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