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. Atmosphere retains ____ CO2
Deep tropics between 15O N and 15 O S are quite
20%
45%
Troposphere
2. x7 smaller - 7m total sea level equivalent.
Greenland
How to define a heatwave
Why ice-albedo feedback is a big deal in the Arctic
Through talik
3. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Importance of ice sheets
Percentile departures
Sea Ice Extent is Changing in Antarctica as well
Discontinuous Permafrosrt
4. 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%
Through talik
Why ice-albedo feedback is a big deal in the Arctic
Increases - decreases
Albedos of Snow and Ice
5. 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.
Altimetry (height)
Infrared radiation
Amount of light actually reaching the Earth
What effects the density
6. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Ice absorbs
Dynamic thinning
Earth's tilt
Monthly maximums and minimums
7. Less frequent and weaker
Some regions of the Earth have warmed faster than other regions.
Why Water Vapor is not a climate forcing
Inversion Layer Summer
Warm
8. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Cause of break of inversion layers or decrease in frequency
Negative
Permafrost
9. 1.4 USA - 57 m total sea level equivalent
Ocean water
Ice Sheets
Antarctica
30%
10. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Contributions to CO2 from different activities
Grounding Lines
Frozen Soil
US and precipitation
11. What can cause a change in the Earth's climate balance?
El Nino
Antarctica
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
IN the last 2 decades what we've seen
12. 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.
Why Water Vapor is not a climate forcing
Nitrous Oxide (N2O)
How we measure Mass Balance
Ice Sheets
13. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
Normal condition for air
Antarctica
30%
14. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Inversion Layer Winter
Ice Cap
Some parts of the planet are dry because of their location
15. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
75-OC
Ice in the Arctic
Depth v Surface
16. 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.
Thermohaline Circulatoin
Carbon Dioxide
Dynamic thinning
Monthly maximums and minimums
17. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
La Nia
Through talik
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Altimetry (height)
18. 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
Melt
Black Carbon
Stronger
Sea Ice Extent is Changing in Antarctica as well
19. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
Amount of light actually reaching the Earth
Ice Sheets
45%
20. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Infrared radiation
IPCC
Active Layer
Arctic Atmosphere
21. Warming- positive feedback - Cooling- negative feedback.
% of Greenhouse Gases
.75OC/km-1
Ice-Albedo
Time Variable Gravity
22. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
All Greenhouse gases
Albedos of Snow and Ice
How to define a heatwave
Mass Budget
23. 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.
Ice Shelf
Carbon Dioxide
Antarctica
Ozone Hole
24. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Severe coastal erosion
Ice in the Arctic
Altimetry
25. Where do greenhouse gases warm up the Earth?
Dry
Layers of Earth
Average radiative flux reaching the atmosphere
In the troposphere that we live in.
26. Permafrost- A frozen soil
Frozen Soil
Stratospheric Ozone Depletion
Longwave Radiation
Thermohaline Circulation Effect
27. The past climate...for this reason - both keep good records of climate change.
Thickness of the active layer and the permafrost depend on this
Stratospheric Ozone Depletion
doubles
Albedos of Snow and Ice
28. Surface Mass Balance is of the order of _____ melting is ____ times more.
air can warm dramatically
1 m/yr; 10x
Shortwave Length
Grounding Lines
29. LW - SW - 55% absorbed by surface
More rain means no drought
Energy Budget
Why Water Vapor is not a climate forcing
Ice loss
30. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
30%
Warm
How we measure Mass Balance
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
31. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
What happens with the Ozone Hole
Thickness of the active layer and the permafrost depend on this
Accumulation
Ozone Hole
32. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Reduction in sea-ice extent
All Greenhouse gases
El Nio is in the coasts of...
Altimetry Pros
33. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Rainy
Positive
More rain means no drought
Precipitation and High Latitudes
34. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Why Water Vapor is not a climate forcing
Ice in the Arctic
Sea Ice Extent is Changing in Antarctica as well
Thermokarst
35. 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
Contributions to CO2 from different activities
Talik
Ice absorbs
36. Number of days that exceed a given temperature
Percentile departures
Absolute thresholds
Natural Causes of Warming
Closed talik
37. How much is the planet really warming?
.7O Celsius over the past century.
Radiative Flux
Agricultural Drought
Sea Ice
38. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
Arctic Atmosphere
50%
Change in vegetation generates a further feedback
39. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Dynamic thinning
Affect Floods and Droughts
air can warm dramatically
Methane
40. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Once every 4 years.
Strong
Heat Source and Pressure
What effects the density
41. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Thickness of the active layer and the permafrost depend on this
Ice Sheets
Surface Mass Balance
Mass Balance
42. 85%
Nitrous Oxide (N2O)
Ozone
Positive feedbacks both found in...
Sea-Ice Albedo
43. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Average radiative flux reaching the atmosphere
Change in vegetation generates a further feedback
Shortwave Length
Thinner atmosphere
44. 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.
Frozen Soil
Layers of Earth
Negative Ice-Albedo Feedback
Thermokarst Lake
45. 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
Agricultural Drought
reduction in sea-ice
Altimetry (height)
winter
46. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Atmospheric Composition?
75-OC
Types of Albedo
Global warming and hot nights?
47. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Very small portion
Why ice-albedo feedback is a big deal in the Arctic
Ozone Hole
The cryosphere
48. 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
The Ozone Hole
In the Arctic where the air is cooler
Indirect heat wave effect
Dynamic thinning
49. 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
Why the Arctic climate is special
Depth v Surface
Why ice-albedo feedback is a big deal in the Arctic
Archimedes' Principle
50. Laser radar - H V - Long time series - high accuracy - Density
Wetter; drier
Open talik
Altimetry (height)
Cause of break of inversion layers or decrease in frequency