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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. 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 Motion
Ozone
Cause of break of inversion layers or decrease in frequency
Agricultural Drought
2. A thick - floating slab of freshwater ice extending from coast to coast.
Dynamic thinning
Ice shelf
Effect of Deforestation on CO-2
winter
3. 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.
summer
Permafrost
Thermohaline Circulation Effect
Ice-Ocean Interactions
4. 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
Thermokarst
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Depth v Surface
5. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
7%
Heat Source and Pressure
20%
Why the Arctic climate is special
6. Is not an externally imposed perturbation to the climate system.
Stratospheric Ozone Depletion
Why Water Vapor is not a climate forcing
Warm
Open talik
7. Over the past century what has happened to the Earth's temperature?
Climate Change in the Arctic
Some regions of the Earth have warmed faster than other regions.
Ozone Hole
Negative Ice-Albedo Feedback
8. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Atlantic Thermohaline Circulation
Some parts of the planet are dry because of their location
Ice/snow
9. The amount of light reflected by an object.
Albedo
The cryosphere
Importance of ice sheets
Ice Sheets
10. Reduction of snow and ice cover - Changes in atmospheric circulation.
30%
Heat wave
Cause of break of inversion layers or decrease in frequency
Thermokarst
11. Permafrost- A frozen soil
Severe coastal erosion
Thermohaline Circulation
Frozen Soil
Accumulation
12. 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.
Change in vegetation generates a further feedback
Negative Ice-Albedo Feedback
Thermohaline Circulation Effect
Monthly maximums and minimums
13. 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.
Ice Cap
Thermohaline Circulation
Severe coastal erosion
Ice Shelf
14. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Negative
Natural Causes of Warming
Ozone
Types of Albedo
15. ~15% of incident solar energy (albedo 85)
Radiative Forcing
Snow and snow covered ice absorb
Permafrost
Air pollution
16. O Unfrozen soil that stays within the permafrost.
Talik
Ice loss
Mass Change
Ice-Albedo
17. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
Surface Mass Balance
Discontinuous Permafrosrt
doubles
Indirect heat wave effect
18. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Severe coastal erosion
Dry
Ice absorbs
19. Antarctica - stratosphere - Sep-Oct
Negative
Climate Change in the Arctic
Ozone Hole
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
20. 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.
Amount of light actually reaching the Earth
% of Greenhouse Gases
Mass Change
Major distinction between Kyoto Protocol and Convention
21. Where does the ozone protect us?
In the stratosphere.
Through talik
Ice Sheets
How we measure Mass Balance
22. In ________- inversion layer is more common in the Arctic
Atlantic Thermohaline Circulation
Precipitation and High Latitudes
winter
Thermohaline Circulation Effect
23. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
30%
Altimetry (height)
Carbon Dioxide
Affect Floods and Droughts
24. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Altimetry Pros
Ozone
Snow and snow covered ice absorb
Greenhouse Gases
25. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
El Nio is in the coasts of...
Depth v Surface
Contributions to CO2 from different activities
26. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Open talik
Troposphere
More rain means no drought
27. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Radiative Forcing
Mass Balance
In the Arctic where the air is cooler
Greenland
28. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Heat wave
Where rise in OC is greatest
Sublimation
29. 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
Importance of ice sheets
Albedo
US and precipitation
50%
30. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
Percentile departures
La Nia
Methane
31. 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
30%
Why ice-albedo feedback is a big deal in the Arctic
Ozone Hole
20%
32. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Methane
Reduction in sea-ice extent
Positive feedbacks both found in...
33. Melting Point decreases
Ozone Hole
Time Variable Gravity
Greenhouse Gases
.75OC/km-1
34. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Atlantic Thermohaline Circulation
Methane
The Ozone Hole
Ice Sheets
35. 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
Absolute thresholds
Average radiative flux reaching the atmosphere
Melt
7%
36. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Positive
Today melting ice
Thermokarst Lake
Ozone Hole
37. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Active Layer
Accumulation
Stratospheric Ozone Depletion
Grounding Lines
38. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Layers of Earth
Ozone Hole
Shortwave Length
Ice Sheets
39. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Why ice-albedo feedback is a big deal in the Arctic
In the stratosphere.
Positive feedbacks both found in...
US and precipitation
40. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
Greenland
Longwave Radiation
Thermohaline Circulation
41. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Thermohaline Circulatoin
Ozone Hole
More rain means no drought
Negative
42. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Thermohaline Circulation
Why the Arctic climate is special
Sea ice melt does not change sea level
Ice absorbs
43. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Sublimation
Increases - decreases
La Nia
Greenland
44. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
75-OC
Severe coastal erosion
Accumulation
Normal condition for air
45. 10 : 1 - grounding ; surface
Grounding v Surface Melting
20%
Severe coastal erosion
How the cryosphere is affected by climate change
46. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Grounding Lines
Importance of ice sheets
Dynamic thinning
Altimetry Cons
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
How to define a heatwave
El Nio is in the coasts of...
Very small portion
Thermohaline Circulation
48. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Melt
Greenland
IN the last 2 decades what we've seen
49. 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.
20%
Antarctica
Thermohaline Circulation Effect
Mass Budget
50. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Some regions of the Earth have warmed faster than other regions.
The cryosphere
Inversion Layer Winter
Energy Budget