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The trends of sunshine on the meteorological stations with the long period of measurement
dc.contributor.advisorSládek, Ivan
dc.creatorOpatrná, Petra
dc.date.accessioned2017-04-18T07:55:46Z
dc.date.available2017-04-18T07:55:46Z
dc.date.issued2009
dc.identifier.urihttp://hdl.handle.net/20.500.11956/20020
dc.description.abstractOne of the main objectives of this thesis is to identify the trends of sunshine which was measured on the meteorological stations and to explain it by the help of synoptical situations. Further, I would like to define the period, in which the days without sunshine dominate and the period, when the total of sunshine is higher, and to determine their influence on human's organism by means of the T and H index. I used data from eight meteorological stations, which are equable dislocated all around Czech Republic and are situated in the different elevations above sea level. Two of these meteorological stations (Praha - Karlov and Milešovka) have series of measurements which are in time longer than eighty years. In the first part of this thesis, I describe the measurement of sunshine and the factors, which affect it. Then I focus on the year totals of sunshine and I uncover their trends. The final chapters deal with the periods without sunshine which are called the dark periods and with the periods with higher total of sunshine which are called the periods of sunshine plentitude and their peripheries. The amount of sunshine had been going up until the fifties of the last century, after that came a distinct fall to the eighties when the trend was changing again and was raising up slowly. This fact harmonizes with...en_US
dc.languageČeštinacs_CZ
dc.language.isocs_CZ
dc.publisherUniverzita Karlova, Přírodovědecká fakultacs_CZ
dc.titleTrendy slunečního svitu na meteorologických stanicích s dlouhou dobou měřenícs_CZ
dc.typediplomová prácecs_CZ
dcterms.created2009
dcterms.dateAccepted2009-05-27
dc.description.departmentDepartment of Physical Geography and Geoecologyen_US
dc.description.departmentKatedra fyzické geografie a geoekologiecs_CZ
dc.description.facultyFaculty of Scienceen_US
dc.description.facultyPřírodovědecká fakultacs_CZ
dc.identifier.repId33921
dc.title.translatedThe trends of sunshine on the meteorological stations with the long period of measurementen_US
dc.contributor.refereeHostýnek, Jiří
dc.identifier.aleph001125201
thesis.degree.nameMgr.
thesis.degree.levelnavazující magisterskécs_CZ
thesis.degree.disciplineFyzická geografie a geoekologiecs_CZ
thesis.degree.disciplinePhysical Geography and Geoecologyen_US
thesis.degree.programGeografiecs_CZ
thesis.degree.programGeographyen_US
uk.thesis.typediplomová prácecs_CZ
uk.taxonomy.organization-csPřírodovědecká fakulta::Katedra fyzické geografie a geoekologiecs_CZ
uk.taxonomy.organization-enFaculty of Science::Department of Physical Geography and Geoecologyen_US
uk.faculty-name.csPřírodovědecká fakultacs_CZ
uk.faculty-name.enFaculty of Scienceen_US
uk.faculty-abbr.csPřFcs_CZ
uk.degree-discipline.csFyzická geografie a geoekologiecs_CZ
uk.degree-discipline.enPhysical Geography and Geoecologyen_US
uk.degree-program.csGeografiecs_CZ
uk.degree-program.enGeographyen_US
thesis.grade.csDobřecs_CZ
thesis.grade.enGooden_US
uk.abstract.enOne of the main objectives of this thesis is to identify the trends of sunshine which was measured on the meteorological stations and to explain it by the help of synoptical situations. Further, I would like to define the period, in which the days without sunshine dominate and the period, when the total of sunshine is higher, and to determine their influence on human's organism by means of the T and H index. I used data from eight meteorological stations, which are equable dislocated all around Czech Republic and are situated in the different elevations above sea level. Two of these meteorological stations (Praha - Karlov and Milešovka) have series of measurements which are in time longer than eighty years. In the first part of this thesis, I describe the measurement of sunshine and the factors, which affect it. Then I focus on the year totals of sunshine and I uncover their trends. The final chapters deal with the periods without sunshine which are called the dark periods and with the periods with higher total of sunshine which are called the periods of sunshine plentitude and their peripheries. The amount of sunshine had been going up until the fifties of the last century, after that came a distinct fall to the eighties when the trend was changing again and was raising up slowly. This fact harmonizes with...en_US
uk.publication.placePrahacs_CZ
uk.grantorUniverzita Karlova, Přírodovědecká fakulta, Katedra fyzické geografie a geoekologiecs_CZ
dc.identifier.lisID990011252010106986


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