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Test your basic knowledge |
Global Warming
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Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Reduction of snow and ice cover - Changes in atmospheric circulation.
Antarctica
30%
Cause of break of inversion layers or decrease in frequency
Threshold departures
2. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Is precipitation around the world increasing?
GHG
Ice shelf
3. Warming- positive feedback - Cooling- negative feedback.
Heat wave
El Nio is in the coasts of...
Very small portion
Ice-Albedo
4. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Depth v Surface
In the Arctic where the air is cooler
Sea Ice Extent is Changing in Antarctica as well
Ice Motion
5. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Radiative Flux
Ice absorbs
Why ice-albedo feedback is a big deal in the Arctic
Negative
6. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Surface Mass Balance
Altimetry (height)
Ocean water
Ice Motion
7. Like weighing oneself on the scale.
Time Variable Gravity
In the troposphere that we live in.
Sublimation
30%
8. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Sunspots
In the Arctic where the air is cooler
Sea-Ice Albedo
Monthly maximums and minimums
9. 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
Altimetry Pros
Thermohaline Circulation
Dry
Ice Shelf
10. 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.
Troposphere
air can warm dramatically
The Ozone Hole
Climate Change in the Arctic
11. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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12. Atmosphere retains ____ CO2
Methane
Effect of Deforestation on CO-2
45%
Indirect heat wave effect
13. A dome shaped cover of perennial ice and snow.
Surface Mass Balance
Energy Budget
The Ozone Hole
Ice Cap
14. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
How we measure Mass Balance
Heat Source and Pressure
Permafrost Degradation
El Nino
15. 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%
Precipitation and High Latitudes
Melt
30%
Albedos of Snow and Ice
16. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
.7O Celsius over the past century.
Thermohaline Circulatoin
Thermokarst
17. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
Earth's tilt
Atmospheric Composition?
El Nio is in the coasts of...
18. Precipitation intensity will rise ___ for every 1 OC of warming.
Sunspots
7%
Cause of break of inversion layers or decrease in frequency
Black Carbon
19. 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
Ice shelf
Earth's tilt
Longwave Radiation
doubles
20. 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.
Absolute thresholds
Ice Shelf
Positive
Ice-Albedo
21. Amount of light absorbed by surface
Questions to think about
How talik forms under lakes
How to define a heatwave
50%
22. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
El Nio is in the coasts of...
In the stratosphere.
Warm
Contributions to CO2 from different activities
23. Summer increase in cloud cover - Winter decrease in cloud cover.
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24. 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
Atmospheric Circulation
50%
Altimetry (height)
25. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Earth's tilt
Ice Sheets
How to define a heatwave
Ice Motion
26. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Antarctica
Thermohaline Circulation
Sea-Ice Albedo
Hydrological Drought
27. LW - SW - 55% absorbed by surface
% of Greenhouse Gases
70%
Energy Budget
What effects the density
28. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Absolute thresholds
25%
Precipitation and High Latitudes
29. How often does El Nio occur?
30%
Grounding Lines
Once every 4 years.
Sea ice melt does not change sea level
30. The amount of light reflected by an object.
Albedo
IN the last 2 decades what we've seen
summer
Strong
31. 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.
Shortwave Length
Air pollution
Thermohaline Circulatoin
Deep tropics between 15O N and 15 O S are quite
32. Number of days that exceed a given temperature
Where rise in OC is greatest
All Greenhouse gases
Discontinuous Permafrosrt
Absolute thresholds
33. 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.
Negative
winter
Ice Sheets
Mass Change
34. Measures input and output.
Discontinuous
Thermohaline Circulation
Dynamic thinning
Mass Budget
35. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
How the cryosphere is affected by climate change
winter
Ocean water
Severe coastal erosion
36. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Melt
In the stratosphere.
Sea ice melt does not change sea level
37. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Albedo
Threshold departures
reduction in sea-ice
Atlantic Thermohaline Circulation
38. 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.
Absolute thresholds
Ice loss
Infrared radiation
Thermohaline Circulation Effect
39. 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.
Albedos of Snow and Ice
doubles
Changes in Arctic sea-ice Extent
Atmospheric Composition
40. 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
El Nino
Severe coastal erosion
Layers of Earth
Active Layer
41. 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.
Greenhouse Gases
Snow and snow covered ice absorb
Atmospheric Composition
Layers of Earth
42. 1.4 USA - 57 m total sea level equivalent
winter
La Nia
All Greenhouse gases
Antarctica
43. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Strong
Severe coastal erosion
Permafrost Degradation
Thermokarst Lake
44. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Ice-Ocean Interactions
.7O Celsius over the past century.
reduction in sea-ice
45. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Ice-Ocean Interactions
Stronger
Ocean-Ice-Atmosphere Interaction
46. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Thermohaline Circulation
Ocean water
Precipitation and High Latitudes
Why the Arctic climate is special
47. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Sublimation
Open talik
Natural Causes of Warming
Change in vegetation generates a further feedback
48. High vs low
In the stratosphere.
Precipitation and High Latitudes
Cloud Feedbacks
Carbon Dioxide
49. 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
Thermokarst Lake
Affect Floods and Droughts
What happens with the Ozone Hole
Effect of Deforestation on CO-2
50. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
30%
Some parts of the planet are dry because of their location
Normal condition for air
Inversion Layer (feedback)
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