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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. Reduction of snow and ice cover - Changes in atmospheric circulation.
Cause of break of inversion layers or decrease in frequency
7%
Negative
Agricultural Drought
2. 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
How we measure Mass Balance
.75OC/km-1
Sunspots
3. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Accumulation
Heat wave
In the troposphere that we live in.
4. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Mass Budget
La Nia
Arctic Atmosphere
Precipitation and High Latitudes
5. 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%
Mass Balance
Absolute thresholds
Albedos of Snow and Ice
Infrared radiation
6. 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
Warming; cooling
Infrared radiation
Surface Mass Balance
Mass Change
7. High vs low
What effects the density
What happens with the Ozone Hole
Cloud Feedbacks
Ice/snow
8. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Negative Ice-Albedo Feedback
Open talik
Air pollution
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
9. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Threshold departures
Ice Shelf
Layers of Earth
Ice Sheets
10. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
doubles
7%
Atmospheric Structure
Negative
11. Greenhouse gases are a ___ portion of the atmosphere
Ocean-Ice-Atmosphere Interaction
Stronger
Average radiative flux reaching the atmosphere
Very small portion
12. 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.
Surface Mass Balance
Greenhouse Gases
IN the last 2 decades what we've seen
Melt
13. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Dry
Albedo
Air pollution
Radiative Flux
14. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Arctic Atmosphere
IN the last 2 decades what we've seen
Permafrost
15. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Mass Balance
Ocean water
Ocean-Ice-Atmosphere Interaction
El Nio is in the coasts of...
16. Where does the ozone protect us?
Positive feedbacks both found in...
Positive
In the stratosphere.
Grounding Lines
17. Amount of light absorbed by surface
50%
% of Greenhouse Gases
What effects the density
Thermohaline Circulation Effect
18. 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
Ice Sheets
GHG
Carbon Dioxide
19. 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.
Climate Change in the Arctic
winter
In the troposphere that we live in.
50%
20. ~15% of incident solar energy (albedo 85)
Affect Floods and Droughts
Nitrous Oxide (N2O)
Altimetry Pros
Snow and snow covered ice absorb
21. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Questions to think about
Some parts of the planet are dry because of their location
Thermokarst
Carbon Dioxide
22. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Very small portion
Mass Balance
Sunspots
Today melting ice
23. Like weighing oneself on the scale.
Albedos of Snow and Ice
Time Variable Gravity
Closed talik
Thermokarst
24. x7 smaller - 7m total sea level equivalent.
Altimetry
Precipitation and High Latitudes
Greenland
Ozone Hole
25. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
What effects the density
Ocean water
IPCC
Air pollution
26. 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
Permafrost
Grounding v Surface Melting
Why the Arctic climate is special
doubles
27. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Ice shelf
Atmospheric Structure
Ice Discharge
28. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
How talik forms under lakes
Positive feedbacks both found in...
Average radiative flux reaching the atmosphere
How a closed talik forms
29. The amount of light reflected by an object.
Black Carbon
Amount of light actually reaching the Earth
Albedo
Frozen Soil
30. Amount of light absorbed by atmosphere
20%
How to define a heatwave
Thermohaline Circulatoin
Black Carbon
31. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Monthly maximums and minimums
El Nino
What effects the density
Longwave Radiation
32. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Types of Albedo
Global warming and hot nights?
Sunspots
Ocean water
33. Number of days when temperatures climb above average by a fixed amount.
Depth v Surface
Threshold departures
Altimetry (height)
GHG
34. 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
Once every 4 years.
Agricultural Drought
Ice Shelf
Precipitation and High Latitudes
35. In ________- inversion layer is more common in the Arctic
Melt
Earth's tilt
Severe coastal erosion
winter
36. O Climate change in the Arctic is occurring now - Changes have been huge already
Is precipitation around the world increasing?
Ice Sheets
Thermohaline Circulation
Today melting ice
37. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Ice Sheets
Why Water Vapor is not a climate forcing
Severe coastal erosion
38. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Warm
Grounding Lines
Atmospheric Composition?
Energy Budget
39. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Radiative Forcing
Ice-Albedo
Thinner atmosphere
Atmospheric Composition
40. 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
Positive feedbacks both found in...
Albedos of Snow and Ice
Thermohaline Circulation
Sunspots
41. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Permafrost
Cause of break of inversion layers or decrease in frequency
Shortwave Length
All Greenhouse gases
42. How often does El Nio occur?
Meteorological Drought
Monthly maximums and minimums
Warming; cooling
Once every 4 years.
43. Rainy on yearly average. In these regions - rising air predominates.
Dynamic thinning
What happens with the Ozone Hole
Ice Shelf
Deep tropics between 15O N and 15 O S are quite
44. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
IN the last 2 decades what we've seen
Ozone Hole
winter
45. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Stronger
Frozen Soil
Increases - decreases
Ice Sheets
46. 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
air can warm dramatically
Today melting ice
IN the last 2 decades what we've seen
47. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Thermohaline Circulation Effect
Albedos of Snow and Ice
Ice Motion
Ice loss
48. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Stronger
30%
Permafrost
Ice Sheets
49. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Deep tropics between 15O N and 15 O S are quite
Increases - decreases
Types of Albedo
50. Unfrozen ground that is found within a mass of permafrost
Once every 4 years.
Atmospheric Composition?
Closed talik
Average radiative flux reaching the atmosphere