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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. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
weather
stratosphere
relative humidity
atmosphere
2. 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.
clouds
dew point
adiabatic cooling
cyclone
3. 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
stratosphere
anticyclone
temp in troposphere
4. 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
lower pressure
weather
cyclone
5. Daily fluctuations in temperature - wind speed - and precipitation
weather
cyclone
troposphere
winds
6. 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.
clouds
cyclone
troposphere
humidity
7. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
troposphere
stratosphere
adiabatic cooling
humidity
8. Envelope of gases surrounding earth - extending from the surface to about 10 -000 km above
cyclone
clouds
stratosphere
atmosphere
9. 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
pressure
clouds
10. 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.
pressure
anticyclone
relative humidity
adiabatic cooling
11. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
absolute humidity
relative humidity
adiabatic cooling
clouds
12. Ratio of observed absolute humidity divided by sbsolute humidity at dew point
absolute humidity
relative humidity
cyclone
humidity
13. 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
temp in troposphere
clouds
cyclone
14. 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
adiabatic cooling
absolute humidity
clouds
troposphere
15. Amount of water vapor an aim mass holds. air can dissolve water
absolute humidity
troposphere
temp in troposphere
humidity
16. 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.
atmosphere
troposphere
weather
winds
17. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
winds
pressure
lower pressure
clouds
18. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
humidity
temp in troposphere
relative humidity
atmosphere
19. Mount of water vapor in the air
layers of atmosphere
clouds
absolute humidity
stratosphere
20. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
anticyclone
absolute humidity
pressure
relative humidity
21. 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
cyclone
relative humidity
troposphere
22. Contains ozone layer - temperature increases upward due to oxygen - which absorbs UV radiation
dew point
atmosphere
adiabatic cooling
stratosphere
23. 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
dew point
anticyclone
winds
winds
24. Depends on temp; cold air can dissolve little water whereas warm air can dissolve a lot.
humidity
anticyclone
weather
lower pressure
25. Amount of water vapor an aim mass holds. air can dissolve water
absolute humidity
humidity
absolute humidity
weather
26. 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
absolute humidity
absolute humidity
humidity
27. 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
anticyclone
troposphere
atmosphere
28. Average atmospheric pressure at sea level equals 14.7 lbs. due to weight of overlying air column
layers of atmosphere
pressure
adiabatic cooling
lower pressure
29. Mount of water vapor in the air
temp in troposphere
stratosphere
absolute humidity
dew point
30. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
layers of atmosphere
temp in troposphere
pressure
absolute humidity
31. Daily fluctuations in temperature - wind speed - and precipitation
weather
cyclone
relative humidity
absolute humidity
32. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
layers of atmosphere
anticyclone
weather
dew point
33. When it is water saturated (the maximum amount of water that the air mass can hold at a given temperature
winds
relative humidity
winds
dew point
34. Atmosphere has layered structure. defined by temp - pressure - and chemical composition
anticyclone
adiabatic cooling
pressure
layers of atmosphere
35. 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
absolute humidity
weather
dew point
temp in troposphere
36. Differences in air pressures between high and low pressure systems. The larger the differences in air pressures - the stronger they are
winds
cyclone
adiabatic cooling
stratosphere