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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. Greenhouse gases are a ___ portion of the atmosphere
Today melting ice
Contributions to CO2 from different activities
Very small portion
Stratospheric Ozone Depletion
2. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Average radiative flux reaching the atmosphere
Major distinction between Kyoto Protocol and Convention
Thermokarst Lake
Types of Albedo
3. Less frequent and weaker
Inversion Layer Summer
Wetter; drier
Black Carbon
Ice Sheets
4. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
How to define a heatwave
In the Arctic where the air is cooler
Layers of Earth
5. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Negative
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Discontinuous Permafrosrt
6. Is not an externally imposed perturbation to the climate system.
Albedos of Snow and Ice
Surface Mass Balance
IPCC
Why Water Vapor is not a climate forcing
7. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Climate Change in the Arctic
Stratospheric Ozone Depletion
Ice Cap
El Nio is in the coasts of...
8. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Depth v Surface
Ice-Ocean Interactions
How a closed talik forms
Air pollution
9. Forms in a mosaic of favoured locations.
Grounding Lines
La Nia
The cryosphere
Discontinuous Permafrosrt
10. 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.
Calving
Thermohaline Circulatoin
Active Layer
Thermohaline Circulation Effect
11. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Ice in the Arctic
Thermohaline Circulatoin
Shortwave Length
How talik forms under lakes
12. Volcanic eruptions - Sunspots - Wobbly Earth
Wetter; drier
Natural Causes of Warming
Why ice-albedo feedback is a big deal in the Arctic
Climate Change in the Arctic
13. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Mass Balance
How to define a heatwave
Cause of break of inversion layers or decrease in frequency
Today melting ice
14. Number of days when temperatures climb above average by a fixed amount.
Stratospheric Ozone Depletion
Threshold departures
Troposphere
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
15. 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.
Methane
Indirect heat wave effect
Global warming and hot nights?
Ice-Albedo
16. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
The Ozone Hole
Normal condition for air
Strong
Hydrological Drought
17. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Ocean-Ice-Atmosphere Interaction
In the Arctic where the air is cooler
Ice Motion
18. 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
How the cryosphere is affected by climate change
How talik forms under lakes
Warm
Some parts of the planet are dry because of their location
19. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
Ice in the Arctic
Albedos of Snow and Ice
Troposphere
20. Cooler water and drought conditions.
La Nia
Monthly maximums and minimums
Permafrost
Ice-Albedo
21. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Troposphere
In the troposphere that we live in.
How to define a heatwave
Heat Source and Pressure
22. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermohaline Circulatoin
Absolute thresholds
Some parts of the planet are dry because of their location
Thermokarst
23. Measures input and output.
Antarctica
Mass Budget
Carbon Dioxide
Open talik
24. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ice Sheets
Accumulation
Stronger
Agricultural Drought
25. Amount of light absorbed by surface
air can warm dramatically
50%
Normal condition for air
Amount of light actually reaching the Earth
26. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Dry
winter
Ice in the Arctic
Atmospheric Composition
27. Atmospheric Cooling - Both negative (stabilizing) feedbacks - It is not happening now - but it has happened in the past - Ice-albedo feedback was the dominant feedback during the ice ages.
Increases - decreases
Absolute thresholds
Negative Ice-Albedo Feedback
Permafrost
28. Laser radar - H V - Long time series - high accuracy - Density
Changes in Arctic sea-ice Extent
All Greenhouse gases
Altimetry (height)
Sea ice melt does not change sea level
29. The amount of light reflected by an object.
Albedo
.75OC/km-1
Stronger
Dynamic thinning
30. The Earth emits this.
.7O Celsius over the past century.
Altimetry (height)
Is precipitation around the world increasing?
Longwave Radiation
31. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Shortwave Length
Atmospheric Structure
summer
In the troposphere that we live in.
32. 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.
Albedo
Greenhouse Gases
Global warming and hot nights?
Ice Shelf
33. Ocean retains ____ CO2
25%
El Nino
El Nio is in the coasts of...
Layers of Earth
34. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Is precipitation around the world increasing?
Ozone
Stronger
Increases - decreases
35. 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
Wetter; drier
Types of Albedo
El Nino
Cloud Feedbacks
36. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Average radiative flux reaching the atmosphere
Today melting ice
Inversion Layer Summer
Atmospheric Composition?
37. 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.
Sea-Ice Albedo
Permafrost
Climate Change in the Arctic
All Greenhouse gases
38. ~10% of incident solar energy (albedo 90)
Natural Causes of Warming
.75OC/km-1
Surface Mass Balance
Ice absorbs
39. 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
Very small portion
Thickness of the active layer and the permafrost depend on this
Inversion Layer Winter
40. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
Questions to think about
Ice Sheets
Ice-Albedo
Normal condition for air
41. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
25%
Amount of light actually reaching the Earth
Carbon Dioxide
42. Rainy on yearly average. In these regions - rising air predominates.
Ice in the Arctic
Deep tropics between 15O N and 15 O S are quite
Layers of Earth
How a closed talik forms
43. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Methane
Sublimation
Altimetry Cons
Ocean water
44. 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.
Ice-Ocean Interactions
Atmospheric Structure
Discontinuous Permafrosrt
reduction in sea-ice
45. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Depth v Surface
Dynamic thinning
Change in vegetation generates a further feedback
Contributions to CO2 from different activities
46. Over the past century what has happened to the Earth's temperature?
Open talik
Some regions of the Earth have warmed faster than other regions.
summer
Once every 4 years.
47. Land Based Ecosystems retain ____ CO2.
Thermokarst
Change in vegetation generates a further feedback
30%
Normal condition for air
48. O Climate change in the Arctic is occurring now - Changes have been huge already
Greenhouse Gases
Today melting ice
Deep tropics between 15O N and 15 O S are quite
75-OC
49. CO2 GHG forcing - H2O - dominant/major GHG
Active Layer
70%
How talik forms under lakes
GHG
50. 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
.7O Celsius over the past century.
Ice Motion
What happens with the Ozone Hole
More rain means no drought