius over the past century.
18. ~15% of incident solar energy (albedo 85)
Arctic Atmosphere
Snow and snow covered ice absorb
Global warming and hot nights?
Dry
19. Land Based Ecosystems retain ____ CO2.
Strong
30%
Earth's tilt
Active Layer
20. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Melt
Ice in the Arctic
Grounding v Surface Melting
Contributions to CO2 from different activities
21. 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.
Amount of light actually reaching the Earth
Greenhouse Gases
Earth's tilt
Atlantic Thermohaline Circulation
22. Cooler water and drought conditions.
Carbon Dioxide
The cryosphere
La Nia
Severe coastal erosion
23. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Ice in the Arctic
The cryosphere
Grounding Lines
24. Amount of light absorbed by atmosphere
In the stratosphere.
Ice loss
20%
Permafrost
25. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Atlantic Thermohaline Circulation
Sublimation
Monthly maximums and minimums
Radiative Flux
26. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Natural Causes of Warming
All Greenhouse gases
Open talik
27. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Longwave Radiation
Positive
Surface Mass Balance
Greenland
28. 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.
Wetter; drier
Albedo
Troposphere
Change in vegetation generates a further feedback
29. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Sea ice melt does not change sea level
Active Layer
Ice-Albedo
Mass Budget
30. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
In the stratosphere.
Some parts of the planet are dry because of their location
Dry
Heat Source and Pressure
31. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How to define a heatwave
Inversion Layer Winter
Ocean water
How we measure Mass Balance
32. Descending Air dry - Convection cells are wet.
Infrared radiation
Atmospheric Circulation
Why Water Vapor is not a climate forcing
Some regions of the Earth have warmed faster than other regions.
33. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
El Nino
Longwave Radiation
Methane
34. Permafrost- A frozen soil
Deep tropics between 15O N and 15 O S are quite
Frozen Soil
Discontinuous Permafrosrt
Some parts of the planet are dry because of their location
35. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Affect Floods and Droughts
Open talik
Where rise in OC is greatest
Air pollution
36. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Warming; cooling
doubles
Open talik
air can warm dramatically
37. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Energy Budget
Atmospheric Circulation
Thermokarst Lake
Monthly maximums and minimums
38. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Sea-Ice Albedo
GHG
Melt
The Ozone Hole
39. 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.
Antarctica
Accumulation
25%
Major distinction between Kyoto Protocol and Convention
40. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Grounding Lines
Average radiative flux reaching the atmosphere
Positive feedbacks both found in...
Why Water Vapor is not a climate forcing
41. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
El Nio is in the coasts of...
winter
Atmospheric Composition
42. x7 smaller - 7m total sea level equivalent.
Surface Mass Balance
How a closed talik forms
Greenland
Types of Albedo
43. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Dry
Warm
Why ice-albedo feedback is a big deal in the Arctic
44. Frozen +2 years - Few centimeters to 1500 m
Open talik
Permafrost
Changes in Arctic sea-ice Extent
Types of Albedo
45. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Changes in Arctic sea-ice Extent
Atmospheric Structure
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Agricultural Drought
46. How often does El Nio occur?
Active Layer
Atmospheric Composition
Once every 4 years.
Increases - decreases
47. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Antarctica
Deep tropics between 15O N and 15 O S are quite
El Nio is in the coasts of...
Methane
48. The Earth emits this.
Time Variable Gravity
Ozone Hole
Longwave Radiation
Permafrost Degradation
49. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
How talik forms under lakes
Stratospheric Ozone Depletion
Shortwave Length
50. 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.
Atmospheric Composition
Inversion Layer Summer
How talik forms under lakes
El Nino