# Kose - Bolu - PISY - ITRDB TURK049 #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite original publication, online resource and date accessed when using these data, # If there is no publication information, please cite investigator, title, online resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/22354 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/europe/turk049a-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk049a.crn # Description: Chronology - Tucson Decadal File # # Archive: Tree Ring # # Dataset_DOI: # # Parameter_Keywords: ring width #------------------- # Contribution_Date # Date: 2016-12-26 #------------------- # File_Last_Modified_Date # Date: 2018-12-19 #------------------- # Title # Study_Name: Kose - Bolu - PISY - ITRDB TURK049 #------------------- # Investigators: Kose, N.; Guner, H.T. #------------------- # Description_Notes_and_Keywords # Description: NOAA Template Chronology file added 2018-12-19. #------------------- # Publication # Authors: Nesibe Kose, H. Tuncay Guner, Grant L. Harley, and Joel Guiot # Journal_Name: Climate of the Past # Published_Title: Spring temperature variability over Turkey since 1800?CE reconstructed from a broad network of tree-ring data # Published_Date_or_Year: 2017 # Volume: 13 # Pages: 1-15 # Report_Number: # DOI: 10.5194/cp-13-1-2017 # Full_Citation: # Abstract: The meteorological observational period in Turkey, which starts ca. 1930?CE, is too short for understanding long-term climatic variability. Tree rings have been used intensively as proxy records to understand summer precipitation history of the region, primarily because they have a dominant precipitation signal. Yet, the historical context of temperature variability is unclear. Here, we used higher-order principle components of a network of 23 tree-ring chronologies to provide a high-resolution spring (March-April) temperature reconstruction over Turkey during the period 1800-2002. The reconstruction model accounted for 67?% (Adj. R2 = ?0.64, p? var components: what,material,error,units,season,archive,detail,method, C or N for Char or Numeric data,additional information ## age_CE age,,,year Common Era,,tree ring,,,N, ## trsgi tree ring standardized growth index,,,,,tree ring,composited,ARSTAN,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1752 1061 2 1753 1536 1 1754 1666 2 1755 1920 2 1756 1836 2 1757 918 2 1758 1430 2 1759 1035 2 1760 984 2 1761 757 2 1762 788 2 1763 787 2 1764 984 2 1765 880 2 1766 1127 2 1767 923 2 1768 812 2 1769 572 2 1770 538 2 1771 789 2 1772 777 2 1773 820 2 1774 774 2 1775 797 2 1776 558 2 1777 422 2 1778 867 2 1779 872 2 1780 940 2 1781 728 2 1782 574 2 1783 730 3 1784 1077 3 1785 1277 4 1786 1417 6 1787 1177 6 1788 1039 7 1789 1033 8 1790 935 8 1791 1036 9 1792 1251 10 1793 1215 10 1794 1116 10 1795 878 10 1796 995 10 1797 957 10 1798 1219 10 1799 1209 10 1800 1294 10 1801 1060 11 1802 989 11 1803 918 12 1804 890 12 1805 923 12 1806 791 12 1807 979 12 1808 997 12 1809 963 12 1810 1069 12 1811 1047 12 1812 958 12 1813 941 12 1814 1069 12 1815 827 14 1816 1106 14 1817 1118 14 1818 956 14 1819 821 14 1820 771 14 1821 985 14 1822 880 14 1823 945 14 1824 835 14 1825 858 14 1826 944 16 1827 942 16 1828 829 16 1829 1215 16 1830 819 16 1831 947 17 1832 791 17 1833 866 18 1834 766 18 1835 1086 18 1836 1052 18 1837 1190 18 1838 1161 18 1839 1137 19 1840 747 19 1841 900 19 1842 832 20 1843 999 20 1844 894 20 1845 821 20 1846 1036 20 1847 905 20 1848 1034 20 1849 1065 20 1850 1041 20 1851 909 20 1852 938 20 1853 1058 20 1854 930 20 1855 1061 20 1856 971 20 1857 985 20 1858 1036 20 1859 1038 20 1860 910 20 1861 910 20 1862 873 20 1863 749 20 1864 787 20 1865 960 20 1866 996 20 1867 981 20 1868 892 20 1869 1038 20 1870 929 20 1871 1082 20 1872 1151 20 1873 932 20 1874 859 20 1875 850 20 1876 932 20 1877 1175 20 1878 1014 20 1879 1040 20 1880 962 20 1881 1090 20 1882 935 20 1883 921 20 1884 1027 20 1885 1170 20 1886 1051 20 1887 778 20 1888 1001 20 1889 1278 20 1890 983 20 1891 1048 20 1892 942 20 1893 696 20 1894 716 20 1895 903 20 1896 882 20 1897 1236 20 1898 1324 20 1899 1067 20 1900 1260 20 1901 1630 20 1902 1523 20 1903 1408 20 1904 964 20 1905 798 20 1906 963 20 1907 814 20 1908 781 20 1909 728 20 1910 960 20 1911 851 20 1912 1014 20 1913 982 20 1914 1056 20 1915 1452 20 1916 1312 20 1917 1435 20 1918 1222 20 1919 1564 20 1920 1197 20 1921 839 20 1922 943 20 1923 904 20 1924 875 20 1925 941 20 1926 873 20 1927 753 20 1928 659 20 1929 761 20 1930 861 20 1931 1033 20 1932 878 20 1933 1099 20 1934 901 20 1935 833 20 1936 1133 20 1937 934 20 1938 843 20 1939 1073 20 1940 1308 20 1941 1150 20 1942 944 20 1943 875 20 1944 944 20 1945 723 20 1946 656 20 1947 607 20 1948 700 20 1949 582 20 1950 769 20 1951 910 20 1952 820 20 1953 882 20 1954 1027 20 1955 1041 20 1956 961 20 1957 816 20 1958 1013 20 1959 1149 20 1960 1114 20 1961 1046 20 1962 1182 20 1963 1152 20 1964 1073 20 1965 1147 20 1966 1033 20 1967 865 20 1968 751 20 1969 847 20 1970 1062 20 1971 1193 20 1972 1105 20 1973 1199 20 1974 1154 20 1975 1199 20 1976 1094 20 1977 922 20 1978 1205 20 1979 1405 20 1980 1326 20 1981 1298 20 1982 1221 20 1983 1231 20 1984 1077 20 1985 1147 20 1986 1143 20 1987 976 20 1988 1008 20 1989 771 20 1990 703 20 1991 915 20 1992 967 20 1993 913 20 1994 770 20 1995 658 19 1996 861 18 1997 946 18 1998 882 18 1999 879 18 2000 958 18 2001 1222 17 2002 1151 14 2003 655 12 2004 1103 12 2005 1111 12 2006 845 12 2007 768 12 2008 1235 9 2009 1236 2