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dc.rights.licenseAtribución-NoComercial-SinDerivadas 2.5 Colombia (CC BY-NC-ND 2.5 CO)*
dc.contributor.authorBunyard, Peterspa
dc.date.accessioned2015-08-21T18:53:51Zspa
dc.date.accessioned2016-05-11T14:38:11Zspa
dc.date.accessioned2017-05-16T19:01:51Zspa
dc.date.available2015-08-21T18:53:51Zspa
dc.date.available2016-05-11T14:38:11Zspa
dc.date.available2017-05-16T19:01:51Zspa
dc.date.created2014spa
dc.date.issued2014-02spa
dc.identifier.isbn978-958-8745-89-3spa
dc.identifier.urihttp://hdl.handle.net/11232/397eng
dc.description.abstractthe Biotic Pump Theory, as set forward by Drs. Makarieva and Gorshkov, states that the primary force driving surface winds, certainly in the tropics, is induced by the negative changes in atmospheric pressure caused by condensation of water vapour when clouds form. A high rate of condensation is necessary and therefore the theory requires that a suffciently high rate of evapotranspiration from large areas of forest provides the "fuel" for the process. The theory therefore runs contrary to the traditional view, as introduced in climate models, that surface winds are the sole products of differences in surface heating as well as of latent heat release during the process of condensation. Indeed, Makarieva and her colleagues claim that transitions in the phases of water play a far more important role in driving atmospheric dynamics than is currently recognisedspa
dc.description.abstractLa teoría de la bomba biótica , establece que la primera fuerza motriz de los vientos de superficie, sobre todo en los trópicos , es inducida por los cambios negativos en la presión atmosférica causada por la condensación de vapor de agua cuando las nubes se forman. Una alta velocidad de condensación es necesaria y por lo tanto, la teoría requiere que una alta evapotranspiración de grandes áreas de bosques que proporcionan el "combustible" para el proceso. Por consiguiente, la teoría va en contra de la visión tradicional , como se presentó en los modelos climáticos , que los vientos de superficie son los únicos productos de diferencias de calentamiento de la superficie, así como de la liberación del calor latente durante el proceso de condensación. De hecho , Makarieva y sus colegas afirman que las transiciones en las fases de agua juegan un papel más importante en el impulso de la dinámica atmosférica de lo que se reconoce actualmente.spa
dc.format.extent114spa
dc.format.mediumDigitalspa
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherUniversidad Sergio Arboledaspa
dc.relation.ispartofseriesInvestigaciónspa
dc.rightshttp://repository.usergioarboleda.edu.co/bitstream/id/5bccc72d-7e6d-4f64-ab18-bad93c49a567/license.txteng
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/2.5/co/*
dc.titleHow the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.eng
dc.subject.lembClimatologíaspa
dc.subject.lembCirculación atmosféricaspa
dc.subject.lembCiclo hidrológicospa
dc.subject.lembTeoría de la bomba bióticaspa
dc.subject.lembClimatologyeng
dc.subject.lembAtmospheric circulationeng
dc.subject.lembHydrologic cycleeng
dc.subject.lembOTHER Biotic pump theoryeng
dc.publisher.programInstituto de Estudios y Servicios Ambientales - IDEASAspa
dc.rights.accesoAbierto (Texto Completo)spa
dc.type.coarversionhttp://purl.org/coar/version/c_970fb48d4fbd8a85spa
dc.identifier.doihttps://doi.org/10.22518/9789588745886eng
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