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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. Set up in 1988 by WMO and UNEP.
IPCC
Changes in Arctic sea-ice Extent
Atlantic Thermohaline Circulation
doubles
2. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Altimetry Pros
Once every 4 years.
Talik
3. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Energy Budget
Methane
In the Arctic where the air is cooler
Ozone Hole
4. Volcanic eruptions - Sunspots - Wobbly Earth
Ocean water
Sunspots
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Natural Causes of Warming
5. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Grounding Lines
Grounding Lines
Negative
Accumulation
6. Total absorbed solar radiation
30%
Layers of Earth
Open talik
70%
7. 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.
What happens with the Ozone Hole
Mass Change
Change in vegetation generates a further feedback
What effects the density
8. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Altimetry (height)
Absolute thresholds
Threshold departures
9. Greenhouse gases are a ___ portion of the atmosphere
Grounding Lines
Active Layer
Dry
Very small portion
10. Reduction of snow and ice cover - Changes in atmospheric circulation.
reduction in sea-ice
Cause of break of inversion layers or decrease in frequency
50%
.75OC/km-1
11. Amount of light absorbed by atmosphere
Thermohaline Circulatoin
How a closed talik forms
20%
Ozone Hole
12. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Permafrost
Air pollution
El Nio is in the coasts of...
Albedo
13. CO2 GHG forcing - H2O - dominant/major GHG
Archimedes' Principle
GHG
Ocean water
Atmospheric Composition?
14. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Melt
Warm
Contributions to CO2 from different activities
Precipitation and High Latitudes
15. How much is the planet really warming?
.7O Celsius over the past century.
Ozone Hole
Infrared radiation
Discontinuous Permafrosrt
16. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Heat wave
Inversion Layer Winter
US and precipitation
Sea ice melt does not change sea level
17. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Mass Balance
Heat wave
Altimetry (height)
In the Arctic where the air is cooler
18. 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:
Thermohaline Circulation
Permafrost
IPCC
Inversion Layer Summer
19. 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.
Thinner atmosphere
Ozone Hole
Ice Sheets
Some regions of the Earth have warmed faster than other regions.
20. Number of days that exceed a given temperature
Stratospheric Ozone Depletion
Absolute thresholds
1 m/yr; 10x
Ozone Hole
21. LW - SW - 55% absorbed by surface
Changes in Arctic sea-ice Extent
Stronger
Antarctica
Energy Budget
22. Ocean retains ____ CO2
Permafrost
Atmospheric Circulation
25%
Altimetry Pros
23. he increase of ozone concentration in the atmosphere helps ____ our planet
Thermohaline Circulatoin
Warm
75-OC
Albedo
24. 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.
Open talik
Inversion Layer (feedback)
Radiative Forcing
Surface Mass Balance
25. 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.
Thermohaline Circulation Effect
Surface Mass Balance
Precipitation and High Latitudes
Sea Ice
26. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Atmospheric Composition?
Deep tropics between 15O N and 15 O S are quite
Positive
Surface Mass Balance
27. 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.
Today melting ice
Changes in Arctic sea-ice Extent
Climate Change in the Arctic
.75OC/km-1
28. Greenhouse gases are mixed in the ____
Positive
How a closed talik forms
Permafrost
Troposphere
29. Amount of light absorbed by surface
Deep tropics between 15O N and 15 O S are quite
air can warm dramatically
El Nino
50%
30. Like weighing oneself on the scale.
Sea-Ice Albedo
Atlantic Thermohaline Circulation
Surface Mass Balance
Time Variable Gravity
31. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
How the cryosphere is affected by climate change
Grounding Lines
Monthly maximums and minimums
Thermokarst
32. 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
Layers of Earth
Shortwave Length
Once every 4 years.
Ice Sheets
33. 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%
Albedos of Snow and Ice
Sunspots
Threshold departures
30%
34. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Affect Floods and Droughts
Atmospheric Structure
Increases - decreases
Discontinuous
35. Warming- positive feedback - Cooling- negative feedback.
Altimetry Cons
Ice-Albedo
Atlantic Thermohaline Circulation
Permafrost
36. x7 smaller - 7m total sea level equivalent.
Greenhouse Gases
El Nio is in the coasts of...
Some parts of the planet are dry because of their location
Greenland
37. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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183
38. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Altimetry Pros
Increases - decreases
Atmospheric Composition?
25%
39. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Accumulation
Average radiative flux reaching the atmosphere
Sunspots
Atmospheric Structure
40. 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
How a closed talik forms
Antarctica
The cryosphere
41. 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 in the Arctic
Ice Shelf
El Nino
Indirect heat wave effect
42. More common
Thermohaline Circulation
Inversion Layer Winter
Dynamic thinning
Positive
43. The past climate...for this reason - both keep good records of climate change.
Sublimation
Thickness of the active layer and the permafrost depend on this
Ice-Albedo
Accumulation
44. ~10% of incident solar energy (albedo 90)
summer
Ice absorbs
Thermohaline Circulatoin
Ice Discharge
45. A dome shaped cover of perennial ice and snow.
Calving
Altimetry Pros
Ice Cap
Ice Sheets
46. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Nitrous Oxide (N2O)
Atlantic Thermohaline Circulation
Today melting ice
How a closed talik forms
47. The Earth emits this.
Is precipitation around the world increasing?
Longwave Radiation
Mass Budget
Negative
48. O Climate change in the Arctic is occurring now - Changes have been huge already
Accumulation
Atlantic Thermohaline Circulation
Today melting ice
Closed talik
49. 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
Mass Change
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Severe coastal erosion
Carbon Dioxide
50. 85%
US and precipitation
Antarctica
Sea-Ice Albedo
.75OC/km-1