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. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Average radiative flux reaching the atmosphere
Inversion Layer Summer
Cloud Feedbacks
Hydrological Drought
2. Where does the ozone protect us?
El Nino
Antarctica
Mass Change
In the stratosphere.
3. ~15% of incident solar energy (albedo 85)
Monthly maximums and minimums
Ice absorbs
Cause of break of inversion layers or decrease in frequency
Snow and snow covered ice absorb
4. 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
Reduction in sea-ice extent
Why ice-albedo feedback is a big deal in the Arctic
Warm
Ice-Albedo
5. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Thickness of the active layer and the permafrost depend on this
Severe coastal erosion
Ocean water
Warm
6. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
30%
Today melting ice
How to define a heatwave
% of Greenhouse Gases
7. Clouds 40~90% - Vegetation 10~15%
Inversion Layer Summer
Types of Albedo
How talik forms under lakes
Ocean water
8. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Longwave Radiation
Effect of Deforestation on CO-2
winter
Altimetry Pros
9. 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.
Change in vegetation generates a further feedback
Mass Change
Very small portion
Deep tropics between 15O N and 15 O S are quite
10. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Time Variable Gravity
Inversion Layer Winter
Grounding Lines
11. 85%
Sea-Ice Albedo
Affect Floods and Droughts
Natural Causes of Warming
Is precipitation around the world increasing?
12. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Once every 4 years.
Major distinction between Kyoto Protocol and Convention
Albedo
air can warm dramatically
13. 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
Thermohaline Circulation
More rain means no drought
Precipitation and High Latitudes
What happens with the Ozone Hole
14. 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:
Radiative Flux
Thermohaline Circulation
Percentile departures
Cause of break of inversion layers or decrease in frequency
15. Reduction of snow and ice cover - Changes in atmospheric circulation.
Cause of break of inversion layers or decrease in frequency
Thermohaline Circulatoin
Dry
Grounding v Surface Melting
16. Is not an externally imposed perturbation to the climate system.
Average radiative flux reaching the atmosphere
Why Water Vapor is not a climate forcing
Negative Ice-Albedo Feedback
Warm
17. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Black Carbon
Talik
Through talik
18. The amount of light reflected by an object.
Albedo
Ice in the Arctic
.7O Celsius over the past century.
Heat wave
19. ~10% of incident solar energy (albedo 90)
Some parts of the planet are dry because of their location
Ice absorbs
Dynamic thinning
Monthly maximums and minimums
20. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Threshold departures
Meteorological Drought
Increases - decreases
21. How much is the planet really warming?
.7O Celsius over the past century.
Sea ice melt does not change sea level
El Nio is in the coasts of...
20%
22. 1.4 USA - 57 m total sea level equivalent
Severe coastal erosion
Altimetry Cons
In the Arctic where the air is cooler
Antarctica
23. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Melt
70%
Sea Ice
The cryosphere
24. 10 : 1 - grounding ; surface
Black Carbon
Grounding v Surface Melting
Positive feedbacks both found in...
Ice Cap
25. US is responsible for ___ of the total CO2
winter
30%
El Nino
US and precipitation
26. How often does El Nio occur?
GHG
Altimetry (height)
Once every 4 years.
Thermohaline Circulatoin
27. Over the Northern Hemisphere than the tropics.
Thinner atmosphere
Where rise in OC is greatest
Frozen Soil
Mass Balance
28. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Change in vegetation generates a further feedback
Atmospheric Composition
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Shortwave Length
29. Amount of light absorbed by surface
In the troposphere that we live in.
25%
What happens with the Ozone Hole
50%
30. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Where rise in OC is greatest
Ice-Albedo
How to define a heatwave
Climate Change in the Arctic
31. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Ice Motion
Closed talik
Some regions of the Earth have warmed faster than other regions.
Carbon Dioxide
32. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Sea Ice Extent is Changing in Antarctica as well
IPCC
.7O Celsius over the past century.
Climate Change in the Arctic
33. Number of days when temperatures climb above average by a fixed amount.
Atlantic Thermohaline Circulation
What effects the density
Some regions of the Earth have warmed faster than other regions.
Threshold departures
34. Amount of light absorbed by atmosphere
Ice Sheets
Active Layer
20%
Atmospheric Composition?
35. 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
.75OC/km-1
Greenhouse Gases
Meteorological Drought
Why ice-albedo feedback is a big deal in the Arctic
36. Summer increase in cloud cover - Winter decrease in cloud cover.
Warning
: Invalid argument supplied for foreach() in
/var/www/html/basicversity.com/show_quiz.php
on line
183
37. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Positive feedbacks both found in...
Sea-Ice Albedo
Active Layer
7%
38. High vs low
Contributions to CO2 from different activities
Depth v Surface
Cloud Feedbacks
Grounding Lines
39. Water vapor means more water up in the clouds and less in the ground!
Greenhouse Gases
How to define a heatwave
Altimetry Cons
More rain means no drought
40. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Atmospheric Circulation
Ozone Hole
Sunspots
Thermokarst Lake
41. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
Grounding Lines
Greenland
Ozone Hole
42. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Permafrost
% of Greenhouse Gases
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
43. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Discontinuous Permafrosrt
Mass Balance
Methane
Heat Source and Pressure
44. 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
How the cryosphere is affected by climate change
% of Greenhouse Gases
Altimetry Cons
Thinner atmosphere
45. Unfrozen ground that is found within a mass of permafrost
Closed talik
Today melting ice
How we measure Mass Balance
Ocean water
46. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
25%
Stronger
Albedos of Snow and Ice
Questions to think about
47. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sunspots
Sea-Ice Albedo
45%
Inversion Layer (feedback)
48. Laser radar - H V - Long time series - high accuracy - Density
Average radiative flux reaching the atmosphere
Altimetry (height)
Reduction in sea-ice extent
Some regions of the Earth have warmed faster than other regions.
49. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Air pollution
50%
Layers of Earth
Permafrost Degradation
50. Changes over time in the highest and lowest single temperature observed during a given month of the year.
75-OC
Ice shelf
Frozen Soil
Monthly maximums and minimums