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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. CO2 - CH4 - O3 - H2O - N2O - CFCs
Talik
Increases - decreases
Thermokarst Lake
All Greenhouse gases
2. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
.75OC/km-1
Black Carbon
Climate Change in the Arctic
Affect Floods and Droughts
3. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Change in vegetation generates a further feedback
.7O Celsius over the past century.
Mass Balance
4. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Mass Balance
Archimedes' Principle
30%
Threshold departures
5. 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
Deep tropics between 15O N and 15 O S are quite
Active Layer
Thermohaline Circulation Effect
6. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
US and precipitation
winter
Albedo
7. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Changes in Arctic sea-ice Extent
Atmospheric Structure
Open talik
Grounding Lines
8. 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
Frozen Soil
Grounding v Surface Melting
Permafrost Degradation
Thermohaline Circulation
9. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Agricultural Drought
Thermohaline Circulation
Increases - decreases
Effect of Deforestation on CO-2
10. LW - SW - 55% absorbed by surface
summer
Discontinuous Permafrosrt
Thermokarst Lake
Energy Budget
11. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Active Layer
Rainy
El Nio is in the coasts of...
Sublimation
12. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Cause of break of inversion layers or decrease in frequency
Atmospheric Composition
The Ozone Hole
Mass Change
13. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Through talik
Monthly maximums and minimums
Permafrost Degradation
Shortwave Length
14. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Ice in the Arctic
Ozone Hole
What effects the density
15. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Active Layer
Hydrological Drought
Ice/snow
16. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
30%
Indirect heat wave effect
Inversion Layer (feedback)
Infrared radiation
17. 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.
Heat wave
Threshold departures
Altimetry (height)
Climate Change in the Arctic
18. 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.
7%
Altimetry Cons
Grounding v Surface Melting
Changes in Arctic sea-ice Extent
19. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
More rain means no drought
Methane
Ozone
IN the last 2 decades what we've seen
20. Amount of light absorbed by surface
50%
air can warm dramatically
Sea ice melt does not change sea level
How we measure Mass Balance
21. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Open talik
Thermokarst
Cause of break of inversion layers or decrease in frequency
22. Like weighing oneself on the scale.
Albedos of Snow and Ice
Increases - decreases
IPCC
Time Variable Gravity
23. 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.
Monthly maximums and minimums
Time Variable Gravity
What effects the density
GHG
24. 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
Grounding Lines
Shortwave Length
In the Arctic where the air is cooler
25. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
Ice in the Arctic
30%
Atmospheric Composition?
26. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Sea ice melt does not change sea level
Open talik
Contributions to CO2 from different activities
Dry
27. Total absorbed solar radiation
Mass Budget
70%
75-OC
Arctic Atmosphere
28. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Discontinuous Permafrosrt
Warming; cooling
Ice-Albedo
29. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Affect Floods and Droughts
Monthly maximums and minimums
Grounding Lines
30. O Climate change in the Arctic is occurring now - Changes have been huge already
El Nio is in the coasts of...
Stronger
Today melting ice
Change in vegetation generates a further feedback
31. Clouds 40~90% - Vegetation 10~15%
Antarctica
Types of Albedo
Global warming and hot nights?
Why ice-albedo feedback is a big deal in the Arctic
32. Unfrozen ground that is found within a mass of permafrost
Thermohaline Circulation
Ice-Albedo
Altimetry
Closed talik
33. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Nitrous Oxide (N2O)
70%
Ice absorbs
34. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Amount of light actually reaching the Earth
Positive feedbacks both found in...
All Greenhouse gases
Thermohaline Circulation Effect
35. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Atmospheric Circulation
Indirect heat wave effect
Thermokarst
Ice/snow
36. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Sea ice melt does not change sea level
Layers of Earth
Warming; cooling
Ice loss
37. 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
Sea Ice
Permafrost
Atlantic Thermohaline Circulation
Ice loss
38. 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
reduction in sea-ice
Global warming and hot nights?
Altimetry Cons
39. Melting Point decreases
Surface Mass Balance
Antarctica
.75OC/km-1
Warming; cooling
40. The Earth emits this.
Surface Mass Balance
Stratospheric Ozone Depletion
Amount of light actually reaching the Earth
Longwave Radiation
41. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Inversion Layer Winter
Troposphere
Black Carbon
.7O Celsius over the past century.
42. How often does El Nio occur?
Ice Cap
Albedo
Once every 4 years.
70%
43. A dome shaped cover of perennial ice and snow.
Ice Cap
Questions to think about
Active Layer
Methane
44. Ice sheets have a very ____ Albedo
Strong
Time Variable Gravity
Permafrost
Thermokarst
45. Number of days that exceed a given temperature
Negative Ice-Albedo Feedback
45%
Thermohaline Circulation
Absolute thresholds
46. ~10% of incident solar energy (albedo 90)
Time Variable Gravity
Ice absorbs
Grounding Lines
Mass Balance
47. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sunspots
Types of Albedo
% of Greenhouse Gases
30%
48. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
Atmospheric Structure
Average radiative flux reaching the atmosphere
Strong
49. The buoyant force is equal to the weight of the displaced water.
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183
50. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Ocean-Ice-Atmosphere Interaction
Thermokarst Lake
In the Arctic where the air is cooler
Threshold departures