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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. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Reduction in sea-ice extent
What happens with the Ozone Hole
45%
Ocean water
2. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Altimetry
Ice Motion
Why the Arctic climate is special
Open talik
3. 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.
Inversion Layer (feedback)
Antarctica
Some regions of the Earth have warmed faster than other regions.
Shortwave Length
4. LW - SW - 55% absorbed by surface
GHG
Energy Budget
Air pollution
Ice shelf
5. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Ice Sheets
All Greenhouse gases
Inversion Layer Winter
6. 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
Ocean water
Thermohaline Circulation
Snow and snow covered ice absorb
7. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Percentile departures
Ozone Hole
Open talik
IN the last 2 decades what we've seen
8. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
In the stratosphere.
Sea Ice
Amount of light actually reaching the Earth
9. 85%
Sea-Ice Albedo
50%
Inversion Layer Winter
Some parts of the planet are dry because of their location
10. Clouds 40~90% - Vegetation 10~15%
Methane
Permafrost
Types of Albedo
IN the last 2 decades what we've seen
11. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Very small portion
Warm
Ice-Ocean Interactions
Permafrost Degradation
12. ~10% of incident solar energy (albedo 90)
Major distinction between Kyoto Protocol and Convention
Ice absorbs
GHG
Thinner atmosphere
13. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Nitrous Oxide (N2O)
Ice Sheets
Layers of Earth
Air pollution
14. 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
Calving
Wetter; drier
Reduction in sea-ice extent
In the stratosphere.
15. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Importance of ice sheets
Threshold departures
Grounding Lines
16. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
In the troposphere that we live in.
Sea Ice
Heat wave
Atmospheric Composition?
17. Total absorbed solar radiation
Inversion Layer Winter
70%
All Greenhouse gases
Importance of ice sheets
18. Precipitation intensity will rise ___ for every 1 OC of warming.
Change in vegetation generates a further feedback
7%
Melt
Permafrost Degradation
19. Over the Northern Hemisphere than the tropics.
.7O Celsius over the past century.
All Greenhouse gases
Ozone Hole
Where rise in OC is greatest
20. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Antarctica
How talik forms under lakes
Climate Change in the Arctic
Negative
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.
Negative
Methane
Greenhouse Gases
Thickness of the active layer and the permafrost depend on this
22. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Altimetry (height)
Types of Albedo
Mass Budget
23. Forms in a mosaic of favoured locations.
What happens with the Ozone Hole
Discontinuous Permafrosrt
Strong
Surface Mass Balance
24. 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
Questions to think about
Ice absorbs
Sunspots
Is precipitation around the world increasing?
25. Water vapor means more water up in the clouds and less in the ground!
Once every 4 years.
More rain means no drought
Radiative Forcing
Snow and snow covered ice absorb
26. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Time Variable Gravity
Ozone
Changes in Arctic sea-ice Extent
Meteorological Drought
27. Where do greenhouse gases warm up the Earth?
Hydrological Drought
Active Layer
Surface Mass Balance
In the troposphere that we live in.
28. Over the past century what has happened to the Earth's temperature?
Altimetry (height)
Surface Mass Balance
Some regions of the Earth have warmed faster than other regions.
Positive
29. A dome shaped cover of perennial ice and snow.
winter
1 m/yr; 10x
In the Arctic where the air is cooler
Ice Cap
30. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ozone Hole
Sea Ice Extent is Changing in Antarctica as well
Stronger
Infrared radiation
31. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
US and precipitation
How we measure Mass Balance
Arctic Atmosphere
Rainy
32. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Atmospheric Structure
Archimedes' Principle
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
33. 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.
Thermohaline Circulation Effect
Ocean-Ice-Atmosphere Interaction
Sunspots
Global warming and hot nights?
34. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Altimetry
Ice-Albedo
Severe coastal erosion
Positive
35. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Negative
Natural Causes of Warming
How to define a heatwave
Mass Change
36. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
El Nino
Time Variable Gravity
Shortwave Length
How we measure Mass Balance
37. 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
Positive
Why the Arctic climate is special
Ice Sheets
Sublimation
38. Amount of light absorbed by surface
Altimetry Cons
50%
IN the last 2 decades what we've seen
Ice Cap
39. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
Inversion Layer Winter
Altimetry (height)
Sunspots
40. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Greenhouse Gases
Ice Sheets
La Nia
Ice in the Arctic
41. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Precipitation and High Latitudes
How a closed talik forms
75-OC
Ice Motion
42. What can cause a change in the Earth's climate balance?
Antarctica
Accumulation
Stratospheric Ozone Depletion
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
43. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
What happens with the Ozone Hole
Average radiative flux reaching the atmosphere
Ice Shelf
Atmospheric Structure
44. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Ocean water
Rainy
Warming; cooling
45. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
reduction in sea-ice
Change in vegetation generates a further feedback
Antarctica
Layers of Earth
46. Frozen +2 years - Few centimeters to 1500 m
Energy Budget
US and precipitation
Permafrost
All Greenhouse gases
47. 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
Warm
Affect Floods and Droughts
Thermohaline Circulation
Contributions to CO2 from different activities
48. 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.
reduction in sea-ice
Inversion Layer Summer
Talik
Longwave Radiation
49. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
winter
Surface Mass Balance
doubles
50. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Ice/snow
Talik
45%
Thermokarst
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