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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. Radiation absorbed by atmospheric greenhouse gases?
Why the Arctic climate is special
Ozone Hole
Ice Shelf
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
2. Where does the ozone protect us?
In the stratosphere.
1 m/yr; 10x
Thermokarst
Ocean water
3. 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
Methane
Monthly maximums and minimums
70%
4. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
Atlantic Thermohaline Circulation
How the cryosphere is affected by climate change
air can warm dramatically
Ozone
5. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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6. Forms in a mosaic of favoured locations.
Sea ice melt does not change sea level
Discontinuous Permafrosrt
How a closed talik forms
Cloud Feedbacks
7. 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
Reduction in sea-ice extent
Importance of ice sheets
Thinner atmosphere
Thickness of the active layer and the permafrost depend on this
8. 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
Dynamic thinning
Thermokarst Lake
.75OC/km-1
Why ice-albedo feedback is a big deal in the Arctic
9. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Arctic Atmosphere
Atmospheric Circulation
Monthly maximums and minimums
10. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
How we measure Mass Balance
% of Greenhouse Gases
Why ice-albedo feedback is a big deal in the Arctic
11. x7 smaller - 7m total sea level equivalent.
How a closed talik forms
Greenland
70%
Why the Arctic climate is special
12. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Ocean water
Infrared radiation
winter
13. 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
Permafrost
Affect Floods and Droughts
US and precipitation
Grounding Lines
14. 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.
Negative Ice-Albedo Feedback
Indirect heat wave effect
Ice shelf
Sea-Ice Albedo
15. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Atlantic Thermohaline Circulation
Surface Mass Balance
25%
Archimedes' Principle
16. Number of days when temperatures climb above average by a fixed amount.
Ice-Albedo
Threshold departures
Why the Arctic climate is special
Amount of light actually reaching the Earth
17. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Sea-Ice Albedo
Monthly maximums and minimums
La Nia
Cause of break of inversion layers or decrease in frequency
18. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Major distinction between Kyoto Protocol and Convention
Heat Source and Pressure
Ice Discharge
La Nia
19. 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
Ocean water
Rainy
Today melting ice
Radiative Flux
20. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Monthly maximums and minimums
Methane
Radiative Forcing
Positive feedbacks both found in...
21. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Questions to think about
Calving
Atmospheric Composition
22. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
IPCC
Percentile departures
US and precipitation
Effect of Deforestation on CO-2
23. Number of days that exceed a given temperature
Questions to think about
Absolute thresholds
45%
Ice-Ocean Interactions
24. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Major distinction between Kyoto Protocol and Convention
Ice Sheets
Agricultural Drought
Atmospheric Composition
25. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Atmospheric Structure
Thermokarst Lake
Precipitation and High Latitudes
Global warming and hot nights?
26. Over the past century what has happened to the Earth's temperature?
Cause of break of inversion layers or decrease in frequency
Negative
Some regions of the Earth have warmed faster than other regions.
Altimetry
27. 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
Heat Source and Pressure
Ocean-Ice-Atmosphere Interaction
Normal condition for air
In the Arctic where the air is cooler
28. US is responsible for ___ of the total CO2
Thermokarst
Discontinuous Permafrosrt
Albedo
30%
29. Number of days that land among the hottest of all days in that month's long-term record.
75-OC
Percentile departures
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Affect Floods and Droughts
30. Land Based Ecosystems retain ____ CO2.
Inversion Layer (feedback)
30%
Ocean water
Sea ice melt does not change sea level
31. 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
Earth's tilt
What happens with the Ozone Hole
50%
Through talik
32. Melting Point decreases
Infrared radiation
.75OC/km-1
How a closed talik forms
Major distinction between Kyoto Protocol and Convention
33. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
20%
Sunspots
El Nio is in the coasts of...
Ice loss
34. Volcanic eruptions - Sunspots - Wobbly Earth
Increases - decreases
Black Carbon
Natural Causes of Warming
50%
35. 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
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
US and precipitation
36. 1.4 USA - 57 m total sea level equivalent
Heat wave
Greenhouse Gases
Types of Albedo
Antarctica
37. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
.7O Celsius over the past century.
Contributions to CO2 from different activities
Ozone
Ice/snow
38. 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.
How we measure Mass Balance
Infrared radiation
Ice loss
Ocean-Ice-Atmosphere Interaction
39. The amount of light reflected by an object.
Troposphere
% of Greenhouse Gases
Talik
Albedo
40. The buoyant force is equal to the weight of the displaced water.
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41. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
Normal condition for air
Arctic Atmosphere
Melt
In the Arctic where the air is cooler
42. Like weighing oneself on the scale.
Time Variable Gravity
More rain means no drought
Atmospheric Circulation
Earth's tilt
43. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
Thermokarst
Mass Change
Albedos of Snow and Ice
44. How much is the planet really warming?
Importance of ice sheets
Thermohaline Circulation
Monthly maximums and minimums
.7O Celsius over the past century.
45. The order of 1 m/year. Melting is ten times more.
Surface Mass Balance
What effects the density
Global warming and hot nights?
Precipitation and High Latitudes
46. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
What happens with the Ozone Hole
Meteorological Drought
Sea Ice Extent is Changing in Antarctica as well
Heat wave
47. 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.
Atmospheric Composition?
Indirect heat wave effect
7%
Sea Ice
48. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Heat Source and Pressure
Ocean water
Severe coastal erosion
Why Water Vapor is not a climate forcing
49. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Thinner atmosphere
Atmospheric Composition?
Thermohaline Circulation
Greenland
50. A dome shaped cover of perennial ice and snow.
Ice loss
Ice Cap
Altimetry Cons
Increases - decreases