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

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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Related Links

Related Dataset #1 : NASA Shuttle Radar Topography Mission Global 3 arc second

Related Dataset #2 : MCD12Q1 MODIS/Terra+Aqua Land Cover Type Yearly L3 Global 500m SIN Grid V006

Related Dataset #3 : MOD13A2 MODIS/Terra Vegetation Indices 16-Day L3 Global 1km SIN Grid V006
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Copyright 2024 American Geophysical Union.
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Author Li, N.
Cuo, L.
Zhang, Yongxin
Flerchinger, G.
Publisher UCAR/NCAR - Library
Publication Date 2024-10-01T00:00:00
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Topic Category geoscientificInformation
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Metadata Date 2025-07-10T19:58:22.580003
Metadata Record Identifier edu.ucar.opensky::articles:42289
Metadata Language eng; USA
Suggested Citation Li, N., Cuo, L., Zhang, Yongxin, Flerchinger, G.. (2024). Diurnal soil freeze‐thaw cycles and the factors determining their changes in warming climate in the Upper Brahmaputra Basin of the Tibetan Plateau. UCAR/NCAR - Library. https://n2t.net/ark:/85065/d74j0kd9. Accessed 04 August 2025.

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