Atmospheric circulation

dc.contributorUniversidade Estadual Paulista (UNESP)
dc.creatorU.S. Geological Survey
dc.date2016-10-26T18:11:14Z
dc.date2016-10-26T18:11:14Z
dc.date.accessioned2017-04-06T13:16:26Z
dc.date.available2017-04-06T13:16:26Z
dc.identifierhttp://acervodigital.unesp.br/handle/unesp/372227
dc.identifierhttp://objetoseducacionais2.mec.gov.br/handle/mec/24180
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/968509
dc.descriptionThe image shows the dunes displacement by the eolic action. The sand moves in the same direction of the wind to the top of the dune, by saltation or fluency. When the sand accumulation is greater than the angle of repose, the grains slide downwind. So, the dune is displaced by the repetition of these movements
dc.descriptionEducação Superior::Ciências Exatas e da Terra::GeoCiências
dc.publisherU.S. Geological Survey
dc.relationcirculate.gif
dc.rightsUSGS-authored or produced data and information are considered to be in the U.S. public domain. When using information from USGS information products, publications, or Web sites, we ask that proper credit be given
dc.subjectEducação Superior::Ciências Exatas e da Terra::Geociências::Climatologia
dc.subjectAtmospheric circulation; Global atmospheric circulation
dc.titleAtmospheric circulation
dc.typeimagem


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