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