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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. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
relative humidity
lower pressure
pressure
dew point
2. Amount of water vapor an aim mass holds. air can dissolve water
humidity
layers of atmosphere
anticyclone
cyclone
3. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
stratosphere
relative humidity
cyclone
stratosphere
4. 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
cyclone
winds
lower pressure
troposphere
5. 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
lower pressure
cyclone
clouds
temp in troposphere
6. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
lower pressure
adiabatic cooling
pressure
absolute humidity
7. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
clouds
humidity
winds
pressure
8. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
pressure
humidity
atmosphere
clouds
9. 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
humidity
layers of atmosphere
anticyclone
layers of atmosphere
10. 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
temp in troposphere
lower pressure
troposphere
relative humidity
11. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
winds
cyclone
dew point
relative humidity
12. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
troposphere
humidity
winds
dew point
13. Amount of water vapor an aim mass holds. air can dissolve water
relative humidity
temp in troposphere
humidity
lower pressure
14. Daily fluctuations in temperature - wind speed - and precipitation
absolute humidity
winds
winds
weather
15. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
humidity
stratosphere
anticyclone
lower pressure
16. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
dew point
atmosphere
layers of atmosphere
humidity
17. 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
relative humidity
humidity
anticyclone
humidity
18. 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.
weather
cyclone
atmosphere
adiabatic cooling
19. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
humidity
clouds
weather
pressure
20. 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.
humidity
temp in troposphere
troposphere
absolute humidity
21. 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.
cyclone
weather
adiabatic cooling
anticyclone
22. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
anticyclone
atmosphere
clouds
layers of atmosphere
23. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
relative humidity
lower pressure
atmosphere
adiabatic cooling
24. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
layers of atmosphere
layers of atmosphere
atmosphere
cyclone
25. 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
clouds
cyclone
relative humidity
lower pressure
26. Mount of water vapor in the air
anticyclone
stratosphere
absolute humidity
cyclone
27. 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
layers of atmosphere
anticyclone
temp in troposphere
absolute humidity
28. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
pressure
dew point
pressure
temp in troposphere
29. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
weather
winds
stratosphere
layers of atmosphere
30. Daily fluctuations in temperature - wind speed - and precipitation
humidity
stratosphere
atmosphere
weather
31. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
clouds
relative humidity
pressure
dew point
32. 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
winds
cyclone
relative humidity
lower pressure
33. 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
absolute humidity
clouds
pressure
layers of atmosphere
34. 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.
winds
layers of atmosphere
troposphere
stratosphere
35. 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
relative humidity
absolute humidity
stratosphere
temp in troposphere
36. Mount of water vapor in the air
absolute humidity
pressure
adiabatic cooling
weather