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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. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Indirect heat wave effect
Shortwave Length
Inversion Layer (feedback)
Ice in the Arctic
2. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Atmospheric Composition
Stronger
Melt
Archimedes' Principle
3. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Today melting ice
Ozone Hole
Ice loss
Dynamic thinning
4. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Strong
Once every 4 years.
.7O Celsius over the past century.
Rainy
5. 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
Thinner atmosphere
Ocean water
In the troposphere that we live in.
How the cryosphere is affected by climate change
6. Forms in a mosaic of favoured locations.
Today melting ice
Discontinuous Permafrosrt
.75OC/km-1
Dynamic thinning
7. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Sea Ice
Ice Discharge
Closed talik
8. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Melt
IN the last 2 decades what we've seen
Snow and snow covered ice absorb
Methane
9. Unfrozen ground that is found within a mass of permafrost
Atmospheric Composition
Black Carbon
Closed talik
.75OC/km-1
10. The past climate...for this reason - both keep good records of climate change.
Grounding Lines
30%
Thickness of the active layer and the permafrost depend on this
Ice Sheets
11. 240 w/m squared
Positive feedbacks both found in...
Amount of light actually reaching the Earth
Ice loss
Rainy
12. 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
Methane
Heat wave
Energy Budget
13. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Motion
The cryosphere
Increases - decreases
Talik
14. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Radiative Flux
Effect of Deforestation on CO-2
30%
Melt
15. 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.
Indirect heat wave effect
Deep tropics between 15O N and 15 O S are quite
Active Layer
Where rise in OC is greatest
16. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Methane
El Nio is in the coasts of...
The Ozone Hole
Meteorological Drought
17. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Threshold departures
Warming; cooling
1 m/yr; 10x
18. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Hydrological Drought
Surface Mass Balance
Permafrost
Atmospheric Composition
19. 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.
Climate Change in the Arctic
Inversion Layer (feedback)
Infrared radiation
Ice Discharge
20. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
50%
Average radiative flux reaching the atmosphere
Today melting ice
21. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
US and precipitation
Closed talik
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Altimetry Cons
22. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
What effects the density
Ice Sheets
Meteorological Drought
Black Carbon
23. 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) -
El Nino
Normal condition for air
Altimetry Pros
Affect Floods and Droughts
24. 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
Inversion Layer Summer
Once every 4 years.
Permafrost Degradation
25. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
reduction in sea-ice
Thinner atmosphere
Cloud Feedbacks
Methane
26. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Negative
Deep tropics between 15O N and 15 O S are quite
Ice in the Arctic
Positive feedbacks both found in...
27. 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.
Meteorological Drought
Changes in Arctic sea-ice Extent
IPCC
El Nio is in the coasts of...
28. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Deep tropics between 15O N and 15 O S are quite
Carbon Dioxide
The Ozone Hole
29. 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
Amount of light actually reaching the Earth
Ice Sheets
What happens with the Ozone Hole
30. 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.
Ozone
Radiative Forcing
Strong
Thermohaline Circulation Effect
31. Ice sheets have a very ____ Albedo
Strong
Thermohaline Circulatoin
Frozen Soil
70%
32. Atmosphere retains ____ CO2
Shortwave Length
7%
45%
Stratospheric Ozone Depletion
33. The order of 1 m/year. Melting is ten times more.
Ozone Hole
Reduction in sea-ice extent
Sea Ice Extent is Changing in Antarctica as well
Surface Mass Balance
34. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Global warming and hot nights?
Dynamic thinning
Grounding Lines
El Nino
35. 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.
Dynamic thinning
Greenhouse Gases
.7O Celsius over the past century.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
36. CO2 - CH4 - O3 - H2O - N2O - CFCs
25%
Sea ice melt does not change sea level
Permafrost
All Greenhouse gases
37. How often does El Nio occur?
Sunspots
Warm
Once every 4 years.
Surface Mass Balance
38. Set up in 1988 by WMO and UNEP.
Inversion Layer Winter
IPCC
Negative
Stronger
39. 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.
Why Water Vapor is not a climate forcing
Earth's tilt
doubles
Inversion Layer (feedback)
40. Number of days that exceed a given temperature
Absolute thresholds
Albedos of Snow and Ice
How talik forms under lakes
Change in vegetation generates a further feedback
41. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
IPCC
Cause of break of inversion layers or decrease in frequency
Increases - decreases
42. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Infrared radiation
Types of Albedo
Ocean water
Earth's tilt
43. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Permafrost Degradation
The cryosphere
Absolute thresholds
Importance of ice sheets
44. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Active Layer
Once every 4 years.
Questions to think about
Stronger
45. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Talik
Positive
Atmospheric Circulation
Ice-Ocean Interactions
46. Where does the ozone protect us?
In the stratosphere.
Altimetry Cons
Mass Balance
Hydrological Drought
47. 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
Thermohaline Circulation Effect
Antarctica
Heat wave
48. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
Sea ice melt does not change sea level
Carbon Dioxide
GHG
49. 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
Atlantic Thermohaline Circulation
Why ice-albedo feedback is a big deal in the Arctic
Ice Sheets
Ice loss
50. Greenhouse gases are a ___ portion of the atmosphere
Monthly maximums and minimums
Questions to think about
Amount of light actually reaching the Earth
Very small portion