THE TEMPERATURE OF THE PLANET EARTH IN LATITUDE 850-250 DEGREES NORTH

dc.contributor.authorM. Mukhammadieva
dc.contributor.authorJ. Ishchanov
dc.contributor.authorM. Mirhosilova
dc.contributor.authorE. Shermatov
dc.date.accessioned2025-12-29T18:16:44Z
dc.date.issued2025-01-17
dc.description.abstractIn the past, hydrometeorology took into account the total thermal impact of radiation on certain geospheres. At the same time, the magnitude of this radiation flux outside the Earth was assumed to be constant.
dc.formatapplication/pdf
dc.identifier.urihttps://webofjournals.com/index.php/4/article/view/2893
dc.identifier.urihttps://asianeducationindex.com/handle/123456789/25395
dc.language.isoeng
dc.publisherWeb of Journals Publishing
dc.relationhttps://webofjournals.com/index.php/4/article/view/2893/2855
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/4.0
dc.sourceWeb of Technology: Multidimensional Research Journal; Vol. 3 No. 1 (2024): WOT; 39-42
dc.source2938-3757
dc.subjectHydrometeorology, solar radiation, Earth, climate, solar constant, earth's atmosphere, thermodynamics, atmosphere, absolute magnitude, cosmic rays, amplitude, latitude, correlation coefficient, mineralization.
dc.titleTHE TEMPERATURE OF THE PLANET EARTH IN LATITUDE 850-250 DEGREES NORTH
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typePeer-reviewed Article

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