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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. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Discontinuous
Longwave Radiation
Heat Source and Pressure
Types of Albedo
2. The past climate...for this reason - both keep good records of climate change.
Why ice-albedo feedback is a big deal in the Arctic
Thickness of the active layer and the permafrost depend on this
Earth's tilt
Calving
3. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Active Layer
Affect Floods and Droughts
How to define a heatwave
winter
4. 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
Altimetry Pros
Natural Causes of Warming
Indirect heat wave effect
5. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Cause of break of inversion layers or decrease in frequency
Once every 4 years.
Greenhouse Gases
Arctic Atmosphere
6. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Very small portion
Stratospheric Ozone Depletion
winter
Types of Albedo
7. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Wetter; drier
Talik
Discontinuous Permafrosrt
Why Water Vapor is not a climate forcing
8. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Sea-Ice Albedo
Types of Albedo
Thinner atmosphere
9. 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.
Ocean water
Thermohaline Circulatoin
Altimetry
Major distinction between Kyoto Protocol and Convention
10. Number of days when temperatures climb above average by a fixed amount.
Archimedes' Principle
Active Layer
Threshold departures
1 m/yr; 10x
11. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Altimetry (height)
Ice in the Arctic
Surface Mass Balance
Talik
12. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Change in vegetation generates a further feedback
Major distinction between Kyoto Protocol and Convention
Questions to think about
Antarctica
13. 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
Dry
How a closed talik forms
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Sea ice melt does not change sea level
14. High vs low
Talik
Cloud Feedbacks
What happens with the Ozone Hole
Albedos of Snow and Ice
15. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Surface Mass Balance
Troposphere
Through talik
16. Volcanic eruptions - Sunspots - Wobbly Earth
Energy Budget
Stronger
Natural Causes of Warming
Methane
17. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Frozen Soil
Ice Cap
Meteorological Drought
Ice Sheets
18. Ice sheets have a very ____ Albedo
Greenhouse Gases
Strong
Where rise in OC is greatest
Open talik
19. he increase of ozone concentration in the atmosphere helps ____ our planet
doubles
Warm
Sea Ice
Positive
20. Ocean retains ____ CO2
Greenland
25%
winter
Energy Budget
21. A thick - floating slab of freshwater ice extending from coast to coast.
Positive feedbacks both found in...
Inversion Layer Summer
Ice shelf
Grounding Lines
22. The amount of light reflected by an object.
How a closed talik forms
Threshold departures
Albedo
Why ice-albedo feedback is a big deal in the Arctic
23. Really measures volume.
Methane
Thickness of the active layer and the permafrost depend on this
Ozone Hole
Altimetry
24. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Thermohaline Circulation
How we measure Mass Balance
Antarctica
Discontinuous Permafrosrt
25. In _______ - the inversions are less frequent and weaker in the Arctic.
Threshold departures
Positive feedbacks both found in...
summer
Shortwave Length
26. Longwave radiation - any radiation with a long wave will heat up quickly.
Types of Albedo
Infrared radiation
IPCC
Shortwave Length
27. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Natural Causes of Warming
Thinner atmosphere
Ice Sheets
air can warm dramatically
28. Where do greenhouse gases warm up the Earth?
Sublimation
Warm
In the troposphere that we live in.
Altimetry Pros
29. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Thickness of the active layer and the permafrost depend on this
Methane
Active Layer
30. Land Based Ecosystems retain ____ CO2.
30%
Ice-Ocean Interactions
Nitrous Oxide (N2O)
Cause of break of inversion layers or decrease in frequency
31. x7 smaller - 7m total sea level equivalent.
Ice Sheets
Greenland
Altimetry Pros
45%
32. 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
Rainy
Affect Floods and Droughts
Importance of ice sheets
75-OC
33. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Meteorological Drought
Grounding Lines
air can warm dramatically
Thermohaline Circulation Effect
34. Where does the ozone protect us?
Questions to think about
In the stratosphere.
Thermohaline Circulatoin
Why the Arctic climate is special
35. Set up in 1988 by WMO and UNEP.
Ice-Ocean Interactions
Thermokarst
IPCC
Ice in the Arctic
36. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
How to define a heatwave
Atlantic Thermohaline Circulation
Some parts of the planet are dry because of their location
Increases - decreases
37. 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
Thermokarst
Sublimation
El Nio is in the coasts of...
38. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Average radiative flux reaching the atmosphere
Thermohaline Circulation
How a closed talik forms
Layers of Earth
39. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Changes in Arctic sea-ice Extent
Sea Ice
Warm
US and precipitation
40. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Infrared radiation
Radiative Forcing
30%
Sublimation
41. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Closed talik
Strong
El Nio is in the coasts of...
Ice Sheets
42. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Troposphere
Ocean-Ice-Atmosphere Interaction
El Nio is in the coasts of...
Altimetry Cons
43. 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
Permafrost Degradation
In the Arctic where the air is cooler
Accumulation
20%
44. The order of 1 m/year. Melting is ten times more.
Altimetry Cons
Surface Mass Balance
70%
Calving
45. 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
Snow and snow covered ice absorb
Infrared radiation
Once every 4 years.
doubles
46. Surface Mass Balance is of the order of _____ melting is ____ times more.
Methane
In the troposphere that we live in.
1 m/yr; 10x
Average radiative flux reaching the atmosphere
47. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Layers of Earth
Albedos of Snow and Ice
Through talik
Ice/snow
48. Like weighing oneself on the scale.
Negative
Time Variable Gravity
Hydrological Drought
Warming; cooling
49. CO2 GHG forcing - H2O - dominant/major GHG
Inversion Layer Winter
The Ozone Hole
Albedo
GHG
50. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Radiative Flux
Open talik
Discontinuous
US and precipitation