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. Laser radar - H V - Long time series - high accuracy - Density
Troposphere
Reduction in sea-ice extent
Altimetry (height)
7%
2. 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.
Troposphere
Ice loss
Air pollution
Indirect heat wave effect
3. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Contributions to CO2 from different activities
More rain means no drought
Questions to think about
Melt
4. Atmosphere retains ____ CO2
summer
How talik forms under lakes
Ice in the Arctic
45%
5. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Active Layer
Ice Sheets
reduction in sea-ice
More rain means no drought
6. Water vapor means more water up in the clouds and less in the ground!
Thickness of the active layer and the permafrost depend on this
Thermokarst
Active Layer
More rain means no drought
7. Warming- positive feedback - Cooling- negative feedback.
Increases - decreases
Ice-Albedo
Albedo
45%
8. The buoyant force is equal to the weight of the displaced water.
Warning
: Invalid argument supplied for foreach() in
/var/www/html/basicversity.com/show_quiz.php
on line
183
9. Antarctica - stratosphere - Sep-Oct
Methane
Albedos of Snow and Ice
Discontinuous
Ozone Hole
10. A dome shaped cover of perennial ice and snow.
Warming; cooling
Ice Cap
Layers of Earth
Nitrous Oxide (N2O)
11. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
7%
Antarctica
Thermohaline Circulatoin
Atlantic Thermohaline Circulation
12. 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
Radiative Flux
Earth's tilt
Altimetry (height)
Normal condition for air
13. 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
14. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Calving
Negative
Normal condition for air
Active Layer
15. Volcanic eruptions - Sunspots - Wobbly Earth
Grounding v Surface Melting
The Ozone Hole
Atmospheric Structure
Natural Causes of Warming
16. The past climate...for this reason - both keep good records of climate change.
Agricultural Drought
Severe coastal erosion
Thickness of the active layer and the permafrost depend on this
Absolute thresholds
17. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Natural Causes of Warming
Severe coastal erosion
How talik forms under lakes
18. Radiation absorbed by atmospheric greenhouse gases?
Grounding v Surface Melting
Mass Balance
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Greenhouse Gases
19. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Sea ice melt does not change sea level
30%
Methane
Albedos of Snow and Ice
20. 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
Ocean water
Thermohaline Circulation Effect
Accumulation
21. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Atmospheric Composition
Heat wave
Grounding v Surface Melting
Closed talik
22. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Thermokarst Lake
% of Greenhouse Gases
Ozone Hole
23. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Ice absorbs
Black Carbon
Ozone Hole
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
24. Forms in a mosaic of favoured locations.
Atlantic Thermohaline Circulation
Discontinuous Permafrosrt
Amount of light actually reaching the Earth
Ice loss
25. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Indirect heat wave effect
Changes in Arctic sea-ice Extent
Open talik
Thermohaline Circulation
26. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
Inversion Layer (feedback)
Thermohaline Circulation Effect
Why Water Vapor is not a climate forcing
27. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Some parts of the planet are dry because of their location
25%
The Ozone Hole
doubles
28. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Snow and snow covered ice absorb
Ice-Albedo
Greenhouse Gases
29. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Shortwave Length
Contributions to CO2 from different activities
Ocean water
Ice Cap
30. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
In the troposphere that we live in.
Altimetry Pros
Strong
The cryosphere
31. In average: +1% in respect to 100 years ago.
El Nino
Ice in the Arctic
Why Water Vapor is not a climate forcing
Is precipitation around the world increasing?
32. LW - SW - 55% absorbed by surface
In the Arctic where the air is cooler
Stratospheric Ozone Depletion
More rain means no drought
Energy Budget
33. 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.
70%
Discontinuous
Air pollution
What effects the density
34. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
air can warm dramatically
Methane
Sea Ice Extent is Changing in Antarctica as well
Ozone
35. 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.
Black Carbon
Accumulation
50%
Indirect heat wave effect
36. Amount of light absorbed by surface
Energy Budget
50%
Albedos of Snow and Ice
Severe coastal erosion
37. 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
Sea Ice
Mass Change
Global warming and hot nights?
Thinner atmosphere
38. 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.
Heat wave
Average radiative flux reaching the atmosphere
Ice Shelf
Ice Motion
39. 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.
Positive
Major distinction between Kyoto Protocol and Convention
The cryosphere
Sea ice melt does not change sea level
40. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
IN the last 2 decades what we've seen
Discontinuous Permafrosrt
Meteorological Drought
Stronger
41. How much is the planet really warming?
Ice/snow
.7O Celsius over the past century.
Ice Cap
GHG
42. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Talik
Thermokarst Lake
La Nia
Monthly maximums and minimums
43. 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.
Active Layer
Ice in the Arctic
Negative Ice-Albedo Feedback
The cryosphere
44. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Ice/snow
Ice Sheets
Wetter; drier
Heat Source and Pressure
45. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Longwave Radiation
Thinner atmosphere
Altimetry (height)
Calving
46. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Average radiative flux reaching the atmosphere
Once every 4 years.
La Nia
47. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
summer
Effect of Deforestation on CO-2
Positive
winter
48. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Amount of light actually reaching the Earth
Antarctica
Sea Ice
49. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Normal condition for air
Ocean water
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Permafrost Degradation
50. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Frozen Soil
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Surface Mass Balance
El Nino