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Test your basic knowledge |
Global Warming
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Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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. 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.
Dynamic thinning
Permafrost
How talik forms under lakes
The Ozone Hole
2. 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
Altimetry
Wetter; drier
Sunspots
Effect of Deforestation on CO-2
3. CO2 - CH4 - O3 - H2O - N2O - CFCs
75-OC
The cryosphere
Active Layer
All Greenhouse gases
4. The order of 1 m/year. Melting is ten times more.
Surface Mass Balance
Altimetry
Ice-Ocean Interactions
Altimetry Pros
5. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Inversion Layer Winter
What effects the density
Average radiative flux reaching the atmosphere
Deep tropics between 15O N and 15 O S are quite
6. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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7. Unfrozen ground that is found within a mass of permafrost
Warm
Affect Floods and Droughts
Closed talik
Atmospheric Circulation
8. Less frequent and weaker
Very small portion
Inversion Layer Summer
.7O Celsius over the past century.
Warming; cooling
9. LW - SW - 55% absorbed by surface
Energy Budget
IN the last 2 decades what we've seen
Ocean-Ice-Atmosphere Interaction
Greenhouse Gases
10. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Thermohaline Circulatoin
Ice Sheets
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Sea ice melt does not change sea level
11. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Atlantic Thermohaline Circulation
Ice Sheets
Nitrous Oxide (N2O)
Thermohaline Circulation
12. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Archimedes' Principle
Sunspots
Greenhouse Gases
Snow and snow covered ice absorb
13. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Ocean water
Sea ice melt does not change sea level
Melt
14. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Ice Motion
Monthly maximums and minimums
Active Layer
What happens with the Ozone Hole
15. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
In the stratosphere.
US and precipitation
Inversion Layer Winter
Some regions of the Earth have warmed faster than other regions.
16. Really measures volume.
How to define a heatwave
Thermohaline Circulation Effect
.75OC/km-1
Altimetry
17. 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
El Nino
Ice Sheets
Thermohaline Circulation Effect
Warming; cooling
18. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
Sea ice melt does not change sea level
Ice Shelf
In the Arctic where the air is cooler
Reduction in sea-ice extent
19. Land Based Ecosystems retain ____ CO2.
Snow and snow covered ice absorb
Archimedes' Principle
Ice-Ocean Interactions
30%
20. ~15% of incident solar energy (albedo 85)
What effects the density
Thermokarst Lake
Ice Sheets
Snow and snow covered ice absorb
21. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Ice in the Arctic
75-OC
Grounding Lines
Nitrous Oxide (N2O)
22. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Accumulation
El Nino
30%
23. 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 Ice-Albedo Feedback
Greenhouse Gases
Rainy
Snow and snow covered ice absorb
24. 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%
Why Water Vapor is not a climate forcing
Albedos of Snow and Ice
Discontinuous
Methane
25. In ________- inversion layer is more common in the Arctic
El Nino
winter
Average radiative flux reaching the atmosphere
Stronger
26. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Discontinuous
Ice Cap
Why ice-albedo feedback is a big deal in the Arctic
Ice absorbs
27. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
How a closed talik forms
75-OC
Surface Mass Balance
Wetter; drier
28. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Infrared radiation
Ozone
How a closed talik forms
29. Ocean retains ____ CO2
25%
75-OC
Dry
How we measure Mass Balance
30. CO2 GHG forcing - H2O - dominant/major GHG
Melt
Hydrological Drought
GHG
Methane
31. 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
Sea Ice Extent is Changing in Antarctica as well
Altimetry (height)
Why the Arctic climate is special
Grounding Lines
32. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Mass Change
Radiative Flux
Atmospheric Composition
33. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Positive
Some parts of the planet are dry because of their location
34. 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
doubles
Surface Mass Balance
.7O Celsius over the past century.
Atmospheric Composition
35. 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.
Climate Change in the Arctic
Grounding v Surface Melting
Altimetry (height)
Negative Ice-Albedo Feedback
36. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Severe coastal erosion
Methane
How the cryosphere is affected by climate change
Ozone Hole
37. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Some regions of the Earth have warmed faster than other regions.
Albedo
Permafrost Degradation
How we measure Mass Balance
38. 1.4 USA - 57 m total sea level equivalent
Threshold departures
Antarctica
Monthly maximums and minimums
Effect of Deforestation on CO-2
39. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Importance of ice sheets
Ozone Hole
Thermohaline Circulatoin
Atmospheric Structure
40. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Inversion Layer (feedback)
Sublimation
Discontinuous
41. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Black Carbon
Radiative Forcing
Mass Budget
Carbon Dioxide
42. The Earth emits this.
Ice shelf
Meteorological Drought
In the stratosphere.
Longwave Radiation
43. 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.
Ice shelf
reduction in sea-ice
20%
Major distinction between Kyoto Protocol and Convention
44. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Calving
Increases - decreases
Longwave Radiation
Mass Change
45. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Ice in the Arctic
Negative
Change in vegetation generates a further feedback
46. 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
Depth v Surface
Atmospheric Structure
Permafrost
Types of Albedo
47. 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.
Why Water Vapor is not a climate forcing
Depth v Surface
Ocean water
Thermohaline Circulatoin
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.
Change in vegetation generates a further feedback
La Nia
Negative
Very small portion
49. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
30%
How to define a heatwave
How a closed talik forms
Heat wave
50. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Methane
Precipitation and High Latitudes
Contributions to CO2 from different activities
What happens with the Ozone Hole
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