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