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Tree-Ring Chronologies from the Upper Treeline in the Russian Altai Mountains Reveal Strong and Stable Summer Temperature Signals

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F24%3A00598470" target="_blank" >RIV/86652079:_____/24:00598470 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/24:00138940

  • Result on the web

    <a href="https://www.mdpi.com/1999-4907/15/8/1402" target="_blank" >https://www.mdpi.com/1999-4907/15/8/1402</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3390/f15081402" target="_blank" >10.3390/f15081402</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Tree-Ring Chronologies from the Upper Treeline in the Russian Altai Mountains Reveal Strong and Stable Summer Temperature Signals

  • Original language description

    Radial tree growth at high-elevation and high-latitude sites is predominantly controlled by changes in summer temperature. This relationship is, however, expected to weaken under projected global warming, which questions the reliability of tree-ring chronologies for climate reconstructions. Here, we examined the growth-climate response patterns of five tree-ring width (TRW) and maximum latewood density (MXD) chronologies of larch (Larix sibirica) from upper-treeline ecotones in the Altai Mountains, which is a key region for developing millennial-long dendroclimatic records in inner Eurasia. The TRW and MXD chronologies exhibited significant year-to-year coherency within and between the two parameters (p < 0.001). While TRW is mostly influenced by temperature changes during the first half of the growing season from June to July (r = 0.66), MXD is most strongly correlated with May-August temperatures (r = 0.73). All seasonal temperature signals are statistically significant at the 99% confidence level, temporally stable back to 1940 CE, the period with reliable instrumental measurements, and spatially representative for a vast area of inner Eurasia between northeastern Kazakhstan in the west, northern Mongolia in the east, southern Russia in the north and northwestern China in the south. Our findings demonstrate the paleoclimatic potential of TRW and especially MXD chronologies and reject any sign of the <acute accent>divergence problem<acute accent> at these high-elevation, mid-latitude larch sites.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    40102 - Forestry

Result continuities

  • Project

    <a href="/en/project/GA23-08049S" target="_blank" >GA23-08049S: Central European HYDRoclimate from Oak stable isotopes over the past 8000 years – HYDRO8</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Forests

  • ISSN

    1999-4907

  • e-ISSN

    1999-4907

  • Volume of the periodical

    15

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    CH - SWITZERLAND

  • Number of pages

    13

  • Pages from-to

    1402

  • UT code for WoS article

    001306724900001

  • EID of the result in the Scopus database

    2-s2.0-85202680312