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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. 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
1 m/yr; 10x
Today melting ice
Grounding Lines
2. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Time Variable Gravity
How we measure Mass Balance
Ice loss
3. Number of days when temperatures climb above average by a fixed amount.
The Ozone Hole
Threshold departures
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
In the Arctic where the air is cooler
4. Precipitation intensity will rise ___ for every 1 OC of warming.
US and precipitation
Antarctica
7%
Ocean water
5. 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
Through talik
Atmospheric Composition?
Why ice-albedo feedback is a big deal in the Arctic
In the Arctic where the air is cooler
6. How often does El Nio occur?
Once every 4 years.
Methane
How talik forms under lakes
Atmospheric Composition
7. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
How the cryosphere is affected by climate change
winter
Carbon Dioxide
8. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Negative
Inversion Layer Summer
Sea Ice
Effect of Deforestation on CO-2
9. Frozen +2 years - Few centimeters to 1500 m
.75OC/km-1
Rainy
Ocean water
Permafrost
10. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Active Layer
Ozone Hole
El Nio is in the coasts of...
Hydrological Drought
11. 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.
Importance of ice sheets
Ice loss
Radiative Flux
Natural Causes of Warming
12. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
All Greenhouse gases
Negative
doubles
13. 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
Deep tropics between 15O N and 15 O S are quite
Thinner atmosphere
Black Carbon
Cloud Feedbacks
14. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Black Carbon
Inversion Layer (feedback)
reduction in sea-ice
GHG
15. The order of 1 m/year. Melting is ten times more.
Ice absorbs
Inversion Layer Winter
Surface Mass Balance
What effects the density
16. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Talik
Surface Mass Balance
% of Greenhouse Gases
Average radiative flux reaching the atmosphere
17. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Dry
Altimetry
Methane
30%
18. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Permafrost
Normal condition for air
In the Arctic where the air is cooler
Global warming and hot nights?
19. 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.
Calving
Thermohaline Circulation
Grounding Lines
Negative Ice-Albedo Feedback
20. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Melt
Surface Mass Balance
.75OC/km-1
21. 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
Thermokarst
IPCC
Inversion Layer Winter
Questions to think about
22. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Inversion Layer Winter
Open talik
Ocean water
All Greenhouse gases
23. 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
Methane
How the cryosphere is affected by climate change
Air pollution
IN the last 2 decades what we've seen
24. 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
Methane
Through talik
Ice in the Arctic
25. High vs low
Ice Sheets
Cloud Feedbacks
Importance of ice sheets
The cryosphere
26. The buoyant force is equal to the weight of the displaced water.
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27. Where does the ozone protect us?
Thermohaline Circulation
In the stratosphere.
In the troposphere that we live in.
In the Arctic where the air is cooler
28. 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.
Melt
Thermohaline Circulatoin
Ocean-Ice-Atmosphere Interaction
Ice Shelf
29. Laser radar - H V - Long time series - high accuracy - Density
Stronger
Deep tropics between 15O N and 15 O S are quite
Altimetry (height)
US and precipitation
30. Total absorbed solar radiation
Thermohaline Circulatoin
70%
Surface Mass Balance
Negative Ice-Albedo Feedback
31. Water vapor means more water up in the clouds and less in the ground!
Why the Arctic climate is special
More rain means no drought
Ozone Hole
Sunspots
32. 10 : 1 - grounding ; surface
Mass Budget
Greenhouse Gases
Talik
Grounding v Surface Melting
33. Atmosphere retains ____ CO2
45%
Once every 4 years.
How we measure Mass Balance
Ice Cap
34. Like weighing oneself on the scale.
Atmospheric Composition
Time Variable Gravity
Sea-Ice Albedo
El Nino
35. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
Altimetry
Effect of Deforestation on CO-2
% of Greenhouse Gases
36. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
summer
How we measure Mass Balance
Surface Mass Balance
Some parts of the planet are dry because of their location
37. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Ocean water
How to define a heatwave
Stronger
Surface Mass Balance
38. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Altimetry Pros
Natural Causes of Warming
Surface Mass Balance
20%
39. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Active Layer
How to define a heatwave
GHG
Thermokarst Lake
40. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
.7O Celsius over the past century.
How a closed talik forms
Types of Albedo
Effect of Deforestation on CO-2
41. Set up in 1988 by WMO and UNEP.
Deep tropics between 15O N and 15 O S are quite
Meteorological Drought
Ocean water
IPCC
42. Over the Northern Hemisphere than the tropics.
El Nio is in the coasts of...
Where rise in OC is greatest
Surface Mass Balance
Mass Budget
43. Permafrost- A frozen soil
Frozen Soil
IN the last 2 decades what we've seen
Affect Floods and Droughts
Ice Motion
44. Surface Mass Balance is of the order of _____ melting is ____ times more.
Change in vegetation generates a further feedback
1 m/yr; 10x
Ocean-Ice-Atmosphere Interaction
Surface Mass Balance
45. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Ice shelf
Rainy
Layers of Earth
Altimetry Cons
46. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Grounding Lines
Thermohaline Circulation Effect
Nitrous Oxide (N2O)
47. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Some parts of the planet are dry because of their location
Ice shelf
Atmospheric Composition?
Negative Ice-Albedo Feedback
48. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Positive feedbacks both found in...
Threshold departures
Reduction in sea-ice extent
Hydrological Drought
49. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
50%
Melt
Shortwave Length
Open talik
50. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Surface Mass Balance
Methane
Thinner atmosphere
Thermohaline Circulation Effect