Number of the records: 1  

Tree-ring record of winter temperature from Humla, Karnali, in central Himalaya: a 229 years-long perspective for recent warming trend

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    SYSNO ASEP0534306
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleTree-ring record of winter temperature from Humla, Karnali, in central Himalaya: a 229 years-long perspective for recent warming trend
    Author(s) Gaire, N. P. (NP)
    Fan, Z.-X. (CN)
    Shah, S. K. (IN)
    Thapa, U. K. (US)
    Rokaya, Maan Bahadur (UEK-B) RID, ORCID, SAI
    Number of authors5
    Source TitleGeografiska Annaler Series A-Physical Geography. - : Taylor & Francis - ISSN 0435-3676
    Roč. 102, č. 3 (2020), s. 297-316
    Number of pages19 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordswestern nepal himalaya ; climate-change ; surface-temperature ; summer temperature ; tibetan plateau ; reconstruction ; growth ; variability ; precipitation ; atlantic ; Tree rings ; climate change ; winter temperature ; Nepal Himalaya ; enso ; Abies spectabilis
    Subject RIVEF - Botanics
    OECD categoryClimatic research
    Method of publishingLimited access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000528475100001
    EID SCOPUS85085006491
    DOI10.1080/04353676.2020.1751446
    AnnotationTree rings are widely used to reconstruct past climates in regions where observational records of climate are short. In this study, we developed a 294 years-long (1718-2011 CE) ring-width chronology of the Himalayan Silver fir (Abies spectabilis (D.Don, Spach)) from Humla district in western Nepal to reconstruct winter minimum temperature for the remote region of central Himalaya where instrumental records are limited to past three or four decades. Ring-width chronology of the Himalayan Silver fir showed strongest and significant positive correlation with minimum winter temperature prior to the growing season. Based on this relationship, we reconstructed the winter season (previous October-current February) minimum temperature for western Nepal covering the period of 1780-2008 CE. Our reconstruction showed that winter minimum temperature is continuously increasing since the early twentieth century with unprecedented rapid warming in the latter half. The cold episodes in the reconstruction coincided with the major volcanic eruptions in the Northern Hemisphere and tropical regions. The spectral analysis using Multi-Taper Method revealed that the winter temperature in the north-western Himalaya has short- to medium-term periodicities of 2-3, 5.8-6.2, 7.9-8.2, 39-46 and 56-73 years, which suggest possible teleconnections with ENSO (El-Nino Southern Oscillation) and AMO (Atlantic Multidecadal Oscillation).
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2021
    Electronic addresshttps://www.tandfonline.com/doi/full/10.1080/04353676.2020.1751446
Number of the records: 1  

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