Cloud formation in different scales and their impact on water isotope signature

A tétel rövid nézete
dc.contributor.advisorLászló, Elemér
dc.contributor.authorSampaio, Mariana Souza
dc.contributor.departmentDE--Természettudományi és Technológiai Kar--Földtudományi Intézethu_HU
dc.date.accessioned2022-05-05T12:56:32Z
dc.date.available2022-05-05T12:56:32Z
dc.date.created2022-05-04
dc.description.abstractThe isotopic content of precipitation is an important hydrological tracer and a key element for understanding the water circulation on the Earth and variations in the composition depend on individual atmospheric cooling processes, dynamical and microphysical states of downpour formations, and other factors in cloud formation. This study proposes an algorithm for disaggregation of precipitation types using SYNOP reports of six weather stations in Europe and builds a correlation between convective and stratiform precipitation amounts and atmospheric contents of tritium and stable isotopes.hu_HU
dc.description.correctortben
dc.description.courseEarth Scienceshu_HU
dc.description.degreeBSc/BAhu_HU
dc.format.extent42hu_HU
dc.identifier.urihttp://hdl.handle.net/2437/332421
dc.language.isoenhu_HU
dc.subjectStable isotopehu_HU
dc.subjectOxygen-18hu_HU
dc.subjectTritiumhu_HU
dc.subjectSYNOPhu_HU
dc.subjectConvective precipitationhu_HU
dc.subjectStratiform precipitationhu_HU
dc.subject.dspaceMeteorologyhu_HU
dc.subject.dspaceEarth Scienceshu_HU
dc.titleCloud formation in different scales and their impact on water isotope signaturehu_HU
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Gyűjtemények
Theses (Faculty of Science and Technology)