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. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
How to define a heatwave
Time Variable Gravity
Antarctica
Contributions to CO2 from different activities
2. 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.
Talik
Ice Cap
Ice Shelf
Changes in Arctic sea-ice Extent
3. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Discontinuous Permafrosrt
Air pollution
45%
Importance of ice sheets
4. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Change in vegetation generates a further feedback
Calving
Infrared radiation
Thermokarst
5. CO2 GHG forcing - H2O - dominant/major GHG
Global warming and hot nights?
Layers of Earth
GHG
IPCC
6. 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
Energy Budget
Importance of ice sheets
Some regions of the Earth have warmed faster than other regions.
Permafrost
7. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Percentile departures
Ice loss
Monthly maximums and minimums
Ice absorbs
8. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Rainy
Once every 4 years.
Ice in the Arctic
In the troposphere that we live in.
9. 10 : 1 - grounding ; surface
Altimetry (height)
Hydrological Drought
Grounding v Surface Melting
Ice-Albedo
10. 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.
Absolute thresholds
Affect Floods and Droughts
Ice-Ocean Interactions
Mass Balance
11. 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.
Importance of ice sheets
30%
Surface Mass Balance
Climate Change in the Arctic
12. 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.
Once every 4 years.
Ice loss
Greenhouse Gases
Thickness of the active layer and the permafrost depend on this
13. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ice Sheets
Why ice-albedo feedback is a big deal in the Arctic
Ocean water
.75OC/km-1
14. How much is the planet really warming?
Ice Sheets
Snow and snow covered ice absorb
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
.7O Celsius over the past century.
15. 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
Where rise in OC is greatest
Negative
Thinner atmosphere
Mass Change
16. Really measures volume.
Ozone
Altimetry
Why the Arctic climate is special
30%
17. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
How to define a heatwave
Ocean water
Sublimation
Inversion Layer (feedback)
18. In _______ - the inversions are less frequent and weaker in the Arctic.
Nitrous Oxide (N2O)
Sunspots
summer
Frozen Soil
19. Where do greenhouse gases warm up the Earth?
Thermohaline Circulation
Accumulation
Ice in the Arctic
In the troposphere that we live in.
20. Industrial product - 300 ppb (parts per billion)
Dynamic thinning
Nitrous Oxide (N2O)
Inversion Layer Winter
Depth v Surface
21. 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.
Inversion Layer (feedback)
air can warm dramatically
Increases - decreases
Agricultural Drought
22. Amount of light absorbed by atmosphere
The cryosphere
20%
Altimetry (height)
Layers of Earth
23. 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.
Ice-Ocean Interactions
Strong
Ice absorbs
Thermohaline Circulation Effect
24. Laser radar - H V - Long time series - high accuracy - Density
Active Layer
Altimetry (height)
Sea Ice
air can warm dramatically
25. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
IPCC
Change in vegetation generates a further feedback
Atmospheric Composition
Atmospheric Composition?
26. 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
How a closed talik forms
Effect of Deforestation on CO-2
Snow and snow covered ice absorb
doubles
27. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Threshold departures
Global warming and hot nights?
summer
The Ozone Hole
28. Cooler water and drought conditions.
reduction in sea-ice
Sea Ice
La Nia
Some parts of the planet are dry because of their location
29. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
In the troposphere that we live in.
Active Layer
Grounding v Surface Melting
30. US is responsible for ___ of the total CO2
Mass Budget
In the stratosphere.
Permafrost
30%
31. 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.
Stratospheric Ozone Depletion
What effects the density
Cause of break of inversion layers or decrease in frequency
Ice Sheets
32. 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
Atlantic Thermohaline Circulation
Discontinuous
Inversion Layer (feedback)
What happens with the Ozone Hole
33. Is not an externally imposed perturbation to the climate system.
In the stratosphere.
Very small portion
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Why Water Vapor is not a climate forcing
34. Antarctica - stratosphere - Sep-Oct
Very small portion
Ozone Hole
Surface Mass Balance
Why ice-albedo feedback is a big deal in the Arctic
35. Atmosphere retains ____ CO2
Is precipitation around the world increasing?
Atmospheric Composition
In the stratosphere.
45%
36. Longwave radiation - any radiation with a long wave will heat up quickly.
Atmospheric Composition
25%
Agricultural Drought
Infrared radiation
37. 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.
Active Layer
45%
Meteorological Drought
Negative Ice-Albedo Feedback
38. 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
All Greenhouse gases
Grounding v Surface Melting
summer
39. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Closed talik
30%
Precipitation and High Latitudes
Effect of Deforestation on CO-2
40. O Unfrozen soil that stays within the permafrost.
Thermohaline Circulation
Permafrost
Talik
Altimetry Cons
41. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Deep tropics between 15O N and 15 O S are quite
Shortwave Length
Infrared radiation
Thermokarst Lake
42. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Radiative Forcing
Increases - decreases
Thermokarst
Once every 4 years.
43. 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
20%
El Nino
Reduction in sea-ice extent
7%
44. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
25%
Greenland
Severe coastal erosion
Why the Arctic climate is special
45. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Why Water Vapor is not a climate forcing
Wetter; drier
More rain means no drought
46. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sea ice melt does not change sea level
Antarctica
Sunspots
Cloud Feedbacks
47. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Average radiative flux reaching the atmosphere
Active Layer
Atmospheric Composition?
Mass Balance
48. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
In the stratosphere.
Strong
Open talik
Atlantic Thermohaline Circulation
49. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Sea Ice
Warm
Ocean water
Grounding Lines
50. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Discontinuous
Why ice-albedo feedback is a big deal in the Arctic
Layers of Earth
Types of Albedo
Can you answer 50 questions in 15 minutes?
Let me suggest you:
Browse all subjects
Browse all tests
Most popular tests
Major Subjects
Tests & Exams
AP
CLEP
DSST
GRE
SAT
GMAT
Certifications
CISSP go to https://www.isc2.org/
PMP
ITIL
RHCE
MCTS
More...
IT Skills
Android Programming
Data Modeling
Objective C Programming
Basic Python Programming
Adobe Illustrator
More...
Business Skills
Advertising Techniques
Business Accounting Basics
Business Strategy
Human Resource Management
Marketing Basics
More...
Soft Skills
Body Language
People Skills
Public Speaking
Persuasion
Job Hunting And Resumes
More...
Vocabulary
GRE Vocab
SAT Vocab
TOEFL Essential Vocab
Basic English Words For All
Global Words You Should Know
Business English
More...
Languages
AP German Vocab
AP Latin Vocab
SAT Subject Test: French
Italian Survival
Norwegian Survival
More...
Engineering
Audio Engineering
Computer Science Engineering
Aerospace Engineering
Chemical Engineering
Structural Engineering
More...
Health Sciences
Basic Nursing Skills
Health Science Language Fundamentals
Veterinary Technology Medical Language
Cardiology
Clinical Surgery
More...
English
Grammar Fundamentals
Literary And Rhetorical Vocab
Elements Of Style Vocab
Introduction To English Major
Complete Advanced Sentences
Literature
Homonyms
More...
Math
Algebra Formulas
Basic Arithmetic: Measurements
Metric Conversions
Geometric Properties
Important Math Facts
Number Sense Vocab
Business Math
More...
Other Major Subjects
Science
Economics
History
Law
Performing-arts
Cooking
Logic & Reasoning
Trivia
Browse all subjects
Browse all tests
Most popular tests