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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. LW - SW - 55% absorbed by surface
Cloud Feedbacks
Black Carbon
Energy Budget
70%
2. 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
Radiative Flux
Altimetry Pros
Ice loss
Arctic Atmosphere
3. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Indirect heat wave effect
summer
The Ozone Hole
Nitrous Oxide (N2O)
4. ~15% of incident solar energy (albedo 85)
Warming; cooling
.75OC/km-1
Air pollution
Snow and snow covered ice absorb
5. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Absolute thresholds
Cloud Feedbacks
Ocean water
Atmospheric Composition?
6. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
US and precipitation
Ozone Hole
Questions to think about
Thermokarst
7. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Thickness of the active layer and the permafrost depend on this
air can warm dramatically
Active Layer
La Nia
8. 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.
Mass Balance
Altimetry Cons
Thermohaline Circulation Effect
Thickness of the active layer and the permafrost depend on this
9. Like weighing oneself on the scale.
Talik
Permafrost
Time Variable Gravity
Methane
10. 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.
1 m/yr; 10x
Heat wave
Climate Change in the Arctic
Inversion Layer Summer
11. A dome shaped cover of perennial ice and snow.
In the stratosphere.
Ice Cap
All Greenhouse gases
summer
12. 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 shelf
Closed talik
Radiative Forcing
13. In ________- inversion layer is more common in the Arctic
.75OC/km-1
winter
Some regions of the Earth have warmed faster than other regions.
Affect Floods and Droughts
14. Radiation absorbed by atmospheric greenhouse gases?
Hydrological Drought
Sea ice melt does not change sea level
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Surface Mass Balance
15. Ice sheets have a very ____ Albedo
20%
Strong
Shortwave Length
Sea-Ice Albedo
16. Precipitation intensity will rise ___ for every 1 OC of warming.
IPCC
7%
doubles
Is precipitation around the world increasing?
17. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Sea Ice
Dynamic thinning
Cloud Feedbacks
Monthly maximums and minimums
18. Number of days that land among the hottest of all days in that month's long-term record.
Archimedes' Principle
Percentile departures
Where rise in OC is greatest
Carbon Dioxide
19. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Positive feedbacks both found in...
Ozone
winter
How a closed talik forms
20. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Infrared radiation
Rainy
El Nio is in the coasts of...
Increases - decreases
21. 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
Sea Ice Extent is Changing in Antarctica as well
Ice Sheets
Indirect heat wave effect
22. 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
25%
Climate Change in the Arctic
Where rise in OC is greatest
Importance of ice sheets
23. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Inversion Layer Winter
Melt
Very small portion
Heat Source and Pressure
24. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Precipitation and High Latitudes
Inversion Layer Summer
How we measure Mass Balance
Why the Arctic climate is special
25. 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.
Changes in Arctic sea-ice Extent
Absolute thresholds
Indirect heat wave effect
Discontinuous Permafrosrt
26. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Ocean-Ice-Atmosphere Interaction
Through talik
Longwave Radiation
Ice-Albedo
27. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Thermokarst
Precipitation and High Latitudes
Warm
Atmospheric Composition
28. Number of days that exceed a given temperature
Absolute thresholds
Antarctica
Importance of ice sheets
Positive
29. 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
Thermohaline Circulation
summer
Ice Sheets
Deep tropics between 15O N and 15 O S are quite
30. Where do greenhouse gases warm up the Earth?
Greenland
In the troposphere that we live in.
Ozone Hole
45%
31. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Grounding Lines
How a closed talik forms
Thermohaline Circulation
Mass Balance
32. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
25%
Very small portion
Atmospheric Composition?
33. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Major distinction between Kyoto Protocol and Convention
The cryosphere
Questions to think about
Accumulation
34. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Altimetry (height)
Changes in Arctic sea-ice Extent
Inversion Layer Winter
Sea Ice Extent is Changing in Antarctica as well
35. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Closed talik
winter
Permafrost
Why ice-albedo feedback is a big deal in the Arctic
36. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Percentile departures
Atmospheric Structure
Severe coastal erosion
Depth v Surface
37. 240 w/m squared
Amount of light actually reaching the Earth
All Greenhouse gases
Heat wave
Severe coastal erosion
38. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Global warming and hot nights?
Hydrological Drought
Stronger
Ocean water
39. 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
Nitrous Oxide (N2O)
What happens with the Ozone Hole
Ice-Ocean Interactions
Active Layer
40. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
How we measure Mass Balance
Ice/snow
Methane
GHG
41. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
GHG
Average radiative flux reaching the atmosphere
Ocean-Ice-Atmosphere Interaction
Calving
42. Surface Mass Balance is of the order of _____ melting is ____ times more.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
1 m/yr; 10x
Ocean water
Sea-Ice Albedo
43. 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
Ice Discharge
Ice-Ocean Interactions
Permafrost Degradation
Why the Arctic climate is special
44. US is responsible for ___ of the total CO2
Grounding Lines
30%
Albedo
Today melting ice
45. Forms in a mosaic of favoured locations.
Air pollution
Discontinuous Permafrosrt
Warm
Ice Motion
46. The Earth emits this.
Stratospheric Ozone Depletion
Inversion Layer (feedback)
Longwave Radiation
Accumulation
47. 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
El Nino
20%
Stratospheric Ozone Depletion
Positive feedbacks both found in...
48. Atmosphere retains ____ CO2
45%
Energy Budget
Surface Mass Balance
In the troposphere that we live in.
49. Over the past century what has happened to the Earth's temperature?
Affect Floods and Droughts
Atmospheric Circulation
Albedo
Some regions of the Earth have warmed faster than other regions.
50. x7 smaller - 7m total sea level equivalent.
IN the last 2 decades what we've seen
Open talik
Greenland
GHG