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