# Kose - Bilecik - PINI - ITRDB TURK050 #----------------------------------------------------------------------- # 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/22355 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/europe/turk050a-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk050a.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 - Bilecik - PINI - ITRDB TURK050 #------------------- # 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 1720 1174 1 1721 1391 1 1722 1470 1 1723 1400 1 1724 1287 1 1725 1324 1 1726 890 1 1727 1167 1 1728 937 1 1729 661 1 1730 1038 1 1731 1360 1 1732 1576 1 1733 652 1 1734 1005 1 1735 1412 1 1736 1581 1 1737 1124 1 1738 827 1 1739 1181 1 1740 1391 2 1741 1307 2 1742 976 2 1743 1230 2 1744 1021 2 1745 605 2 1746 866 2 1747 863 2 1748 811 2 1749 1090 2 1750 1025 2 1751 845 2 1752 950 2 1753 1342 2 1754 909 2 1755 1222 2 1756 1137 2 1757 1065 2 1758 1000 2 1759 1139 2 1760 1234 2 1761 769 2 1762 1192 2 1763 744 2 1764 813 2 1765 1346 2 1766 1193 2 1767 863 2 1768 763 2 1769 849 2 1770 972 2 1771 1162 2 1772 868 3 1773 1166 5 1774 1218 5 1775 934 6 1776 747 6 1777 797 6 1778 1052 7 1779 987 7 1780 1093 7 1781 1000 8 1782 751 9 1783 930 9 1784 1119 9 1785 894 11 1786 1044 11 1787 1012 11 1788 1105 12 1789 891 12 1790 946 12 1791 1055 12 1792 814 12 1793 996 12 1794 820 12 1795 899 12 1796 870 12 1797 696 12 1798 825 12 1799 997 13 1800 975 14 1801 903 14 1802 892 14 1803 1023 14 1804 1106 14 1805 1101 14 1806 800 14 1807 926 14 1808 960 15 1809 1012 15 1810 1083 15 1811 1350 15 1812 1034 15 1813 624 16 1814 966 16 1815 1111 16 1816 1243 16 1817 1167 16 1818 1124 16 1819 951 16 1820 841 17 1821 1125 17 1822 927 17 1823 867 17 1824 893 17 1825 936 17 1826 1088 17 1827 1113 18 1828 881 19 1829 992 19 1830 695 18 1831 717 20 1832 694 20 1833 842 20 1834 598 20 1835 954 20 1836 1079 21 1837 1201 21 1838 1177 21 1839 1176 21 1840 499 21 1841 743 21 1842 926 21 1843 1072 21 1844 1203 21 1845 834 21 1846 1300 21 1847 1127 21 1848 1115 21 1849 935 21 1850 923 21 1851 1036 21 1852 688 21 1853 882 21 1854 1152 21 1855 1476 21 1856 1153 21 1857 1246 22 1858 1033 22 1859 1302 22 1860 1143 22 1861 703 22 1862 628 22 1863 731 22 1864 927 22 1865 1288 22 1866 1359 22 1867 953 22 1868 646 23 1869 669 23 1870 745 23 1871 1002 23 1872 1462 23 1873 1240 23 1874 1045 23 1875 877 23 1876 1065 23 1877 1045 23 1878 678 23 1879 694 23 1880 977 23 1881 1265 23 1882 1050 23 1883 974 23 1884 937 23 1885 1396 23 1886 964 23 1887 675 23 1888 977 23 1889 1100 23 1890 897 23 1891 1217 23 1892 994 23 1893 579 23 1894 670 23 1895 915 23 1896 977 23 1897 1154 23 1898 972 23 1899 657 23 1900 966 23 1901 1498 23 1902 1211 23 1903 1060 23 1904 898 23 1905 944 23 1906 970 23 1907 749 23 1908 950 23 1909 598 23 1910 1040 23 1911 918 23 1912 911 23 1913 1181 23 1914 1386 23 1915 1339 23 1916 1053 23 1917 1217 23 1918 1011 23 1919 1469 23 1920 1195 23 1921 1041 23 1922 998 23 1923 985 23 1924 962 23 1925 882 22 1926 903 22 1927 652 22 1928 541 22 1929 579 22 1930 905 22 1931 1011 22 1932 979 22 1933 875 22 1934 802 22 1935 587 22 1936 1197 22 1937 1229 22 1938 911 22 1939 1116 22 1940 1426 22 1941 1612 22 1942 1178 22 1943 1098 22 1944 842 22 1945 517 22 1946 840 22 1947 920 22 1948 909 22 1949 718 22 1950 1104 22 1951 1254 22 1952 922 22 1953 853 22 1954 1166 22 1955 1165 22 1956 900 22 1957 840 22 1958 1058 22 1959 1290 22 1960 1507 22 1961 1355 22 1962 874 22 1963 798 22 1964 770 22 1965 942 22 1966 1098 22 1967 884 22 1968 820 22 1969 933 22 1970 1017 22 1971 1139 22 1972 1559 22 1973 1029 22 1974 784 22 1975 1396 22 1976 1025 22 1977 748 22 1978 804 22 1979 1238 22 1980 994 22 1981 1296 22 1982 1290 22 1983 1409 22 1984 1279 22 1985 954 22 1986 779 22 1987 844 22 1988 1020 22 1989 793 22 1990 784 22 1991 1239 22 1992 1257 22 1993 817 22 1994 728 22 1995 619 22 1996 817 22 1997 1045 22 1998 1405 22 1999 1338 22 2000 1033 22 2001 1010 22 2002 897 22 2003 663 22 2004 973 22 2005 1124 22 2006 732 22 2007 707 22 2008 770 22