# Wilson - Salzstadel 1 Straubing Historical Timbers - ABAL - ITRDB GERM098 #---------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #---------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/10703 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-tree-10703.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Tree Ring # # Dataset_DOI: # # Science_Keywords: drought #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/measurements/europe/germ098-rwl-noaa.txt # Data_Download_Description: Raw Measurements - NOAA Template File; germ098-rwl-noaa.txt # # Related_Online_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/measurements/europe/germ098.rwl # Related_Online_Description: RWL File; Raw Measurements - Tucson Decadal File # # Supplemental_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/germ098.txt # Supplemental_Description: Text File; Correlation Stats # #-------------------- # Contribution_Date # Date: 2010-06-23 #-------------------- # File_Last_Modified_Date # Date: 2010-06-23 #-------------------- # Title # Study_Name: Wilson - Salzstadel 1 Straubing Historical Timbers - ABAL - ITRDB GERM098 #-------------------- # Investigators # Investigators: Wilson, R.J.S.(https://orcid.org/0000-0003-4486-8904) #-------------------- # Description_Notes_and_Keywords # Description: Purpose of Collection: # # Hydroclimatic reconstructions # # # # # # References: # # Wilson, R.J.S. and W. Elling. 2004. # # Temporal instabilities of tree-growth/climate response # # in the Lower Bavarian Forest Region: Implications for # # dendroclimatic reconstruction. # # Trees: Structure and Function, 18 (1): 19-28. # # # # Wilson, R.J.S., J. Esper, and B.H. Luckman. 2004. # # Utilising Historical Tree-Ring Data for Dendroclimatology: # # A Case study from the Bavarian Forest, Germany. # # Dendrochronologia. 21 (2): 53-68. # # # # Wilson, R.J.S., B.H. Luckman, and J. Esper. 2005. # # A 500-Year Dendroclimatic Reconstruction of Spring/Summer # # Precipitation from the Lower Bavarian Forest Region, Germany. # # International Journal of Climatology, 25: 611-630. # # # # # # Notes: # # Bavarian Forest Region Historical Timbers # # # # NOAA Template Raw Measurements file added 2019-02-05. #-------------------- # Publication # Authors: # Journal_Name: International Journal of Climatology # Published_Title: A 500-Year Dendroclimatic Reconstruction of Spring/Summer Precipitation from the Lower Bavarian Forest Region, Germany # Published_Date_or_Year: 2005 # Volume: # Pages: # Issue: # Report_Number: # DOI: 10.1002/joc.1150 # Full_Citation: Wilson, R.J.S., B.H. Luckman, and J. Esper. 2005. A 500-Year Dendroclimatic Reconstruction of Spring/Summer Precipitation from the Lower Bavarian Forest Region, Germany. International Journal of Climatology, 25: 611-630. # Abstract: This paper presents a 500 year March-August precipitation reconstruction for the Bavarian Forest region of southeast # Germany based on a composite, well-replicated data set of 676 living and historical tree-ring width series from Norway # spruce. Two versions of the chronology are developed. The cubic smoothing spline (SPL) chronology, standardized # with a fixed 80 year spline function, retains decadal and higher frequency variation. The regional curve standardization # (RCS) chronology uses regional curve standardization to retain additional lower frequency variation from the same # data. Calibration (1879-1978) of these chronologies with March-August precipitation indicates they explain 40% (SPL) # and 34% (RCS) of the variability in the instrumental precipitation record. The SPL reconstruction models the high frequency # variation better, whereas the RCS reconstruction tracks the low-frequency trends more robustly. It suggests # that spring-summer precipitation was above the long-term average for the periods 1730-1810 and 1870-2000, about # average between 1560 and 1610 and that significantly drier periods occurred during 1510-60, 1610-35, 1660-1730 and # 1830-70. The low-frequency trends of the RCS reconstruction during the 19th century were verified by comparison with a # regional precipitation series derived from 14 long precipitation records from central Europe. Better verification results were # obtained using the original (non-homogenized) records over this interval. These results suggest that some low-frequency # variability may have been removed during correction of these early records. Periods of synchronous decadal variability # were observed between the SPL series and independent dendroclimatic reconstructions from central Europe. The RCS # reconstruction is the first dendroclimatic precipitation reconstruction in Europe to capture low-frequency information. # These long-term trends, however, are difficult to verify owing to the paucity of other proxy precipitation records in # central Europe that portray low-frequency information. Further verification and testing of the RCS reconstruction will # require the development of additional reconstructions from tree-rings (or other proxy data series) that similarly target # low-frequency variability. #-------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #-------------------- # Site_Information # Site_Name: Salzstadel 1 Straubing Historical Timbers # Location: Bavaria # Northernmost_Latitude: 48.8833 # Southernmost_Latitude: 48.8833 # Easternmost_Longitude: 12.5667 # Westernmost_Longitude: 12.5667 # Elevation_m: None #-------------------- # Data_Collection # Collection_Name: GERM098 # First_Year: 1683 # Last_Year: 1839 # Time_Unit: CE # Core_Length_m: # Parameter_Keywords: ring width # Notes: #-------------------- # Species # Species_Name: Abies alba Mill. # Common_Name: silver fir # Tree_Species_Code: ABAL #-------------------- # Variables # # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Data variables follow that are preceded by '##' in columns one and two. # Variables format: shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # ## age_CE age,,,year Common Era,,tree ring,,,N, ## SSS19A_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS19A; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS19B_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS19B; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS20A_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS20A; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS20B_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS20B; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS24A_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS24A; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS24B_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS24B; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## SSS24C_raw total ring width,,,millimeter,,tree ring,,,N,Tree ID: SSS24C; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 #--------------------- # Data: # Missing_Values: NA age_CE SSS19A_raw SSS19B_raw SSS20A_raw SSS20B_raw SSS24A_raw SSS24B_raw SSS24C_raw 1683 NA NA NA NA 0.596 0.65 0.776 1684 NA NA NA NA 0.919 1.048 0.983 1685 NA NA NA NA 0.9 0.761 0.924 1686 NA NA NA NA 0.738 0.956 0.706 1687 NA NA NA NA 1.248 1.226 1.027 1688 NA NA NA NA 1.444 1.543 1.566 1689 NA NA NA NA 1.099 1.19 1.335 1690 NA NA NA NA 1.194 1.197 1.319 1691 NA NA NA NA 1.128 1.131 1.375 1692 NA NA NA NA 0.942 0.835 0.818 1693 NA NA NA NA 1.333 1.118 1.261 1694 NA NA NA NA 1.169 0.942 1.041 1695 NA NA NA NA 1.076 0.793 1.002 1696 NA NA NA NA 1.115 0.846 1.017 1697 NA NA NA NA 0.871 0.744 0.708 1698 NA NA NA NA 0.952 0.868 0.844 1699 NA NA NA NA 0.896 0.723 0.98 1700 NA NA NA NA 0.655 0.695 0.885 1701 NA NA NA NA 0.856 0.88 1.154 1702 NA NA NA NA 0.901 1.021 0.915 1703 NA NA NA NA 0.743 0.712 0.829 1704 NA NA NA NA 0.813 0.634 0.811 1705 NA NA NA NA 0.94 0.776 0.785 1706 NA NA NA NA 0.682 0.552 0.638 1707 NA NA NA NA 0.641 0.479 0.678 1708 NA NA NA NA 0.738 0.678 0.717 1709 NA NA NA NA 0.937 0.808 1.014 1710 NA NA NA NA 0.98 0.83 1.162 1711 NA NA NA NA 0.937 0.842 0.833 1712 NA NA NA NA 1.234 0.897 1.107 1713 NA NA NA NA 1.462 1.033 1.148 1714 NA NA NA NA 1.424 0.983 1.115 1715 NA NA NA NA 1.111 0.715 0.978 1716 NA NA NA NA 0.985 0.659 0.86 1717 NA NA NA NA 0.954 0.82 0.849 1718 NA NA NA NA 0.942 0.82 0.558 1719 NA NA NA NA 0.798 0.823 0.57 1720 NA NA NA NA 0.734 0.877 0.683 1721 NA NA NA NA 0.332 0.375 0.39 1722 NA NA NA NA 0.808 0.917 1.048 1723 NA NA NA NA 1.288 1.215 1.195 1724 NA NA NA NA 1.911 1.332 1.314 1725 NA NA NA NA 2.069 1.57 1.153 1726 NA NA NA NA 1.794 1.381 1.191 1727 NA NA NA NA 2.412 1.799 1.314 1728 NA NA NA NA 1.712 1.143 1.24 1729 NA NA NA NA 1.926 1.584 1.346 1730 NA NA NA NA 2.575 2.205 2.17 1731 NA NA NA NA 2.242 1.841 1.796 1732 NA NA NA NA 1.579 2.059 1.439 1733 NA NA NA NA 1.087 2.062 1.526 1734 NA NA NA NA 1.794 1.94 1.608 1735 NA NA NA NA 1.718 1.924 1.558 1736 NA NA NA NA 1.485 2.01 1.682 1737 NA NA NA NA 1.936 2.238 2.06 1738 NA NA NA NA 1.896 2.029 2.073 1739 NA NA NA NA 1.512 2.018 1.892 1740 NA NA NA NA 1.507 1.609 2.125 1741 NA NA NA NA 1.915 1.983 2.703 1742 NA NA NA NA 2.031 2.192 2.381 1743 NA NA NA NA 2.072 2.248 2.835 1744 NA NA NA NA 2.436 2.796 3.366 1745 NA NA NA NA 2.241 3.317 3.71 1746 NA NA NA NA 1.572 2.407 2.513 1747 NA NA NA NA 1.489 2.342 3.055 1748 NA NA NA NA 1.827 2.811 3.47 1749 NA NA NA NA 2.466 3.558 3.634 1750 NA NA NA NA 1.668 2.953 3.024 1751 NA NA NA NA 1.359 2.785 2.798 1752 1.377 1.371 NA NA 1.79 2.937 3.131 1753 2.078 2.282 NA NA 1.312 2.492 2.509 1754 3.003 2.918 NA NA 1.517 2.654 2.536 1755 2.904 2.716 NA NA 1.476 2.885 2.689 1756 3.146 2.969 NA NA 1.635 3.398 2.912 1757 3.819 3.097 NA NA 1.364 3.101 2.412 1758 3.429 2.954 NA NA 1.247 1.915 1.589 1759 3.596 3.331 NA NA 1.666 3.304 2.185 1760 3.323 2.638 NA NA 1.478 2.187 1.474 1761 3.751 3.245 NA NA 1.642 2.673 1.674 1762 2.333 2.033 NA NA 1.162 1.464 1.056 1763 2.879 2.414 NA NA 1.71 2.337 1.9 1764 2.334 1.89 NA NA 1.506 1.844 1.603 1765 2.943 2.71 NA NA 1.947 2 2.028 1766 3.063 2.935 NA NA 1.798 1.854 1.45 1767 3.419 3.41 NA NA 1.147 1.305 1.126 1768 2.524 2.908 NA NA 1.264 1.031 0.828 1769 3.072 3.133 3.356 3.185 1.228 1.184 1.417 1770 4.257 4.735 3.493 3.496 1.347 1.312 1.718 1771 3.401 4.305 3.399 3.594 1.043 1.225 NA 1772 4.521 5.515 4.163 3.975 1.375 1.477 NA 1773 3.429 3.531 3.347 3.087 0.706 0.845 NA 1774 4.081 3.898 3.266 3.407 0.776 0.973 NA 1775 3.717 3.813 3.153 3.396 0.706 0.751 NA 1776 3.845 4.1 2.661 2.744 0.589 0.584 NA 1777 3.881 4.811 3.029 2.832 0.501 0.539 NA 1778 4.027 4.812 2.787 2.697 0.335 0.372 NA 1779 4.378 4.474 2.602 2.695 0.294 0.336 NA 1780 4.32 4.395 2.518 3.011 0.308 0.326 NA 1781 4.453 4.193 2.496 3.191 0.276 0.291 NA 1782 4.085 3.716 3.301 3.226 0.241 0.26 NA 1783 4.769 4.558 3.713 3.109 0.296 0.322 NA 1784 3.413 2.821 2.977 2.539 0.189 0.249 NA 1785 3.508 3.216 3.635 2.826 0.233 0.314 NA 1786 3.664 3.487 3.551 3.191 0.231 0.301 NA 1787 4.173 3.947 4.238 3.289 0.236 0.352 NA 1788 3.801 4.692 3.733 2.693 0.232 0.385 NA 1789 1.384 3.345 2.9 2.241 0.137 0.259 NA 1790 1.349 3.791 2.575 2.069 0.057 0.169 NA 1791 1.362 4.185 2.923 2.632 0.133 0.206 NA 1792 1.102 2.996 2.974 2.304 NA NA NA 1793 1.174 2.669 3.371 2.509 NA NA NA 1794 0.933 2.037 2.645 2.136 NA NA NA 1795 1.051 2.166 2.677 2.478 NA NA NA 1796 1.579 3.184 2.755 2.675 NA NA NA 1797 0.739 1.261 1.83 1.539 NA NA NA 1798 1.026 1.593 2.367 1.85 NA NA NA 1799 1.348 1.687 2.505 2.261 NA NA NA 1800 0.893 1.242 1.757 1.573 NA NA NA 1801 1.169 1.939 2.108 2.194 NA NA NA 1802 1.928 2.059 3.085 2.509 NA NA NA 1803 1.496 1.679 1.613 1.275 NA NA NA 1804 1.635 1.842 2.255 1.923 NA NA NA 1805 2.074 2.28 2.145 1.764 NA NA NA 1806 1.586 1.646 1.987 1.884 NA NA NA 1807 1.716 1.699 2.005 1.6 NA NA NA 1808 1.64 1.363 2.013 1.676 NA NA NA 1809 2.343 2.011 2.403 2.525 NA NA NA 1810 2.69 2.26 2.712 2.783 NA NA NA 1811 2.489 1.78 2.086 2.168 NA NA NA 1812 2.03 1.349 2.291 2.704 NA NA NA 1813 2.915 1.999 2.945 2.692 NA NA NA 1814 3.004 2.153 3.534 3.655 NA NA NA 1815 2.834 2.185 3.26 3.193 NA NA NA 1816 NA 2.226 2.911 2.59 NA NA NA 1817 NA 2.025 2.589 2.636 NA NA NA 1818 NA NA 2.207 3.081 NA NA NA 1819 NA NA 2.438 3.265 NA NA NA 1820 NA NA 1.797 2.082 NA NA NA 1821 NA NA 1.682 1.768 NA NA NA 1822 NA NA 2.088 2.449 NA NA NA 1823 NA NA 1.981 2.397 NA NA NA 1824 NA NA 1.816 2.644 NA NA NA 1825 NA NA 1.836 2.869 NA NA NA 1826 NA NA 1.844 2.769 NA NA NA 1827 NA NA 1.742 2.333 NA NA NA 1828 NA NA 2.459 2.959 NA NA NA 1829 NA NA 2.503 2.898 NA NA NA 1830 NA NA 1.396 2.385 NA NA NA 1831 NA NA 1.936 2.859 NA NA NA 1832 NA NA NA 2.894 NA NA NA 1833 NA NA NA 1.606 NA NA NA 1834 NA NA NA 2.298 NA NA NA 1835 NA NA NA 1.841 NA NA NA 1836 NA NA NA 2.275 NA NA NA 1837 NA NA NA 1.854 NA NA NA 1838 NA NA NA 2.179 NA NA NA 1839 NA NA NA 2.447 NA NA NA