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