Determining the level of global solar radiation on the earth's surface

dc.contributor.authorDostál, Zdeněk
dc.contributor.authorĎulík, Miroslav
dc.date.accessioned2016-07-15T09:12:25Z
dc.date.available2016-07-15T09:12:25Z
dc.date.issued2015
dc.description.abstractThe article analyzes the Earth's surface insolation. For the analysis, two methods are described - the method of approximate calculation and turbidity method using Linke turbidity index. The methods consider the latitude of current location on the Earth's surface, atmosphere attenuation and other major factors. To obtain more accurate values, long-term measurements at the current location should be obtained.cs
dc.format.extent509803 bytes
dc.format.mimetypeapplication/pdf
dc.identifier.citationAdvances in electrical and electronic engineering. 2015, vol. 13, no. 5, p. 471-477 : ill.cs
dc.identifier.doi10.15598/aeee.v13i5.1391
dc.identifier.issn1336-1376
dc.identifier.issn1804-3119
dc.identifier.urihttp://hdl.handle.net/10084/111881
dc.language.isoencs
dc.publisherVysoká škola báňská - Technická univerzita Ostravacs
dc.relation.ispartofseriesAdvances in electrical and electronic engineeringcs
dc.relation.urihttp://dx.doi.org/10.15598/aeee.v13i5.1391cs
dc.rights© Vysoká škola báňská - Technická univerzita Ostrava
dc.rightsCreative Commons Attribution 3.0 Unported (CC BY 3.0)
dc.rights.accessopenAccess
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectinsolation of the Earth's surfacecs
dc.subjectmethod of approximate calculationcs
dc.subjectrenewable energy resourcescs
dc.subjectturbidity methodcs
dc.titleDetermining the level of global solar radiation on the earth's surfacecs
dc.typearticlecs
dc.type.statusPeer-reviewedcs
dc.type.versionpublishedVersioncs

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