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