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Joshua N.`s SFP
Joshua N.`s SFP

...  The clouds move from left to right. In the night time you really cant see it. The thing about clouds are that you can right through them. It may look like it’s a solid but its not. A cloud is just a visible collection of particles of water or ice suspended in the air, usually at an elevation above ...


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... relationship  between  hurricanes,  the  ocean  and  the  Sun.       a. _____________________  play  an  important  role  in  the  formation  of  tropical   ________________________  and  ______________________________________  because   ______________ ...
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... A weather satellite is a type of satellite that is primarily used to monitor the weather and climate of the Earth. Satellites can be either polar orbiting, seeing the same swath of the Earth every 12 hours, or geostationary, hovering over the same spot on Earth by orbiting over the equator while mov ...
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... In low pressure areas, air is less _______ in areas of higher pressure. The low pressure rise Moist water vapor can rise allows air to _____. and form _____________. storm clouds Low pressure areas, or lows, are shown by “L” symbols. Low barometric pressure supports unstable, and sometimes stormy we ...
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5.07 Wind
5.07 Wind

... Anabatic Wind Slopes of hills not covered by snow will be warmed during the day. The air in contact with them becomes warmer and less dense and therefore flows up the slope. Also known as a Valley Breeze. ...
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... heated cylinders, where each cylinder releases an equal, uniform heat flux distribution q 00 and a Boussinesq approximation is introduced to represent buoyancy effects. Periodic boundary conditions are enforced along the cross flow directions y and z as well as the streamwise direction x on all comp ...
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... much must the air cool for dew to form that night? Question 4: The relative humidity is 90% at a noon-time temperature of 75°F (297°K). At what temperature will dew form that night? Notice that dew will form at higher temperature if the relative humidity is greater. Question 5: If Td = T, what is re ...
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Atmospheric convection



Atmospheric convection is the result of a parcel-environment instability, or temperature difference, layer in the atmosphere. Different lapse rates within dry and moist air lead to instability. Mixing of air during the day which expands the height of the planetary boundary layer leads to increased winds, cumulus cloud development, and decreased surface dew points. Moist convection leads to thunderstorm development, which is often responsible for severe weather throughout the world. Special threats from thunderstorms include hail, downbursts, and tornadoes.
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