NOAA/WDS Paleoclimatology - Hughes - Kologrivsky Forest Nature Reserve - PISY - ITRDB RUSS276
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title: NOAA/WDS Paleoclimatology - Hughes - Kologrivsky Forest Nature Reserve - PISY - ITRDB RUSS276
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date: 2019-06-26
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Anchor: DOI doi:10.25921/psyx-vz31
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abstract: 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 121 to -59 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
purpose: Tree 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
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keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Biological Records > Tree Rings
keyword: Earth Science > Paleoclimate > Land Records > Tree Rings
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keyword: earth science > paleoclimate > tree ring
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keyword: earth science > paleoclimate > tree-ring > width
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keyword: PISY
keyword: Pinus sylvestris L.
keyword: Scots pine
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keyword: Continent > Europe > Eastern Europe > Russia > Kologrivsky Forest Nature Reserve > LATITUDE 58.896 > LONGITUDE 44.079
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otherConstraints: Cite as: Hughes, M.K.; Olchev, A.; Bunn, A.G.; Berner, L.T.; Losleben, M.V.; Novenko, E. (2019-06-26): NOAA/WDS Paleoclimatology - Hughes - Kologrivsky Forest Nature Reserve - PISY - ITRDB RUSS276. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/psyx-vz31. Accessed [date].
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otherConstraints: 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.
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otherConstraints: 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.
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otherConstraints: 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.
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title: Different Climate Responses of Spruce and Pine Growth in Northern European Russia
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date: 2019
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individualName: Malcolm K. Hughes, Alexander Olchev, Andrew G. Bunn, Logan T. Berner, Mark Losleben, Elena Novenko
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description: Malcolm K. Hughes, Alexander Olchev, Andrew G. Bunn, Logan T. Berner, Mark Losleben, Elena Novenko, 2019: Different Climate Responses of Spruce and Pine Growth in Northern European Russia. Dendrochronologia, 56, , 10.1016/j.dendro.2019.05.005
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language: eng; USA
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description: Date Range: 1829 CE to 2009 CE; Date Range: 121 cal yr BP to -59 cal yr BP;
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supplementalInformation: STUDY NOTES: NOAA Template Raw Measurements file added 2020-01-15. ABSTRACT SUPPLIED BY ORIGINATOR: We report new data on tree-ring growth in northern European Russia, a region with a hitherto relatively sparse tree-ring network. We explore its associations with climate variability. Areas, sampling locations and trees were selected for representativeness rather than climate sensitivity. Using tree rings from 651 conifers from six widely dispersed areas we show strong intercorrelation between trees within each major conifer species within and between areas. Regional composite tree-ring series for spruce and pine contain a major fraction of decadal and multidecadal variability. The most likely driver of this common variability is interannual to multidecadal climate variability. Gridded monthly instrumental climate data for the period 1902-2008, particularly mean temperature and total precipitation, were tested as predictors of each local species-specific tree-ring site chronology. The most consistent pattern emerged for spruce at all but the southernmost area. Cool and moist summers the year before growth were consistent drivers of spruce ring growth throughout the period, with no change in recent decades. Self-calibrating Palmer Drought Severity Index for prior summer was also a strong and consistent driver of spruce ring growth. For pine, there was a weaker but similarly stable association between larger rings and warm, moist conditions, in this case in the current summer. These associations were also identified at multidecadal time scales, particularly for spruce. On the other hand, the specific role of moisture variability in determining interannual to multidecadal variability in tree growth in this high latitude region raises questions about the relative vulnerability of spruce and pine there under global warming.
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