Atmospheric Science: Winds And Air Currents (1986)

Creator: A/V Geeks 16mm Films

Description: Illustrates how different sized convection cells produce land- seal breezes, monsoons and, on a giant scale, trade winds. Also shows how winds are lifted by mountains and how unusual warm and cold winds descend from them. We digitized and uploaded this film from the A/V Geeks 16mm Archive. Email us at footage@avgeeks.com if you have questions about the footage and are interested in using it in your project.

Transcription

for [Music] 9:00 a.m. Sailors wait for the first breath of wind as yet there's not a breath to be felt in the meantime there's plenty of work to be done they know it's only a matter of time before the wind kicks up but where is the wind is it out there beyond the harbor working its way slowly toward the land wind is air in motion you can't see it but you can see its [Music] effect so you can see what wind does but how do you study something you don't really see one good way of studying wind is to look at water because air and water are both fluids they behave much alike a similarity filmmakers use to create special atmospheric effects [Music] atmospheric scientists use tank simulations to study wind the fluid is set in motion by a heat source as the water warms it rises and surrounding water moves in to take its place this kind of flow pattern produced by heat is called a convection [Music] cell the same thing happens in the atmosphere here a hot sunbaked field produces a convection cell it's rising column of air is called a thermal by searching out thermals so soaring birds can travel hundreds of miles without flapping a wing and they aren't the only ones that ride thermals climbing at 5 m a second a sail plane can soar High into the sky the pilot Maneuvers his craft carefully keeping it within the rising currents of air the sunw warmed land below is the heat source for this small atmospheric convection cell a greater mass of air rises from a sunwarm tropical island as the sun comes up it heats the land causing air over the land to rise this warm Rising air draws in cooler air from Over the Water This seab breeze May blow in from all sides and the moist Rising air produces a towering stack of cumulus clouds then at night when the land cools the wind reverses since it now blows from the land side it's called a land breeze along coastlines the same thing happens it's now late morning the sun has heated the land and the convection cell has formed the awaited seab breeze has arrived [Music] it's a fine Breeze out of the harbor wind fills the sails bringing hours of steady sailing from wind generated by this giant convection [Music] cell Steam from a nearby power plant shows the direction of the seab breeze wind will hold steady all afternoon but as evening Falls it gradually stops and reverses Direction [Music] here the daily land breeze seab Breeze cycle creates Coastal winds but in other parts of the world a seab breeze likee pattern follows a seasonal cycle and affects entire continents as the continent of Asia soaks up summer heat air begins Rising this huge atmospheric convection cell draws in moist air from surrounding oceans [Music] clouds swarm over the land bringing Monsoon rains welcome after many months of Aid [Music] conditions nearly half the world's population depends on the monsoon for lifegiving water [Music] of course some places get more rain than others to the Village of cherapunji in India the monsoon wind brings a particularly heavy load of rain in a heavy monsoon season cherapunji receives some 25 M of rain over 80 ft of water some winds sweep over the entire Globe year round near the equator the Tropical Sun generates the largest convection cell on Earth the return flow from this convection cell is deflected by Earth's spin forming the trade winds and in the mid latitudes where many of us live prevailing Westerly winds form great bands embedded in this prevailing flow are the storm systems which bring rain and snow so wind from Coastal winds to monsoons to prevailing winds is set in motion by heat but once in motion a wind's flow can be affected by obstacles like mountains Rising thousands of feet mountains change the flow twisting bending swirling around the wind becomes erratic changing direction and stirring up the powdery snow where wind funnels between mountains it picks up speed sometimes with enough forc to tumble rocks and blow down [Music] trees but now and then an unusual Mountain wind sweeps down bringing a day of warmth in the middle of ski season it's called a shinook the shanuk occurs when air rising up one side of a mountain loses its moisture in rain and snow flowing over this dry air is compressed by the weight of the atmosphere above causing its temperature to rise melting the snow a much colder type of wind begins in the still of high mountain plateaus here protected by the surrounding mountains air gathers for weeks taking on the temperature of the Frozen land then set in motion by its own weight this icy air spills over with chilling [Music] effect when wind flows over a range of mountains it's pushed up into a Mountain Wave these saucer-shaped clouds indicate that a strong wave is building sail plane Pilots carrying oxygen have ridden these Mountain waves to 46,000 ft 14,000 M along a coast Cliffs also create a wave of air these gulls hover leisurely in the updraft like H glider Pilots who use these waves to stay Al Loft for hours at a [Music] time wherever the wind blows people have learned to harness its power [Music] wind air set in motion by the energy of the Sun [Music] [Music] [Music] [Music]

Online Copy: https://www.youtube.com/watch?v=leqqrH2A-NQ

Metadata Source:YouTube


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