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