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Data · dataset · 2026

Diurnal soil freeze‐thaw cycles and the factors determining their changes in warming climate in the Upper Brahmaputra Basin of the Tibetan Plateau

Listed in National Center for Atmospheric Research

The number of diurnal freeze‐thaw cycles (DFTC) in shallow soil increase slightly during the period 1980–2018 in the upper Brahmaputra (UB) basinAir temperature effects on the changes in DFTC frequency center on the freezing pointSnowfall plays a more important role in the temporal variability of DFTC than rainfall

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SourceKeyLast seenRaw
National Center for Atmospheric Research5b427c7d-4800-442c-addf-586469ca627313 d agoJSON v1
FieldAssertionExtractorEvidence
concepts[field].local:field:earth-environmentalmapping · data ucar educonnector:data_ucar_edu@1.0.0
concepts[field].local:field:ocean-atmosphericmapping · data ucar educonnector:data_ucar_edu@1.0.0
created_datesource · data ucar educonnector:data_ucar_edu@1.0.0
descriptionsource · data ucar educonnector:data_ucar_edu@1.0.0/notes
publication_datesource · data ucar educonnector:data_ucar_edu@1.0.0
titlesource · data ucar educonnector:data_ucar_edu@1.0.0/title
updated_datesource · data ucar educonnector:data_ucar_edu@1.0.0