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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. 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.
Heat Source and Pressure
Inversion Layer (feedback)
Thermohaline Circulation Effect
Once every 4 years.
2. O Unfrozen soil that stays within the permafrost.
More rain means no drought
GHG
Time Variable Gravity
Talik
3. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Affect Floods and Droughts
Positive
Dry
4. Where do greenhouse gases warm up the Earth?
summer
Precipitation and High Latitudes
Climate Change in the Arctic
In the troposphere that we live in.
5. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Atmospheric Circulation
Average radiative flux reaching the atmosphere
Ozone
Ice in the Arctic
6. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Thermokarst
Positive feedbacks both found in...
Discontinuous
Sea-Ice Albedo
7. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Ice-Albedo
Sunspots
Ice-Ocean Interactions
Methane
8. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Normal condition for air
How to define a heatwave
Average radiative flux reaching the atmosphere
Through talik
9. Antarctica - stratosphere - Sep-Oct
% of Greenhouse Gases
Percentile departures
Ozone Hole
Contributions to CO2 from different activities
10. 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%
Methane
Reduction in sea-ice extent
Albedos of Snow and Ice
Layers of Earth
11. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Permafrost
winter
More rain means no drought
12. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
The Ozone Hole
Negative
How to define a heatwave
Monthly maximums and minimums
13. Like weighing oneself on the scale.
7%
Sunspots
Altimetry Cons
Time Variable Gravity
14. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
The Ozone Hole
Ice Motion
Infrared radiation
Ice Sheets
15. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
More rain means no drought
The Ozone Hole
Troposphere
Grounding Lines
16. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Altimetry
Inversion Layer Winter
Severe coastal erosion
Sea Ice Extent is Changing in Antarctica as well
17. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Ice Motion
Sublimation
Increases - decreases
18. Descending Air dry - Convection cells are wet.
Sea Ice Extent is Changing in Antarctica as well
Greenhouse Gases
Atmospheric Circulation
Shortwave Length
19. 1.4 USA - 57 m total sea level equivalent
Active Layer
Antarctica
GHG
7%
20. US is responsible for ___ of the total CO2
Ice Sheets
Sea ice melt does not change sea level
50%
30%
21. 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.
El Nio is in the coasts of...
Longwave Radiation
% of Greenhouse Gases
Indirect heat wave effect
22. Precipitation intensity will rise ___ for every 1 OC of warming.
Snow and snow covered ice absorb
7%
summer
Air pollution
23. 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.
7%
Very small portion
Active Layer
How talik forms under lakes
24. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Ice loss
Atmospheric Composition
Talik
25. 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
Agricultural Drought
Indirect heat wave effect
Accumulation
Why ice-albedo feedback is a big deal in the Arctic
26. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Frozen Soil
% of Greenhouse Gases
Increases - decreases
27. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Ice Motion
Wetter; drier
Natural Causes of Warming
Dynamic thinning
28. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
Ocean water
Where rise in OC is greatest
Thermohaline Circulatoin
Radiative Forcing
29. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
El Nio is in the coasts of...
Atmospheric Structure
Grounding v Surface Melting
Melt
30. 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!
La Nia
Change in vegetation generates a further feedback
Wetter; drier
Antarctica
31. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
In the troposphere that we live in.
Inversion Layer Winter
air can warm dramatically
32. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Ice-Ocean Interactions
Negative Ice-Albedo Feedback
Calving
Thermokarst
33. Greenhouse gases are mixed in the ____
How talik forms under lakes
Air pollution
Calving
Troposphere
34. 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.
Global warming and hot nights?
Climate Change in the Arctic
Permafrost
winter
35. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Ice-Ocean Interactions
Greenhouse Gases
Surface Mass Balance
Monthly maximums and minimums
36. The Earth emits this.
Longwave Radiation
Ocean water
Troposphere
Surface Mass Balance
37. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Some regions of the Earth have warmed faster than other regions.
Ice Sheets
How a closed talik forms
Antarctica
38. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
doubles
Reduction in sea-ice extent
Hydrological Drought
Surface Mass Balance
39. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
Is precipitation around the world increasing?
Permafrost
Why ice-albedo feedback is a big deal in the Arctic
Altimetry (height)
40. 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.
Inversion Layer Winter
Once every 4 years.
reduction in sea-ice
Closed talik
41. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Longwave Radiation
Greenhouse Gases
Atmospheric Structure
Effect of Deforestation on CO-2
42. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Types of Albedo
Increases - decreases
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Active Layer
43. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Natural Causes of Warming
Inversion Layer Summer
Thermokarst
Hydrological Drought
44. Set up in 1988 by WMO and UNEP.
IPCC
Permafrost
Why ice-albedo feedback is a big deal in the Arctic
Warming; cooling
45. Ice sheets have a very ____ Albedo
Strong
Thermohaline Circulation
Ice-Ocean Interactions
Importance of ice sheets
46. The past climate...for this reason - both keep good records of climate change.
Ice-Albedo
Thickness of the active layer and the permafrost depend on this
Ice-Ocean Interactions
.75OC/km-1
47. 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.
Ice loss
Dynamic thinning
Nitrous Oxide (N2O)
Ice-Ocean Interactions
48. A dome shaped cover of perennial ice and snow.
Ice Cap
Black Carbon
Sea ice melt does not change sea level
Sunspots
49. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
50%
Archimedes' Principle
Atmospheric Structure
50. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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