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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. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Longwave Radiation
More rain means no drought
Talik
Ozone Hole
2. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Indirect heat wave effect
Types of Albedo
Earth's tilt
3. 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-Albedo
Agricultural Drought
Inversion Layer Summer
Normal condition for air
4. Water vapor means more water up in the clouds and less in the ground!
Shortwave Length
Discontinuous Permafrosrt
Positive feedbacks both found in...
More rain means no drought
5. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Why ice-albedo feedback is a big deal in the Arctic
How we measure Mass Balance
Sea Ice Extent is Changing in Antarctica as well
Air pollution
6. High cloud has a _____ effect and cool cloud has a ____ effect
50%
Warming; cooling
Percentile departures
Deep tropics between 15O N and 15 O S are quite
7. The past climate...for this reason - both keep good records of climate change.
Mass Balance
Stronger
Thickness of the active layer and the permafrost depend on this
In the stratosphere.
8. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Absolute thresholds
Effect of Deforestation on CO-2
Mass Balance
Ozone Hole
9. 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
Why the Arctic climate is special
Thermohaline Circulation
Why ice-albedo feedback is a big deal in the Arctic
Altimetry (height)
10. Atmosphere retains ____ CO2
Depth v Surface
Melt
45%
.7O Celsius over the past century.
11. How much is the planet really warming?
.7O Celsius over the past century.
What effects the density
Troposphere
Heat Source and Pressure
12. Antarctica - stratosphere - Sep-Oct
Ozone Hole
In the stratosphere.
Changes in Arctic sea-ice Extent
Heat wave
13. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
El Nio is in the coasts of...
1 m/yr; 10x
Some regions of the Earth have warmed faster than other regions.
Atmospheric Structure
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
Longwave Radiation
Deep tropics between 15O N and 15 O S are quite
Why the Arctic climate is special
Wetter; drier
15. In average: +1% in respect to 100 years ago.
Grounding Lines
.7O Celsius over the past century.
Percentile departures
Is precipitation around the world increasing?
16. he increase of ozone concentration in the atmosphere helps ____ our planet
Ice/snow
Warm
Major distinction between Kyoto Protocol and Convention
Climate Change in the Arctic
17. 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.
Thermohaline Circulation
Changes in Arctic sea-ice Extent
Layers of Earth
Thermokarst
18. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
How talik forms under lakes
Atmospheric Composition
Precipitation and High Latitudes
Energy Budget
19. Permafrost- A frozen soil
Frozen Soil
Meteorological Drought
Today melting ice
El Nio is in the coasts of...
20. 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
Albedo
Questions to think about
What happens with the Ozone Hole
Black Carbon
21. 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 Shelf
Ice Sheets
75-OC
Earth's tilt
22. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
How talik forms under lakes
US and precipitation
Thermohaline Circulation
23. 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
Permafrost
Time Variable Gravity
Questions to think about
Increases - decreases
24. O Climate change in the Arctic is occurring now - Changes have been huge already
Ice-Ocean Interactions
Sea Ice Extent is Changing in Antarctica as well
Today melting ice
Atmospheric Composition
25. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Infrared radiation
Surface Mass Balance
Negative Ice-Albedo Feedback
26. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Discontinuous
Grounding Lines
Heat Source and Pressure
27. CO2 - CH4 - O3 - H2O - N2O - CFCs
Rainy
Normal condition for air
La Nia
All Greenhouse gases
28. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Indirect heat wave effect
Heat wave
Thermokarst Lake
Earth's tilt
29. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Changes in Arctic sea-ice Extent
Earth's tilt
Reduction in sea-ice extent
Severe coastal erosion
30. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Dynamic thinning
Threshold departures
Stratospheric Ozone Depletion
Ice Sheets
31. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Stronger
Contributions to CO2 from different activities
Agricultural Drought
Ice Sheets
32. 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.
Altimetry Cons
Carbon Dioxide
Atlantic Thermohaline Circulation
Thermohaline Circulation Effect
33. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
El Nio is in the coasts of...
Ozone
Surface Mass Balance
Altimetry
34. Number of days that land among the hottest of all days in that month's long-term record.
Thinner atmosphere
Percentile departures
Major distinction between Kyoto Protocol and Convention
Ice Motion
35. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Sublimation
Accumulation
Heat Source and Pressure
Arctic Atmosphere
36. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Increases - decreases
Changes in Arctic sea-ice Extent
Air pollution
37. Frozen +2 years - Few centimeters to 1500 m
Surface Mass Balance
Permafrost
Ice absorbs
Climate Change in the Arctic
38. 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
Warming; cooling
Atlantic Thermohaline Circulation
50%
Altimetry Pros
39. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Permafrost Degradation
Very small portion
Today melting ice
Global warming and hot nights?
40. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
doubles
Arctic Atmosphere
Positive feedbacks both found in...
41. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Methane
summer
Atmospheric Composition?
El Nio is in the coasts of...
42. 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
Carbon Dioxide
Reduction in sea-ice extent
Albedo
La Nia
43. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Severe coastal erosion
Monthly maximums and minimums
Importance of ice sheets
Meteorological Drought
44. More common
Ice in the Arctic
Negative Ice-Albedo Feedback
Inversion Layer Winter
Ice-Albedo
45. A dome shaped cover of perennial ice and snow.
Depth v Surface
Surface Mass Balance
Ice Cap
Changes in Arctic sea-ice Extent
46. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Agricultural Drought
Meteorological Drought
In the Arctic where the air is cooler
Major distinction between Kyoto Protocol and Convention
47. Cooler water and drought conditions.
Today melting ice
Why Water Vapor is not a climate forcing
Antarctica
La Nia
48. 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.
Through talik
Climate Change in the Arctic
Troposphere
Ice loss
49. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Troposphere
Active Layer
Inversion Layer Summer
50. LW - SW - 55% absorbed by surface
Ice Shelf
Energy Budget
Precipitation and High Latitudes
Albedos of Snow and Ice