NOAA/WDS Paleoclimatology - Hantemirov - Yamal - LASI - ITRDB RUSS223

browse graphicPaleoclimatology - Tree Ring
This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Tree Ring. The data include parameters of tree ring with a geographic location of Russia, Eastern Europe. The time period coverage is from 2714 to -55 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
  • Cite as: Hantemirov, R.M.; Shiyatov, S.G.; Surkov, A.; Gorlanova, L. (2013-05-21): NOAA/WDS Paleoclimatology - Hantemirov - Yamal - LASI - ITRDB RUSS223. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/ekha-nr57. Accessed [date].
  • Please refer to Credit tab for full citation information.
noaa-tree-15339
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Ordering InstructionsContact NCEI for other distribution options and instructions.
DistributorNOAA National Centers for Environmental Information
ncei.info@noaa.gov
Dataset Point of Contact NOAA National Centers for Environmental Information
ncei.info@noaa.gov
Dataset Point of Contact Data Center Contact
NOAA World Data Service for Paleoclimatology
828-271-4800
paleo@noaa.gov
Coverage DescriptionDate Range: -764 CE to 2005 CE; Date Range: 2714 cal yr BP to -55 cal yr BP;
Time Period-764 to 2005
Spatial Bounding Box Coordinates
N: 67.5
S: 67.5
E: 70
W: 70
Spatial Coverage Map
General Documentation
Associated Resources
  • Reassessing the evidence for tree-growth and inferred temperature change during the Common Era in Yamalia, northwest Siberia
    • Associated Reference published 2013
      Keith R. Briffa, Thomas M. Melvin, Timothy J. Osborn, Rashit M. Hantemirov, Alexander V. Kirdyanov, Valeriy S. Mazepa, Stepan G. Shiyatov, Jan Esper, 2013: Reassessing the evidence for tree-growth and inferred temperature change during the Common Era in Yamalia, northwest Siberia. Quaternary Science Reviews, 72, 83-107, 10.1016/j.quascirev.2013.04.008
Publication Dates
  • publication: 2013-05-21
Data Presentation Form Digital table - digital representation of facts or figures systematically displayed, especially in columns
Dataset Progress StatusComplete - production of the data has been completed
Data Update Frequency Data update frequency not available
Supplemental Information
STUDY NOTES: Purpose of Collection: # Climatology - temperature analyses NOAA Template Raw Measurements file added 2019-04-08.
ABSTRACT SUPPLIED BY ORIGINATOR: The development of research into the history of tree growth and inferred summer temperature changes in Yamalia spanning the last 2000 years is reviewed. One focus is the evolving production of tree-ring width (TRW) and tree-ring maximum-latewood density (MXD) larch (Larix sibirica) chronologies, incorporating different applications of Regional Curve Standardisation (RCS). Another focus is the comparison of independent data representing past tree growth in adjacent Yamalia areas: Yamal and Polar Urals, and the examination of the evidence for common growth behaviour at different timescales. The sample data we use are far more numerous and cover a longer time-span at Yamal compared to the Polar Urals, but Yamal has only TRW, while there are both TRW and MXD for the Polar Urals. We use more data (sub-fossil and from living trees) than in previous dendroclimatic studies in this region. We develop a new TRW chronology for Yamal, more than 2000 years long and running up to 2005. For the Polar Urals we develop new TRW and MXD chronologies that show good agreement at short (<15 years) and medium (15-100 years) timescales demonstrating the validity of attempts to reconcile the evidence of longer-timescale information that they provide. We use a "conservative" application of the RCS approach (two-curve signal-free RCS), guarding against the possibility of "modern sample bias": a possible inflation of recent chronology values arising out of inadvertent selection of mostly relatively fast-growing trees in recent centuries. We also transform tree indices to have a normal distribution to remove the positive chronology skew often apparent in RCS TRW chronologies. This also reduces the apparent magnitude of 20th century tree-growth levels. There is generally good agreement between all chronologies as regards the major features of the decadal to centennial variability. Low tree-growth periods for which the inferred summer temperatures are approximately 2.5C below the 1961-90 reference are apparent in the 15-year smoothed reconstructions, centred around 1005, 1300, 1455, 1530, particularly the 1810s where the inferred cooling reaches -4C or even -6C for individual years, and the 1880s. These are superimposed on generally cool pre-20th century conditions: the long-term means of the pre-1900 reconstructed temperature anomalies range from -0.6 to -0.9C in our alternative reconstructions. There are numerous periods of one or two decades with relatively high growth (and inferred summer temperatures close to the 1961-1990 level) but at longer timescales only the 40-year period centred at 250 CE appears comparable with 20th century warmth. Although the central temperature estimate for this period is below that for the recent period, when we take into account the uncertainties we cannot be highly confident that recent warmth has exceeded the temperature of this earlier warm period. While there are clear warm decades either side of 1000 CE, neither TRW nor MXD data support the conclusion that temperatures were exceptionally high during medieval times. One previous version of the Polar Urals TRW chronology is shown here to be in error due to an injudicious application of RCS to non-homogeneous sample data, partly derived from root-collar samples that produce spuriously high chronology values in the 11th and 15th centuries. This biased chronology has been used in a number of recent studies aimed at reconstructing wider scale temperature histories. All of the chronologies we have produced here clearly show a generally high level of growth throughout their most recent 80 years. Allowing for chronology and reconstruction uncertainty, the mean of the last 100 years of the reconstruction is likely warmer than any century in the last 2000 years in this region.
PurposeTree ring data from the International Tree Ring Data Bank and World Data Center for Paleoclimatology archives. Most data sets include raw treering measurements (most are annual ring width, with some collections of earlywood or latewood width or wood density), plus chronologies (standardized growth indices for a site compiled from multiple treering samples). Reconstructions of climate variables are included with some of these data sets. Each data type is stored in a separate data file; the data type is coded into the file name. For details please see: http://www.ncei.noaa.gov/products/paleoclimatology/tree-ring
Dataset Citation
  • Cite as: Hantemirov, R.M.; Shiyatov, S.G.; Surkov, A.; Gorlanova, L. (2013-05-21): NOAA/WDS Paleoclimatology - Hantemirov - Yamal - LASI - ITRDB RUSS223. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/ekha-nr57. Accessed [date].
  • Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.
Cited Authors
  • Hantemirov, R.M.
  • Shiyatov, S.G.
  • Surkov, A.
  • Gorlanova, L.
Originators
  • Hantemirov, R.M.
  • Shiyatov, S.G.
  • Surkov, A.
  • Gorlanova, L.
Publishers
  • NOAA National Centers for Environmental Information
Theme keywordsGlobal Change Master Directory (GCMD) Science Keywords
  • Earth Science > Climate Indicators > Paleoclimate Indicators > Biological Records > Tree Rings
  • Earth Science > Paleoclimate > Land Records > Tree Rings
Global Change Master Directory (GCMD) Science Keywords
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  • earth science > paleoclimate > tree ring
  • earth science > paleoclimate > tree ring
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  • earth science > paleoclimate > tree ring
  • earth science > paleoclimate > tree-ring > width
  • LASI
  • Larix sibirica Ledeb. = Larix russica (Endl.) Sabine ex Trautv.
  • Siberian larch
Paleoenvironmental Standard Terms (PaST) Thesaurus
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  • What: age; Material: null
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Data Center keywordsGlobal Change Master Directory (GCMD) Data Center Keywords
  • DOC/NOAA/NESDIS/NCEI > National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
Place keywords
  • Continent > Europe > Eastern Europe > Russia > Yamal > LATITUDE 67.5 > LONGITUDE 70
Use Constraints
  • Cite as: Hantemirov, R.M.; Shiyatov, S.G.; Surkov, A.; Gorlanova, L. (2013-05-21): NOAA/WDS Paleoclimatology - Hantemirov - Yamal - LASI - ITRDB RUSS223. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/ekha-nr57. Accessed [date].
  • Use liability: NOAA and NCEI cannot provide any warranty as to the accuracy, reliability, or completeness of furnished data. Users assume responsibility to determine the usability of these data. The user is responsible for the results of any application of this data for other than its intended purpose.
  • Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.
Access Constraints
  • Distribution liability: NOAA and NCEI make no warranty, expressed or implied, regarding these data, nor does the fact of distribution constitute such a warranty. NOAA and NCEI cannot assume liability for any damages caused by any errors or omissions in these data. If appropriate, NCEI can only certify that the data it distributes are an authentic copy of the records that were accepted for inclusion in the NCEI archives.
  • None
Fees
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Last Modified: 2024-04-16
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