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. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
IPCC
Increases - decreases
Sublimation
Grounding Lines
2. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
How to define a heatwave
Ice/snow
Negative
Grounding Lines
3. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Altimetry Pros
Thickness of the active layer and the permafrost depend on this
Dry
Shortwave Length
4. Unfrozen ground that is found within a mass of permafrost
Closed talik
La Nia
Absolute thresholds
Cloud Feedbacks
5. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Thermohaline Circulation
Grounding v Surface Melting
Atmospheric Composition
6. 10 : 1 - grounding ; surface
GHG
Grounding v Surface Melting
Infrared radiation
Calving
7. A dome shaped cover of perennial ice and snow.
1 m/yr; 10x
Ice Cap
Mass Change
Sublimation
8. Land Based Ecosystems retain ____ CO2.
Methane
30%
Increases - decreases
Ice Motion
9. O Climate change in the Arctic is occurring now - Changes have been huge already
Ice in the Arctic
Today melting ice
All Greenhouse gases
Very small portion
10. 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.
Changes in Arctic sea-ice Extent
Climate Change in the Arctic
Thermohaline Circulation
Depth v Surface
11. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Energy Budget
US and precipitation
La Nia
12. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Strong
Atmospheric Composition
Ice Discharge
Increases - decreases
13. 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.
Normal condition for air
Atmospheric Structure
What effects the density
Cause of break of inversion layers or decrease in frequency
14. Volcanic eruptions - Sunspots - Wobbly Earth
summer
25%
Is precipitation around the world increasing?
Natural Causes of Warming
15. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
75-OC
Very small portion
Heat Source and Pressure
Methane
16. What can cause a change in the Earth's climate balance?
Today melting ice
Why ice-albedo feedback is a big deal in the Arctic
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Dry
17. 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
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Grounding Lines
Increases - decreases
18. The amount of light reflected by an object.
Albedo
Through talik
Atmospheric Composition
Ozone Hole
19. 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.
Normal condition for air
Average radiative flux reaching the atmosphere
Permafrost Degradation
Ice Sheets
20. ~10% of incident solar energy (albedo 90)
Ice absorbs
Permafrost Degradation
Carbon Dioxide
Global warming and hot nights?
21. 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
Ice absorbs
50%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
How the cryosphere is affected by climate change
22. 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
What happens with the Ozone Hole
Questions to think about
In the Arctic where the air is cooler
Very small portion
23. Melting Point decreases
Black Carbon
reduction in sea-ice
Positive
.75OC/km-1
24. Forms in a mosaic of favoured locations.
Ice in the Arctic
Heat wave
In the troposphere that we live in.
Discontinuous Permafrosrt
25. Permafrost- A frozen soil
El Nino
Frozen Soil
Methane
25%
26. In _______ - the inversions are less frequent and weaker in the Arctic.
Thermohaline Circulation Effect
Dry
summer
Ice loss
27. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
50%
Permafrost Degradation
Melt
Global warming and hot nights?
28. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
How to define a heatwave
Absolute thresholds
Grounding Lines
25%
29. 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.
Natural Causes of Warming
Mass Balance
Ocean water
Ice Shelf
30. CO2 GHG forcing - H2O - dominant/major GHG
Ice Discharge
GHG
Longwave Radiation
Altimetry (height)
31. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
La Nia
Calving
Depth v Surface
Monthly maximums and minimums
32. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Discontinuous Permafrosrt
Atmospheric Structure
Hydrological Drought
IN the last 2 decades what we've seen
33. Reduction of Summer Sea- 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 - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Positive
Thermohaline Circulation
Changes in Arctic sea-ice Extent
Reduction in sea-ice extent
34. LW - SW - 55% absorbed by surface
70%
% of Greenhouse Gases
Active Layer
Energy Budget
35. 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%
Cloud Feedbacks
Albedos of Snow and Ice
Sea Ice Extent is Changing in Antarctica as well
Layers of Earth
36. Surface Mass Balance is of the order of _____ melting is ____ times more.
US and precipitation
1 m/yr; 10x
Stronger
Importance of ice sheets
37. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Albedos of Snow and Ice
Ice loss
Rainy
Sunspots
38. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Absolute thresholds
Permafrost
Agricultural Drought
Discontinuous
39. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
How the cryosphere is affected by climate change
Frozen Soil
Ozone Hole
Sea Ice Extent is Changing in Antarctica as well
40. The order of 1 m/year. Melting is ten times more.
Strong
Ice Sheets
Ocean water
Surface Mass Balance
41. Where do greenhouse gases warm up the Earth?
Stratospheric Ozone Depletion
In the troposphere that we live in.
Grounding Lines
Climate Change in the Arctic
42. 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:
Nitrous Oxide (N2O)
Heat wave
Black Carbon
Thermohaline Circulation
43. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Dry
Thermohaline Circulation
All Greenhouse gases
Black Carbon
44. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Ocean-Ice-Atmosphere Interaction
Positive feedbacks both found in...
Precipitation and High Latitudes
7%
45. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Sea Ice Extent is Changing in Antarctica as well
Antarctica
Altimetry (height)
46. O Unfrozen soil that stays within the permafrost.
Very small portion
Why ice-albedo feedback is a big deal in the Arctic
Atmospheric Structure
Talik
47. Antarctica - stratosphere - Sep-Oct
Ice loss
Ice/snow
Ozone Hole
7%
48. 1.4 USA - 57 m total sea level equivalent
50%
US and precipitation
Mass Budget
Antarctica
49. Greenhouse gases are a ___ portion of the atmosphere
Dry
Heat Source and Pressure
Ozone Hole
Very small portion
50. How often does El Nio occur?
Once every 4 years.
Ocean water
75-OC
Sea Ice