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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. 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
Why ice-albedo feedback is a big deal in the Arctic
Surface Mass Balance
Some regions of the Earth have warmed faster than other regions.
Affect Floods and Droughts
2. 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.
Warming; cooling
Ice Sheets
What effects the density
Precipitation and High Latitudes
3. Like weighing oneself on the scale.
Ice/snow
How the cryosphere is affected by climate change
Time Variable Gravity
Grounding v Surface Melting
4. Amount of light absorbed by surface
50%
Surface Mass Balance
Sea Ice Extent is Changing in Antarctica as well
Thermokarst
5. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Thermohaline Circulation
Ice in the Arctic
What effects the density
Shortwave Length
6. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Absolute thresholds
Today melting ice
Ocean water
Air pollution
7. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Shortwave Length
Surface Mass Balance
Sea Ice
Ice-Albedo
8. 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.
Frozen Soil
Ice loss
Agricultural Drought
Thermohaline Circulation
9. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Air pollution
Thinner atmosphere
Ocean-Ice-Atmosphere Interaction
Grounding Lines
10. 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.
Earth's tilt
Longwave Radiation
Percentile departures
Negative Ice-Albedo Feedback
11. Where do greenhouse gases warm up the Earth?
How to define a heatwave
Ice Discharge
In the troposphere that we live in.
Why the Arctic climate is special
12. A dome shaped cover of perennial ice and snow.
Ice Sheets
Meteorological Drought
Ice Cap
45%
13. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
Radiative Flux
Depth v Surface
Archimedes' Principle
Monthly maximums and minimums
14. Atmosphere retains ____ CO2
Thickness of the active layer and the permafrost depend on this
Discontinuous Permafrosrt
In the stratosphere.
45%
15. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Is precipitation around the world increasing?
Sea Ice Extent is Changing in Antarctica as well
Shortwave Length
Antarctica
16. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
The cryosphere
summer
Positive feedbacks both found in...
Ice Sheets
17. Land Based Ecosystems retain ____ CO2.
Stronger
30%
Albedo
Increases - decreases
18. Number of days that land among the hottest of all days in that month's long-term record.
Albedo
20%
How talik forms under lakes
Percentile departures
19. A thick - floating slab of freshwater ice extending from coast to coast.
Warm
Ice Sheets
Nitrous Oxide (N2O)
Ice shelf
20. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Energy Budget
How to define a heatwave
Ozone Hole
Types of Albedo
21. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
Is precipitation around the world increasing?
GHG
Antarctica
22. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Time Variable Gravity
Greenland
Increases - decreases
US and precipitation
23. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Ocean-Ice-Atmosphere Interaction
Snow and snow covered ice absorb
Arctic Atmosphere
24. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Accumulation
Ice Discharge
Affect Floods and Droughts
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
25. Cooler water and drought conditions.
La Nia
Very small portion
Monthly maximums and minimums
Altimetry (height)
26. Reduction of snow and ice cover - Changes in atmospheric circulation.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Cause of break of inversion layers or decrease in frequency
Why Water Vapor is not a climate forcing
Thermokarst
27. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Calving
Increases - decreases
Ice-Ocean Interactions
Permafrost
28. Forms in a mosaic of favoured locations.
Heat Source and Pressure
Discontinuous Permafrosrt
All Greenhouse gases
How we measure Mass Balance
29. Set up in 1988 by WMO and UNEP.
Global warming and hot nights?
IPCC
summer
Inversion Layer Summer
30. 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
Depth v Surface
Where rise in OC is greatest
In the Arctic where the air is cooler
Ocean water
31. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
Reduction in sea-ice extent
Ice in the Arctic
Radiative Flux
32. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
Mass Budget
Ocean water
Ocean-Ice-Atmosphere Interaction
33. 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.
Major distinction between Kyoto Protocol and Convention
What effects the density
How talik forms under lakes
Air pollution
34. Permafrost- A frozen soil
Frozen Soil
Active Layer
In the stratosphere.
Global warming and hot nights?
35. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Thermohaline Circulatoin
Sea Ice
Climate Change in the Arctic
Strong
36. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Ocean water
.75OC/km-1
Affect Floods and Droughts
Normal condition for air
37. Where does the ozone protect us?
In the stratosphere.
Dynamic thinning
Infrared radiation
Stronger
38. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Discontinuous Permafrosrt
Atmospheric Composition
In the Arctic where the air is cooler
39. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Stratospheric Ozone Depletion
Layers of Earth
Methane
40. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Inversion Layer Winter
Normal condition for air
Absolute thresholds
41. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Infrared radiation
All Greenhouse gases
Discontinuous
summer
42. Volcanic eruptions - Sunspots - Wobbly Earth
Where rise in OC is greatest
Normal condition for air
Grounding v Surface Melting
Natural Causes of Warming
43. 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.
winter
Negative
Ice Shelf
Thermohaline Circulation Effect
44. 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
Positive
Ice-Albedo
Climate Change in the Arctic
45. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Thermokarst Lake
50%
Sea Ice Extent is Changing in Antarctica as well
Ozone
46. More common
Antarctica
Agricultural Drought
Inversion Layer Winter
El Nio is in the coasts of...
47. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
Average radiative flux reaching the atmosphere
Earth's tilt
Inversion Layer Winter
48. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
The cryosphere
Thermokarst
Greenland
winter
49. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
How the cryosphere is affected by climate change
70%
US and precipitation
50. Number of days that exceed a given temperature
Absolute thresholds
Radiative Flux
Arctic Atmosphere
Types of Albedo