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. 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:
Thermohaline Circulation
Positive feedbacks both found in...
Albedo
Ice-Albedo
2. 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
winter
.7O Celsius over the past century.
Dry
Ice Shelf
3. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Time Variable Gravity
Affect Floods and Droughts
Negative Ice-Albedo Feedback
Dynamic thinning
4. 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
5. High vs low
Agricultural Drought
Cloud Feedbacks
Thermokarst
Mass Budget
6. The amount of light reflected by an object.
Ice shelf
Heat Source and Pressure
Change in vegetation generates a further feedback
Albedo
7. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Change in vegetation generates a further feedback
Why Water Vapor is not a climate forcing
Rainy
Atmospheric Composition
8. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
Thermokarst
IPCC
summer
9. ~10% of incident solar energy (albedo 90)
50%
Ice absorbs
Antarctica
Radiative Forcing
10. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Through talik
How to define a heatwave
Agricultural Drought
Infrared radiation
11. The past climate...for this reason - both keep good records of climate change.
More rain means no drought
IN the last 2 decades what we've seen
Thickness of the active layer and the permafrost depend on this
Air pollution
12. Greenhouse gases are mixed in the ____
Warm
Discontinuous
Atmospheric Composition?
Troposphere
13. CO2 GHG forcing - H2O - dominant/major GHG
Atmospheric Circulation
GHG
How the cryosphere is affected by climate change
Ice Motion
14. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Frozen Soil
Mass Change
Stronger
15. 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.
Atmospheric Circulation
Climate Change in the Arctic
Thermohaline Circulation Effect
Time Variable Gravity
16. Less frequent and weaker
Inversion Layer Summer
summer
Dynamic thinning
What happens with the Ozone Hole
17. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Monthly maximums and minimums
1 m/yr; 10x
Precipitation and High Latitudes
Types of Albedo
18. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
doubles
Effect of Deforestation on CO-2
Snow and snow covered ice absorb
Albedo
19. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Inversion Layer Summer
Thickness of the active layer and the permafrost depend on this
Ozone Hole
20. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Black Carbon
Methane
Thermohaline Circulatoin
Threshold departures
21. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Ice-Ocean Interactions
Questions to think about
Today melting ice
Is precipitation around the world increasing?
22. Number of days that exceed a given temperature
Absolute thresholds
Inversion Layer Summer
Shortwave Length
Discontinuous
23. High cloud has a _____ effect and cool cloud has a ____ effect
Ocean-Ice-Atmosphere Interaction
Warming; cooling
Sea Ice Extent is Changing in Antarctica as well
Ice Sheets
24. 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.
Ice-Ocean Interactions
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Indirect heat wave effect
Why the Arctic climate is special
25. Over the past century what has happened to the Earth's temperature?
Radiative Flux
GHG
Sea ice melt does not change sea level
Some regions of the Earth have warmed faster than other regions.
26. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Permafrost
Rainy
Thermokarst Lake
Positive
27. 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
Changes in Arctic sea-ice Extent
Ice/snow
Positive feedbacks both found in...
28. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Earth's tilt
Grounding Lines
Altimetry
IN the last 2 decades what we've seen
29. Atmosphere retains ____ CO2
45%
Ice Sheets
7%
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
30. Water vapor means more water up in the clouds and less in the ground!
Accumulation
Calving
More rain means no drought
In the stratosphere.
31. Extent 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.
reduction in sea-ice
.75OC/km-1
Discontinuous Permafrosrt
Radiative Forcing
32. 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
Global warming and hot nights?
Agricultural Drought
Discontinuous
Amount of light actually reaching the Earth
33. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Surface Mass Balance
Ocean water
Very small portion
34. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Why Water Vapor is not a climate forcing
75-OC
Atlantic Thermohaline Circulation
Global warming and hot nights?
35. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Changes in Arctic sea-ice Extent
Deep tropics between 15O N and 15 O S are quite
US and precipitation
Positive
36. In ________- inversion layer is more common in the Arctic
winter
Thermohaline Circulation
The cryosphere
Ocean-Ice-Atmosphere Interaction
37. 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 Sheets
Through talik
Ice Shelf
Thermohaline Circulation
38. Clouds 40~90% - Vegetation 10~15%
El Nino
Types of Albedo
.75OC/km-1
Arctic Atmosphere
39. 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.
Ice Sheets
Absolute thresholds
Altimetry Cons
Atmospheric Composition?
40. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
Warning
: Invalid argument supplied for foreach() in
/var/www/html/basicversity.com/show_quiz.php
on line
183
41. Amount of light absorbed by surface
More rain means no drought
Surface Mass Balance
50%
Layers of Earth
42. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Longwave Radiation
Accumulation
How a closed talik forms
Is precipitation around the world increasing?
43. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Nitrous Oxide (N2O)
Normal condition for air
Albedos of Snow and Ice
Thermokarst
44. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Ice Sheets
Monthly maximums and minimums
Altimetry Pros
45. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Permafrost
Where rise in OC is greatest
The Ozone Hole
Sunspots
46. Where does the ozone protect us?
In the stratosphere.
Arctic Atmosphere
Infrared radiation
Ice Cap
47. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Ice-Albedo
Permafrost
Depth v Surface
Some parts of the planet are dry because of their location
48. In _______ - the inversions are less frequent and weaker in the Arctic.
Altimetry Cons
7%
summer
Albedos of Snow and Ice
49. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Grounding v Surface Melting
IN the last 2 decades what we've seen
Today melting ice
Atlantic Thermohaline Circulation
50. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Meteorological Drought
Black Carbon
Altimetry Pros
Normal condition for air