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