SUBJECTS
|
BROWSE
|
CAREER CENTER
|
POPULAR
|
JOIN
|
LOGIN
Business Skills
|
Soft Skills
|
Basic Literacy
|
Certifications
About
|
Help
|
Privacy
|
Terms
|
Email
Search
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. Permafrost- A frozen soil
Precipitation and High Latitudes
Effect of Deforestation on CO-2
Cloud Feedbacks
Frozen Soil
2. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Radiative Flux
Ice Sheets
Affect Floods and Droughts
Sea Ice
3. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Antarctica
Carbon Dioxide
Ocean-Ice-Atmosphere Interaction
Is precipitation around the world increasing?
4. Unfrozen ground that is found within a mass of permafrost
Sublimation
In the Arctic where the air is cooler
Closed talik
Radiative Flux
5. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
How to define a heatwave
Changes in Arctic sea-ice Extent
Wetter; drier
Heat wave
6. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Sea Ice
Heat Source and Pressure
Some parts of the planet are dry because of their location
Black Carbon
7. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Thermohaline Circulation Effect
How a closed talik forms
Contributions to CO2 from different activities
Severe coastal erosion
8. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
How we measure Mass Balance
Ice Sheets
Archimedes' Principle
9. 1.4 USA - 57 m total sea level equivalent
Active Layer
How the cryosphere is affected by climate change
Antarctica
Stratospheric Ozone Depletion
10. 240 w/m squared
Albedo
Ocean water
Amount of light actually reaching the Earth
Calving
11. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Dry
75-OC
Albedos of Snow and Ice
Altimetry Cons
12. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Grounding Lines
Ice absorbs
Mass Change
In the troposphere that we live in.
13. Greenhouse gases are mixed in the ____
Questions to think about
Troposphere
Ice Motion
Deep tropics between 15O N and 15 O S are quite
14. 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
The Ozone Hole
Ice Sheets
How we measure Mass Balance
In the troposphere that we live in.
15. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Thermohaline Circulation
Cause of break of inversion layers or decrease in frequency
Ice in the Arctic
Greenland
16. 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
20%
Why the Arctic climate is special
Antarctica
Grounding Lines
17. 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
Antarctica
Thermohaline Circulation
Talik
Thermokarst
18. Total absorbed solar radiation
Atmospheric Composition
Ice/snow
70%
Hydrological Drought
19. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Talik
Surface Mass Balance
Energy Budget
Increases - decreases
20. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
The Ozone Hole
20%
Heat Source and Pressure
21. Over the past century what has happened to the Earth's temperature?
Altimetry Cons
Thickness of the active layer and the permafrost depend on this
Some regions of the Earth have warmed faster than other regions.
Inversion Layer Summer
22. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Sea Ice Extent is Changing in Antarctica as well
Arctic Atmosphere
Rainy
Ice/snow
23. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Mass Balance
Surface Mass Balance
Indirect heat wave effect
45%
24. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Discontinuous
Dynamic thinning
Why Water Vapor is not a climate forcing
In the stratosphere.
25. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Grounding v Surface Melting
Greenland
Negative
Thinner atmosphere
26. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Climate Change in the Arctic
Methane
Calving
Agricultural Drought
27. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Ice Motion
reduction in sea-ice
Atmospheric Structure
28. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Some regions of the Earth have warmed faster than other regions.
How to define a heatwave
Heat wave
Dry
29. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
What happens with the Ozone Hole
Thermokarst
The cryosphere
30. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
US and precipitation
Threshold departures
Time Variable Gravity
Discontinuous
31. US is responsible for ___ of the total CO2
30%
Meteorological Drought
Natural Causes of Warming
Depth v Surface
32. Set up in 1988 by WMO and UNEP.
IPCC
Absolute thresholds
El Nio is in the coasts of...
Hydrological Drought
33. 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.
Sea-Ice Albedo
Greenhouse Gases
Ice-Ocean Interactions
Thickness of the active layer and the permafrost depend on this
34. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Longwave Radiation
Ice/snow
Air pollution
Ice Sheets
35. Number of days when temperatures climb above average by a fixed amount.
30%
Air pollution
Threshold departures
In the troposphere that we live in.
36. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Ice Cap
Open talik
El Nio is in the coasts of...
Ice Sheets
37. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Thickness of the active layer and the permafrost depend on this
Carbon Dioxide
Ice in the Arctic
The cryosphere
38. Really measures volume.
Ozone Hole
Ocean water
What effects the density
Altimetry
39. ~15% of incident solar energy (albedo 85)
Ice Discharge
Snow and snow covered ice absorb
Accumulation
Atmospheric Structure
40. Descending Air dry - Convection cells are wet.
Atmospheric Circulation
Monthly maximums and minimums
Inversion Layer (feedback)
Change in vegetation generates a further feedback
41. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Importance of ice sheets
Cloud Feedbacks
Ice Motion
Wetter; drier
42. Like weighing oneself on the scale.
Time Variable Gravity
Dynamic thinning
Black Carbon
Atmospheric Circulation
43. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Thermokarst
Increases - decreases
Cause of break of inversion layers or decrease in frequency
Energy Budget
44. 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.
El Nio is in the coasts of...
Radiative Flux
Ice Sheets
What effects the density
45. Reduction of Summer Sea- will increase the warming because less energy will be reflected back to the atmosphere by the ice and more will be absorbed by the ocean - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Stratospheric Ozone Depletion
Atmospheric Structure
Reduction in sea-ice extent
Closed talik
46. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Grounding Lines
Thermokarst
Ozone Hole
Monthly maximums and minimums
47. Is not an externally imposed perturbation to the climate system.
1 m/yr; 10x
What effects the density
Affect Floods and Droughts
Why Water Vapor is not a climate forcing
48. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
The cryosphere
Today melting ice
Thermohaline Circulatoin
Why Water Vapor is not a climate forcing
49. 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
Thermohaline Circulation
Archimedes' Principle
Wetter; drier
summer
50. The buoyant force is equal to the weight of the displaced water.