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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. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
How to define a heatwave
How we measure Mass Balance
doubles
30%
2. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Mass Budget
Stronger
Energy Budget
Rainy
3. Where does the ozone protect us?
Ice Sheets
In the stratosphere.
Importance of ice sheets
El Nio is in the coasts of...
4. In ________- inversion layer is more common in the Arctic
El Nino
Permafrost Degradation
winter
Warm
5. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Troposphere
US and precipitation
Ice Sheets
Ice Discharge
6. Ice sheets have a very ____ Albedo
Sea Ice
Negative Ice-Albedo Feedback
Ice Shelf
Strong
7. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Cloud Feedbacks
70%
Dynamic thinning
Deep tropics between 15O N and 15 O S are quite
8. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Dynamic thinning
20%
In the Arctic where the air is cooler
Sublimation
9. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Archimedes' Principle
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thermohaline Circulatoin
Wetter; drier
10. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Open talik
Calving
Layers of Earth
What effects the density
11. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Methane
Atmospheric Composition?
IN the last 2 decades what we've seen
Positive feedbacks both found in...
12. 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
El Nino
Ice Sheets
Absolute thresholds
Precipitation and High Latitudes
13. Industrial product - 300 ppb (parts per billion)
Troposphere
winter
Climate Change in the Arctic
Nitrous Oxide (N2O)
14. 1.4 USA - 57 m total sea level equivalent
Active Layer
Increases - decreases
Albedos of Snow and Ice
Antarctica
15. 240 w/m squared
Depth v Surface
Layers of Earth
Amount of light actually reaching the Earth
Ice Sheets
16. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Today melting ice
In the troposphere that we live in.
Ocean-Ice-Atmosphere Interaction
7%
17. 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.
Altimetry
Ice Shelf
Earth's tilt
Some regions of the Earth have warmed faster than other regions.
18. 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.
What effects the density
Indirect heat wave effect
Grounding v Surface Melting
How a closed talik forms
19. High vs low
All Greenhouse gases
75-OC
Cloud Feedbacks
Closed talik
20. The buoyant force is equal to the weight of the displaced water.
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21. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Ozone
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Warm
Severe coastal erosion
22. 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
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Negative Ice-Albedo Feedback
Atmospheric Composition?
In the Arctic where the air is cooler
23. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Albedos of Snow and Ice
Atmospheric Structure
Ice absorbs
Precipitation and High Latitudes
24. 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:
Effect of Deforestation on CO-2
How to define a heatwave
Thermohaline Circulation
Once every 4 years.
25. 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.
More rain means no drought
Thermohaline Circulation
Sea Ice
Change in vegetation generates a further feedback
26. 10 : 1 - grounding ; surface
Ozone Hole
Once every 4 years.
Grounding v Surface Melting
Active Layer
27. 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.
Grounding Lines
Heat Source and Pressure
% of Greenhouse Gases
Greenhouse Gases
28. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
Thermohaline Circulation Effect
Strong
More rain means no drought
29. Number of days that land among the hottest of all days in that month's long-term record.
Sublimation
Layers of Earth
Percentile departures
Climate Change in the Arctic
30. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Infrared radiation
Discontinuous
Why the Arctic climate is special
Active Layer
31. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Atlantic Thermohaline Circulation
Black Carbon
30%
Permafrost
32. 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) -
air can warm dramatically
Accumulation
30%
Normal condition for air
33. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Melt
Grounding v Surface Melting
Ice Shelf
34. 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
Threshold departures
Wetter; drier
Thinner atmosphere
Sunspots
35. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Altimetry (height)
The Ozone Hole
Antarctica
Precipitation and High Latitudes
36. 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.
Inversion Layer (feedback)
Today melting ice
Troposphere
Thermokarst
37. Over the past century what has happened to the Earth's temperature?
Ice Discharge
How the cryosphere is affected by climate change
Some regions of the Earth have warmed faster than other regions.
Sea Ice
38. Amount of light absorbed by atmosphere
How talik forms under lakes
All Greenhouse gases
Atmospheric Circulation
20%
39. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
summer
% of Greenhouse Gases
Grounding Lines
air can warm dramatically
40. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Albedo
Depth v Surface
20%
41. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Surface Mass Balance
Contributions to CO2 from different activities
Heat wave
30%
42. 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
Climate Change in the Arctic
Thermohaline Circulation Effect
Reduction in sea-ice extent
Importance of ice sheets
43. Unfrozen ground that is found within a mass of permafrost
Surface Mass Balance
Dry
Closed talik
Ice/snow
44. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Thickness of the active layer and the permafrost depend on this
Mass Change
Precipitation and High Latitudes
45. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Positive
What effects the density
Albedos of Snow and Ice
Sea Ice
46. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Agricultural Drought
Open talik
Ice absorbs
Mass Budget
47. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Why Water Vapor is not a climate forcing
Ice loss
Archimedes' Principle
48. 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
More rain means no drought
Atmospheric Structure
How the cryosphere is affected by climate change
Methane
49. LW - SW - 55% absorbed by surface
Grounding Lines
.75OC/km-1
Energy Budget
Melt
50. The order of 1 m/year. Melting is ten times more.
Climate Change in the Arctic
Average radiative flux reaching the atmosphere
Surface Mass Balance
Albedos of Snow and Ice