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. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
IN the last 2 decades what we've seen
Rainy
Stronger
Today melting ice
2. 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.
Some parts of the planet are dry because of their location
How to define a heatwave
Ice-Ocean Interactions
Radiative Forcing
3. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Atmospheric Composition?
Amount of light actually reaching the Earth
Discontinuous
Thermohaline Circulation Effect
4. 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.
Ice Sheets
Thermokarst Lake
Positive
reduction in sea-ice
5. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Permafrost Degradation
Surface Mass Balance
More rain means no drought
Ice shelf
6. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Affect Floods and Droughts
Severe coastal erosion
In the troposphere that we live in.
Antarctica
7. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Change in vegetation generates a further feedback
Negative
50%
Mass Balance
8. 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
winter
Ice Discharge
Talik
9. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Frozen Soil
Affect Floods and Droughts
Time Variable Gravity
Infrared radiation
10. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
Permafrost
20%
Ozone
Importance of ice sheets
11. Set up in 1988 by WMO and UNEP.
Meteorological Drought
IPCC
Ozone Hole
Sea ice melt does not change sea level
12. 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.
20%
Negative Ice-Albedo Feedback
Ice Sheets
Ice/snow
13. 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.
Normal condition for air
30%
Through talik
Ice Shelf
14. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
El Nio is in the coasts of...
Threshold departures
Greenhouse Gases
Ozone
15. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
70%
Sublimation
Longwave Radiation
Talik
16. Frozen +2 years - Few centimeters to 1500 m
Monthly maximums and minimums
Permafrost
Ice Sheets
Cloud Feedbacks
17. Less frequent and weaker
Atmospheric Structure
Surface Mass Balance
Is precipitation around the world increasing?
Inversion Layer Summer
18. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
How talik forms under lakes
Ice Motion
US and precipitation
Depth v Surface
19. Melting Point decreases
Negative Ice-Albedo Feedback
Increases - decreases
Ice/snow
.75OC/km-1
20. ~10% of incident solar energy (albedo 90)
Stronger
Some parts of the planet are dry because of their location
Calving
Ice absorbs
21. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Thermokarst
Amount of light actually reaching the Earth
doubles
22. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Permafrost
Thermohaline Circulatoin
The Ozone Hole
Surface Mass Balance
23. Unfrozen ground that is found within a mass of permafrost
Ice/snow
How talik forms under lakes
Closed talik
All Greenhouse gases
24. 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.
Altimetry
Sunspots
What happens with the Ozone Hole
Greenhouse Gases
25. Amount of light absorbed by atmosphere
Today melting ice
20%
Positive
Closed talik
26. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
1 m/yr; 10x
Ozone Hole
How a closed talik forms
Carbon Dioxide
27. 85%
Stratospheric Ozone Depletion
Sea-Ice Albedo
Where rise in OC is greatest
Black Carbon
28. 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
Black Carbon
Amount of light actually reaching the Earth
Active Layer
29. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Monthly maximums and minimums
El Nino
Ice Sheets
Mass Budget
30. Ocean retains ____ CO2
25%
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Permafrost Degradation
Cause of break of inversion layers or decrease in frequency
31. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
More rain means no drought
Atmospheric Structure
How to define a heatwave
Very small portion
32. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Talik
How we measure Mass Balance
25%
Global warming and hot nights?
33. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
Some parts of the planet are dry because of their location
Time Variable Gravity
What effects the density
34. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Ocean water
IN the last 2 decades what we've seen
What happens with the Ozone Hole
Contributions to CO2 from different activities
35. CO2 GHG forcing - H2O - dominant/major GHG
IPCC
Percentile departures
GHG
Ocean water
36. How often does El Nio occur?
Once every 4 years.
Inversion Layer Summer
Ocean-Ice-Atmosphere Interaction
20%
37. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Once every 4 years.
Layers of Earth
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
38. In average: +1% in respect to 100 years ago.
What happens with the Ozone Hole
Is precipitation around the world increasing?
Time Variable Gravity
Absolute thresholds
39. 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
Today melting ice
How a closed talik forms
Dry
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
40. Rainy on yearly average. In these regions - rising air predominates.
Carbon Dioxide
Deep tropics between 15O N and 15 O S are quite
In the Arctic where the air is cooler
30%
41. More common
Questions to think about
How the cryosphere is affected by climate change
Inversion Layer Winter
Active Layer
42. Where does the ozone protect us?
In the stratosphere.
Atmospheric Structure
Wetter; drier
Antarctica
43. Where do greenhouse gases warm up the Earth?
Agricultural Drought
30%
In the troposphere that we live in.
Depth v Surface
44. 1.4 USA - 57 m total sea level equivalent
Active Layer
Thermokarst
Antarctica
Black Carbon
45. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Thermokarst
Surface Mass Balance
30%
Changes in Arctic sea-ice Extent
46. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Sea-Ice Albedo
Thermokarst
Heat wave
Positive
47. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
All Greenhouse gases
30%
Contributions to CO2 from different activities
Altimetry Cons
48. 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:
Antarctica
Increases - decreases
In the Arctic where the air is cooler
Thermohaline Circulation
49. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Discontinuous
Thermokarst
Talik
Dry
50. 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.
Some parts of the planet are dry because of their location
Negative Ice-Albedo Feedback
Frozen Soil
What effects the density