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dc.contributor.authorRamos, Isabel
dc.contributor.authorDe la Cruz, Gustavo
dc.contributor.authorSuarez, Wilson
dc.coverage.spatialArequipa
dc.date.accessioned2022-04-22T21:11:09Z
dc.date.available2022-04-22T21:11:09Z
dc.date.issued2018
dc.identifier.urihttps://hdl.handle.net/20.500.12542/1977
dc.description.abstractThe main objective of this work is to analyze the influence of cloud cover on shortwave radiation incident of the Nevado Coropuna during 2015-2016. In this presentation they propose to discuss that Arequipa, during the day, has more clouds between December to March above 80%. At night the cloudiness diminish significantly, hourly there are more clouds in the afternoon. The NC has a similar pattern, and there is a difference among the oriental and occidental side. Also, propose the cloudiness radiation has a high impact in the incident shortwave, in clear moments the radiation could reach 1200 W/m2, meanwhile with cloudiness this does not pass the 600 W/m2. In the dry period, generally there are not clouds; in the conventional meteorological stations are found predominantly high clouds, cirrus.es_PE
dc.formatapplication/pdfes_PE
dc.language.isospaes_PE
dc.publisherServicio Nacional de Meteorología e Hidrología del Perúes_PE
dc.relationProyecto CRYOPERU 144-2015es_PE
dc.rightsinfo:eu-repo/semantics/openAccesses_PE
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.sourceRepositorio Institucional - SENAMHIes_PE
dc.sourceServicio Nacional de Meteorología e Hidrología del Perúes_PE
dc.subjectGlaciareses_PE
dc.subjectCloud Radiationes_PE
dc.titleInfluence of cloudiness on the incident shortwave radiation of Nevado Coropunaes_PE
dc.typeinfo:eu-repo/semantics/lecturees_PE
dc.identifier.doihttps://doi.org/10.13140/RG.2.2.28699.92966
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.11es_PE
dc.publisher.countryPEes_PE
dc.subject.siniavariabilidad climatica - Clima y Eventos Naturales
dc.type.siniatext/libro.presentacion
dc.identifier.urlhttps://hdl.handle.net/20.500.12542/1977


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