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