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A 561-yr (1461-2022 CE) summer temperature reconstruction for Mid-Atlantic-Northeast USA shows connections to volcanic forcing and atmospheric circulation

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F24%3A00598464" target="_blank" >RIV/86652079:_____/24:00598464 - isvavai.cz</a>

  • Result on the web

    <a href="https://link.springer.com/article/10.1007/s10584-024-03798-z" target="_blank" >https://link.springer.com/article/10.1007/s10584-024-03798-z</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s10584-024-03798-z" target="_blank" >10.1007/s10584-024-03798-z</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    A 561-yr (1461-2022 CE) summer temperature reconstruction for Mid-Atlantic-Northeast USA shows connections to volcanic forcing and atmospheric circulation

  • Original language description

    Contextualizing current increases in Northern Hemisphere temperatures is precluded by the short instrumental record of the past ca. 120 years and the dearth of temperature-sensitive proxy records, particularly at lower latitudes south of <50 degrees N. We develop a network of 29 blue intensity chronologies derived from tree rings of Tsuga canadensis (L.) Carri & egravere and Picea rubens Sarg. trees distributed across the Mid-Atlantic and Northeast USA (MANE)-a region underrepresented by multi-centennial temperature records. We use this network to reconstruct mean March-September air temperatures back to 1461 CE based on a model that explains 62% of the instrumental temperature variance from 1901-1976 CE. Since 1998 CE, MANE summer temperatures are consistently the warmest within the context of the past 561 years exceeding the 1951-1980 mean of +1.3 degrees C. Cool summers across MANE were frequently volcanically forced, with significant (p<0.05) temperature departures associated with 80% of the largest tropical (n=13) and extratropical (n=15) eruptions since 1461 CE. Yet, we find that more of the identified cool events in the record were likely unforced by volcanism and either related to stochastic variability or atmospheric circulation via significant associations (p<0.05) to regional, coastal sea-surface temperatures, 500-hpa geopotential height, and 300-hpa meridional and zonal wind vectors. Expanding the MANE network to the west and south and combining it with existing temperature-sensitive proxies across North America is an important next step toward producing a gridded temperature reconstruction field for North America.

  • 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

    10511 - Environmental sciences (social aspects to be 5.7)

Result continuities

  • Project

  • 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

    Climatic Change

  • ISSN

    0165-0009

  • e-ISSN

    1573-1480

  • Volume of the periodical

    177

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    23

  • Pages from-to

    144

  • UT code for WoS article

    001307862700001

  • EID of the result in the Scopus database

    2-s2.0-85203250294