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