noaa-tree-16696 Neuwirth - Nordrhein-Westfalen/Eifel dre08- FASY - ITRDB GERM180 Neuwirth, B. Neuwirth - Nordrhein-Westfalen/Eifel dre08- FASY - ITRDB GERM180 2014-02-27 NCDC-Paleoclimatology ONLINE Files 10.25921/d27d-v185 https://www.ncdc.noaa.gov/paleo/study/16696 Investigator B. Neuwirth earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0810m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0807m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0803m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0801m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0814m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0811m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0802m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0809m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0806m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0805m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0812m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0808m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring age,null,null,year Common Era,null,tree ring,null,null,N,null earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree ring total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: dre0804m; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 earth science paleoclimate tree-ring width geoscientificInformation FASY Fagus sylvatica L. European beech common beech 1858 AD 2005 AD 92 cal yr BP -55 cal yr BP Complete 50.6667 50.6667 6.2667 6.2667 440 440 Continent Europe Western Europe Germany Nordrhein-Westfalen/Eifel dre08>LATITUDE 50.6667>LONGITUDE 6.2667 None 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. English DOC/NOAA/NESDIS/NCEI National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce https://www.ncdc.noaa.gov/data-access/paleoclimatology-data DATA Center Contact Bruce Bauer bruce.a.bauer@noaa.gov paleo@noaa.gov 303-497-6280 303-497-6513

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Boulder CO 80305-3328 USA online ASCII Dagmar A. Friedrichs, Burkhard Neuwirth, Matthias Winiger, Jörg Löffler 2009 Dendrochronologia 27 1 21-30 10.1016/j.dendro.2008.02.001 http://www.sciencedirect.com/science/article/pii/S1125786508000568 Dagmar A. Friedrichs, Valerie Trouet, Ulf Büntgen, David C. Frank, Jan Esper, Burkhard Neuwirth, Jörg Löffler 2009 Trees - Structure and Function 23 4 729-739 10.1007/s00468-009-0315-2 http://link.springer.com/article/10.1007/s00468-009-0315-2 Johannes Andreas Schultz and Burkhard Neuwirth 2012 Agricultural and Forest Meteorology 164 149-160 10.1016/j.agrformet.2012.05.007 http://www.sciencedirect.com/science/article/pii/S0168192312001761 Stefanie Fischer and Burkhard Neuwirth 2013 ISRN Forestry 2013 201360 10.1155/2013/201360 http://www.hindawi.com/journals/isrn.forestry/2013/201360/

This paper introduces a new procedure to investigate the influence of weather types on spatio-temporal tree-ring growth patterns. Within the framework of the procedure a new proxy-based climate index termed as the atmospheric circulation tree-ring index (ACTI) is calculated that combines weather-type classification data with climate proxies. The new approach is tested using a Central European multi-species tree-ring width network consisting of 115 sites. The procedure used to calculate the ACTI time series includes: 1. Monte Carlo simulations, 2. multiple testing correction, and 3. selection and grouping algorithms. The tree-ring width series are grouped according to their weather-type responses, and the ACTI time series were computed for each group. The new procedure explains the climate signal preserved in tree-ring chronologies more comprehensively because the complex interaction between the different climate elements is taken into account by using weather-type classification data. Strong correlations between the ACTI and tree-ring width series (r = 0.69) and between the ACTI time series and climate gridded datasets (r > 0.6) were observed. Further a correlation between ACTI and northern hemisphere mean temperatures (r = 0.5) were found. These results indicate that the ACTI enables the investigation of weather-type growth relationships. STUDY NOTES: Purpose of Collection: # climate/growth relationship NOAA Template Raw Measurements file added 2019-02-05.

GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/germ180.txt GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/germ180-noaa.rwl Raw Measurements - NOAA Template File; germ180-noaa.rwl GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/germ180.rwl USA/NOAA DIF Version 9.8.4 2019-02-08 2019-02-08