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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. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Reduction in sea-ice extent
How to define a heatwave
Types of Albedo
Sea Ice Extent is Changing in Antarctica as well
2. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
70%
Heat wave
Ice Discharge
Natural Causes of Warming
3. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Discontinuous
Thinner atmosphere
Shortwave Length
Archimedes' Principle
4. Cooler water and drought conditions.
La Nia
Grounding Lines
.7O Celsius over the past century.
What happens with the Ozone Hole
5. Permafrost- A frozen soil
Thermohaline Circulatoin
Surface Mass Balance
Grounding Lines
Frozen Soil
6. Forms in a mosaic of favoured locations.
Cause of break of inversion layers or decrease in frequency
More rain means no drought
Discontinuous Permafrosrt
Arctic Atmosphere
7. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Sea ice melt does not change sea level
Warm
Ice loss
Grounding Lines
8. he increase of ozone concentration in the atmosphere helps ____ our planet
Albedo
Frozen Soil
Warm
.75OC/km-1
9. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Closed talik
Ice Cap
Albedo
Depth v Surface
10. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Ice in the Arctic
Average radiative flux reaching the atmosphere
Agricultural Drought
Frozen Soil
11. CO2 GHG forcing - H2O - dominant/major GHG
The cryosphere
Deep tropics between 15O N and 15 O S are quite
45%
GHG
12. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ice Motion
Stronger
Sea-Ice Albedo
Ice loss
13. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
Methane
La Nia
Thermokarst
14. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Agricultural Drought
Atlantic Thermohaline Circulation
Types of Albedo
15. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Inversion Layer (feedback)
Contributions to CO2 from different activities
Natural Causes of Warming
Cause of break of inversion layers or decrease in frequency
16. High vs low
Cloud Feedbacks
El Nio is in the coasts of...
Antarctica
More rain means no drought
17. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
7%
Ice-Ocean Interactions
Energy Budget
18. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Thermohaline Circulation
Atmospheric Composition
Ice/snow
Thermohaline Circulation Effect
19. Total absorbed solar radiation
70%
Importance of ice sheets
20%
Mass Change
20. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Some regions of the Earth have warmed faster than other regions.
How the cryosphere is affected by climate change
Negative Ice-Albedo Feedback
21. 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.
Why ice-albedo feedback is a big deal in the Arctic
Ice loss
Ice-Albedo
Negative Ice-Albedo Feedback
22. 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
Affect Floods and Droughts
Antarctica
Contributions to CO2 from different activities
How the cryosphere is affected by climate change
23. Precipitation intensity will rise ___ for every 1 OC of warming.
air can warm dramatically
70%
Ice loss
7%
24. Descending Air dry - Convection cells are wet.
Through talik
Atmospheric Circulation
Thermohaline Circulation
Negative
25. 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.
Black Carbon
Permafrost Degradation
Major distinction between Kyoto Protocol and Convention
Climate Change in the Arctic
26. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Nitrous Oxide (N2O)
Heat wave
IPCC
Through talik
27. Set up in 1988 by WMO and UNEP.
How the cryosphere is affected by climate change
Severe coastal erosion
Albedo
IPCC
28. 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
Thermohaline Circulation
Cause of break of inversion layers or decrease in frequency
Ice Sheets
Active Layer
29. How much is the planet really warming?
30%
Air pollution
How talik forms under lakes
.7O Celsius over the past century.
30. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Reduction in sea-ice extent
Negative
Altimetry
Ozone Hole
31. CO2 - CH4 - O3 - H2O - N2O - CFCs
50%
Questions to think about
All Greenhouse gases
Depth v Surface
32. 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.
Altimetry Pros
70%
Changes in Arctic sea-ice Extent
Ozone Hole
33. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Active Layer
Thickness of the active layer and the permafrost depend on this
Thermokarst Lake
Ocean-Ice-Atmosphere Interaction
34. Reduction of Summer Sea- 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 - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Positive
Reduction in sea-ice extent
7%
Altimetry (height)
35. LW - SW - 55% absorbed by surface
Warm
Energy Budget
Discontinuous
% of Greenhouse Gases
36. 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
Effect of Deforestation on CO-2
What happens with the Ozone Hole
Dynamic thinning
Depth v Surface
37. 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
Indirect heat wave effect
Wetter; drier
Normal condition for air
Ozone Hole
38. Water vapor means more water up in the clouds and less in the ground!
Radiative Forcing
More rain means no drought
Inversion Layer Summer
Atmospheric Composition?
39. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Closed talik
Atmospheric Structure
Sea Ice
Thickness of the active layer and the permafrost depend on this
40. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Grounding Lines
Black Carbon
Contributions to CO2 from different activities
Average radiative flux reaching the atmosphere
41. Rainy on yearly average. In these regions - rising air predominates.
Stronger
Deep tropics between 15O N and 15 O S are quite
Energy Budget
Ocean-Ice-Atmosphere Interaction
42. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Thickness of the active layer and the permafrost depend on this
Change in vegetation generates a further feedback
El Nio is in the coasts of...
Dry
43. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Sea Ice Extent is Changing in Antarctica as well
Ozone
Surface Mass Balance
Agricultural Drought
44. 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%
Ice Discharge
Albedos of Snow and Ice
Thickness of the active layer and the permafrost depend on this
Absolute thresholds
45. Number of days when temperatures climb above average by a fixed amount.
Atmospheric Composition
Threshold departures
Amount of light actually reaching the Earth
doubles
46. Greenhouse gases are mixed in the ____
Thermokarst
Through talik
Ocean water
Troposphere
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
Stronger
La Nia
Absolute thresholds
Thermohaline Circulation
48. 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.
Altimetry
Absolute thresholds
Altimetry Pros
Change in vegetation generates a further feedback
49. US is responsible for ___ of the total CO2
Arctic Atmosphere
Inversion Layer Summer
30%
45%
50. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
Thermokarst
Effect of Deforestation on CO-2
Ice Shelf
La Nia