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Test your basic knowledge |
Weather Fundamentals
Start Test
Study First
Subject
:
science
Instructions:
Answer 36 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. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
atmosphere
layers of atmosphere
cyclone
temp in troposphere
2. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
adiabatic cooling
stratosphere
layers of atmosphere
relative humidity
3. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
humidity
winds
weather
pressure
4. Occurs when rising air expands without change in heat content. Whenever an air mass expands - the available heat is distributed over a larger volume so the air becomes cooler.
clouds
cyclone
clouds
adiabatic cooling
5. Low pressure system. When an air mass near the ground is heated - the air molecules vibrate faster - cause the air mass to expand and its density to decrease. With a lower density than the surrounding air - the mass rises to create a low pressure reg
dew point
humidity
cyclone
pressure
6. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
absolute humidity
winds
humidity
weather
7. Amount of water vapor an aim mass holds. air can dissolve water
clouds
absolute humidity
humidity
troposphere
8. Occurs when rising air expands without change in heat content. Whenever an air mass expands - the available heat is distributed over a larger volume so the air becomes cooler.
troposphere
dew point
adiabatic cooling
layers of atmosphere
9. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
temp in troposphere
pressure
cyclone
weather
10. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
pressure
clouds
relative humidity
dew point
11. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
temp in troposphere
humidity
weather
cyclone
12. High pressure system. when cool air in the upper atmosphere has higher density than its surrounding - creating high pressure system. It moves twd the ground - so air moves way from the high pressure system near earth's surface
winds
stratosphere
anticyclone
absolute humidity
13. Daily fluctuations in temperature - wind speed - and precipitation
relative humidity
anticyclone
cyclone
weather
14. If air cools to the temp at which its relative humidity is 100% - the water saturated air is still invisible. If it cools further - it will have more ater vapor than it can hold and some of the water will condense into tiny water droplets - to form c
clouds
dew point
stratosphere
weather
15. Lowest layer. Where all weather phenomena occur. Extends to altitude of 10 to 15 km - contains about 90@ of mass of atmosphere - including about all water vapor.
troposphere
layers of atmosphere
humidity
atmosphere
16. Rising air exerts less downward pressure than falling air. air near the ground surface is pulled in toward the low pressure center to replace the rising air
humidity
cyclone
weather
lower pressure
17. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
atmosphere
layers of atmosphere
relative humidity
anticyclone
18. Amount of water vapor an aim mass holds. air can dissolve water
humidity
dew point
lower pressure
pressure
19. Daily fluctuations in temperature - wind speed - and precipitation
pressure
weather
humidity
relative humidity
20. Decreases upward to altitude of 10-15 km due to increase distance above main mass of earth - which absorbs sunlight and reradiates it as heat
temp in troposphere
adiabatic cooling
absolute humidity
clouds
21. Lowest layer. Where all weather phenomena occur. Extends to altitude of 10 to 15 km - contains about 90@ of mass of atmosphere - including about all water vapor.
troposphere
humidity
absolute humidity
cyclone
22. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
atmosphere
humidity
stratosphere
humidity
23. Rising air exerts less downward pressure than falling air. air near the ground surface is pulled in toward the low pressure center to replace the rising air
clouds
adiabatic cooling
lower pressure
humidity
24. Decreases upward to altitude of 10-15 km due to increase distance above main mass of earth - which absorbs sunlight and reradiates it as heat
absolute humidity
dew point
layers of atmosphere
temp in troposphere
25. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
layers of atmosphere
atmosphere
troposphere
weather
26. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
temp in troposphere
layers of atmosphere
clouds
winds
27. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
clouds
stratosphere
humidity
relative humidity
28. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
winds
clouds
atmosphere
dew point
29. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
troposphere
winds
adiabatic cooling
adiabatic cooling
30. If air cools to the temp at which its relative humidity is 100% - the water saturated air is still invisible. If it cools further - it will have more ater vapor than it can hold and some of the water will condense into tiny water droplets - to form c
adiabatic cooling
lower pressure
clouds
winds
31. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
relative humidity
pressure
dew point
absolute humidity
32. Mount of water vapor in the air
layers of atmosphere
absolute humidity
atmosphere
humidity
33. Mount of water vapor in the air
layers of atmosphere
relative humidity
absolute humidity
humidity
34. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
weather
humidity
dew point
stratosphere
35. High pressure system. when cool air in the upper atmosphere has higher density than its surrounding - creating high pressure system. It moves twd the ground - so air moves way from the high pressure system near earth's surface
winds
layers of atmosphere
anticyclone
clouds
36. Low pressure system. When an air mass near the ground is heated - the air molecules vibrate faster - cause the air mass to expand and its density to decrease. With a lower density than the surrounding air - the mass rises to create a low pressure reg
relative humidity
cyclone
absolute humidity
adiabatic cooling