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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. 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.
What effects the density
Thermohaline Circulation Effect
Importance of ice sheets
Reduction in sea-ice extent
2. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
.75OC/km-1
The Ozone Hole
Thinner atmosphere
Grounding v Surface Melting
3. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Ice in the Arctic
El Nio is in the coasts of...
Earth's tilt
In the troposphere that we live in.
4. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Altimetry (height)
Thermokarst
reduction in sea-ice
Air pollution
5. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Once every 4 years.
Layers of Earth
How talik forms under lakes
US and precipitation
6. 240 w/m squared
Amount of light actually reaching the Earth
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Active Layer
El Nino
7. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Average radiative flux reaching the atmosphere
Ocean water
Once every 4 years.
Active Layer
8. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Ozone
Ice Discharge
Layers of Earth
Radiative Forcing
9. 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
Natural Causes of Warming
Why ice-albedo feedback is a big deal in the Arctic
Air pollution
Why the Arctic climate is special
10. In ________- inversion layer is more common in the Arctic
winter
Ice in the Arctic
Depth v Surface
Where rise in OC is greatest
11. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Questions to think about
20%
Monthly maximums and minimums
12. Amount of light absorbed by surface
Greenhouse Gases
What effects the density
50%
air can warm dramatically
13. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Air pollution
Atmospheric Structure
14. 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
Nitrous Oxide (N2O)
Sea Ice Extent is Changing in Antarctica as well
Ozone Hole
Thermohaline Circulation
15. The order of 1 m/year. Melting is ten times more.
Ice-Ocean Interactions
Radiative Flux
Ice Cap
Surface Mass Balance
16. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Global warming and hot nights?
Ozone Hole
Methane
Atmospheric Circulation
17. 10 : 1 - grounding ; surface
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Thermohaline Circulation
70%
Grounding v Surface Melting
18. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Warm
More rain means no drought
Methane
Dynamic thinning
19. 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.
Ice loss
Natural Causes of Warming
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Dynamic thinning
20. 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.
Antarctica
7%
Greenhouse Gases
Altimetry Pros
21. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Thermokarst
Discontinuous Permafrosrt
Ice Sheets
Some regions of the Earth have warmed faster than other regions.
22. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Thermohaline Circulatoin
Time Variable Gravity
70%
The cryosphere
23. How often does El Nio occur?
Ocean water
Altimetry (height)
Once every 4 years.
Thermohaline Circulation Effect
24. Greenhouse gases are mixed in the ____
Troposphere
Global warming and hot nights?
Agricultural Drought
Albedos of Snow and Ice
25. 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
Ice Sheets
Normal condition for air
Importance of ice sheets
Thermokarst Lake
26. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
Ice Discharge
Surface Mass Balance
Nitrous Oxide (N2O)
27. Unfrozen ground that is found within a mass of permafrost
Why the Arctic climate is special
Closed talik
Dry
El Nino
28. Cooler water and drought conditions.
Antarctica
Change in vegetation generates a further feedback
La Nia
Thermokarst
29. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Permafrost Degradation
Grounding Lines
Contributions to CO2 from different activities
50%
30. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Arctic Atmosphere
Thermokarst
Sea Ice
25%
31. Warming- positive feedback - Cooling- negative feedback.
Accumulation
Ice-Albedo
Why ice-albedo feedback is a big deal in the Arctic
Severe coastal erosion
32. High vs low
Cloud Feedbacks
Normal condition for air
Positive
Reduction in sea-ice extent
33. 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
30%
Active Layer
25%
Radiative Flux
34. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Shortwave Length
Affect Floods and Droughts
US and precipitation
Troposphere
35. Longwave radiation - any radiation with a long wave will heat up quickly.
Monthly maximums and minimums
Ocean water
Archimedes' Principle
Infrared radiation
36. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Air pollution
Discontinuous
reduction in sea-ice
Carbon Dioxide
37. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
reduction in sea-ice
IPCC
Hydrological Drought
38. Volcanic eruptions - Sunspots - Wobbly Earth
What effects the density
20%
Albedo
Natural Causes of Warming
39. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Ice Shelf
Ozone Hole
Black Carbon
40. Ice sheets have a very ____ Albedo
Strong
Radiative Flux
Snow and snow covered ice absorb
Thermohaline Circulation Effect
41. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat Source and Pressure
Heat wave
30%
Ocean water
42. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Mass Change
Dry
Through talik
43. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
.7O Celsius over the past century.
Ocean-Ice-Atmosphere Interaction
Grounding Lines
How to define a heatwave
44. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Meteorological Drought
Percentile departures
IPCC
Sublimation
45. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Thermohaline Circulation Effect
Permafrost
Stratospheric Ozone Depletion
US and precipitation
46. 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
Ice loss
In the Arctic where the air is cooler
Mass Budget
Ice-Albedo
47. Descending Air dry - Convection cells are wet.
Positive feedbacks both found in...
Mass Balance
1 m/yr; 10x
Atmospheric Circulation
48. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Ice-Albedo
Inversion Layer Winter
Ozone Hole
49. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Greenhouse Gases
Thermohaline Circulation
Severe coastal erosion
Atmospheric Composition?
50. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Natural Causes of Warming
Frozen Soil
Why ice-albedo feedback is a big deal in the Arctic