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. 1.4 USA - 57 m total sea level equivalent
Heat Source and Pressure
Antarctica
Discontinuous Permafrosrt
Closed talik
2. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Is precipitation around the world increasing?
Ozone Hole
In the troposphere that we live in.
air can warm dramatically
3. 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.
Depth v Surface
Ozone Hole
Meteorological Drought
Indirect heat wave effect
4. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Atlantic Thermohaline Circulation
Methane
Importance of ice sheets
Cloud Feedbacks
5. 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
Types of Albedo
doubles
Reduction in sea-ice extent
Ice loss
6. Less frequent and weaker
summer
Surface Mass Balance
Inversion Layer Summer
Deep tropics between 15O N and 15 O S are quite
7. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Surface Mass Balance
30%
Severe coastal erosion
Heat Source and Pressure
8. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Ice shelf
El Nio is in the coasts of...
Precipitation and High Latitudes
Surface Mass Balance
9. 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.
1 m/yr; 10x
Climate Change in the Arctic
Ice Shelf
Atmospheric Structure
10. Water vapor means more water up in the clouds and less in the ground!
Black Carbon
More rain means no drought
Talik
Monthly maximums and minimums
11. 240 w/m squared
Arctic Atmosphere
El Nino
Amount of light actually reaching the Earth
Once every 4 years.
12. O Climate change in the Arctic is occurring now - Changes have been huge already
Frozen Soil
Positive
Today melting ice
Sea Ice Extent is Changing in Antarctica as well
13. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Ocean water
Depth v Surface
Positive
7%
14. Amount of light absorbed by surface
Atmospheric Circulation
Sea Ice
50%
30%
15. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
US and precipitation
Ice/snow
Greenland
Shortwave Length
16. Clouds 40~90% - Vegetation 10~15%
What happens with the Ozone Hole
Archimedes' Principle
Types of Albedo
Inversion Layer Summer
17. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
Indirect heat wave effect
Thermokarst Lake
Air pollution
18. 10 : 1 - grounding ; surface
Major distinction between Kyoto Protocol and Convention
Grounding v Surface Melting
US and precipitation
Layers of Earth
19. What can cause a change in the Earth's climate balance?
Affect Floods and Droughts
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Warming; cooling
Ice Discharge
20. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Ice Cap
Atmospheric Composition?
Antarctica
Thermokarst Lake
21. 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) -
Shortwave Length
Thinner atmosphere
1 m/yr; 10x
Normal condition for air
22. 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
23. 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.
Negative Ice-Albedo Feedback
Ice Cap
Sea Ice
Layers of Earth
24. Precipitation intensity will rise ___ for every 1 OC of warming.
Meteorological Drought
reduction in sea-ice
7%
El Nio is in the coasts of...
25. Greenhouse gases are mixed in the ____
Troposphere
Snow and snow covered ice absorb
Ozone Hole
What effects the density
26. The past climate...for this reason - both keep good records of climate change.
Thermokarst Lake
Time Variable Gravity
Change in vegetation generates a further feedback
Thickness of the active layer and the permafrost depend on this
27. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
The cryosphere
Accumulation
Heat wave
Dynamic thinning
28. CO2 GHG forcing - H2O - dominant/major GHG
Shortwave Length
GHG
Indirect heat wave effect
Sea-Ice Albedo
29. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
How to define a heatwave
Why ice-albedo feedback is a big deal in the Arctic
Increases - decreases
What happens with the Ozone Hole
30. 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
In the Arctic where the air is cooler
Time Variable Gravity
30%
Altimetry Cons
31. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
IN the last 2 decades what we've seen
Nitrous Oxide (N2O)
Importance of ice sheets
Altimetry Cons
32. 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
What effects the density
Ice-Albedo
Albedo
Ice Sheets
33. Descending Air dry - Convection cells are wet.
Thinner atmosphere
Why Water Vapor is not a climate forcing
Atmospheric Circulation
Ice shelf
34. More common
Ice Shelf
Absolute thresholds
Inversion Layer Winter
Ozone Hole
35. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
La Nia
Ice Motion
Warm
Methane
36. A dome shaped cover of perennial ice and snow.
Ice Cap
Ocean water
The Ozone Hole
Severe coastal erosion
37. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Methane
winter
Contributions to CO2 from different activities
Dry
38. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ice/snow
Meteorological Drought
Ozone Hole
Agricultural Drought
39. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
Normal condition for air
Mass Balance
La Nia
40. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Threshold departures
Frozen Soil
Negative
In the troposphere that we live in.
41. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Thermokarst
Atmospheric Composition?
Methane
Surface Mass Balance
42. 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
Major distinction between Kyoto Protocol and Convention
Why ice-albedo feedback is a big deal in the Arctic
Methane
Is precipitation around the world increasing?
43. Radiation absorbed by atmospheric greenhouse gases?
Amount of light actually reaching the Earth
Ice Sheets
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Sunspots
44. 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.
Antarctica
Greenhouse Gases
Permafrost
Ocean-Ice-Atmosphere Interaction
45. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
Surface Mass Balance
Thermohaline Circulation
GHG
What happens with the Ozone Hole
46. Greenhouse gases are a ___ portion of the atmosphere
Archimedes' Principle
Very small portion
Negative Ice-Albedo Feedback
All Greenhouse gases
47. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Ocean water
Effect of Deforestation on CO-2
Change in vegetation generates a further feedback
Mass Budget
48. Atmosphere retains ____ CO2
Average radiative flux reaching the atmosphere
45%
Layers of Earth
Accumulation
49. 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.
Sea Ice
Thermohaline Circulatoin
reduction in sea-ice
Surface Mass Balance
50. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Discharge
Atmospheric Structure
Ice Motion
How to define a heatwave