# 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/turk049r-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk049r.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,residual,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1753 1499 1 1754 1339 2 1755 1513 2 1756 1274 2 1757 408 2 1758 1479 2 1759 772 2 1760 963 2 1761 767 2 1762 936 2 1763 917 2 1764 1114 2 1765 890 2 1766 1200 2 1767 845 2 1768 859 2 1769 687 2 1770 800 2 1771 1071 2 1772 906 2 1773 956 2 1774 884 2 1775 935 2 1776 681 2 1777 692 2 1778 1220 2 1779 954 2 1780 1018 2 1781 765 2 1782 741 2 1783 990 3 1784 1242 3 1785 1230 4 1786 1248 6 1787 922 6 1788 931 7 1789 1009 8 1790 914 8 1791 1077 9 1792 1228 10 1793 1062 10 1794 985 10 1795 807 10 1796 1070 10 1797 960 10 1798 1246 10 1799 1075 10 1800 1167 10 1801 880 11 1802 953 11 1803 924 12 1804 941 12 1805 990 12 1806 838 12 1807 1107 12 1808 1010 12 1809 965 12 1810 1091 12 1811 1005 12 1812 930 12 1813 966 12 1814 1105 12 1815 785 14 1816 1211 14 1817 1054 14 1818 884 14 1819 848 14 1820 881 14 1821 1125 14 1822 889 14 1823 1018 14 1824 868 14 1825 959 14 1826 1030 16 1827 977 16 1828 864 16 1829 1320 16 1830 688 16 1831 1057 17 1832 824 17 1833 993 18 1834 847 18 1835 1229 18 1836 999 18 1837 1158 18 1838 1045 18 1839 1039 19 1840 664 19 1841 1054 19 1842 893 20 1843 1101 20 1844 895 20 1845 886 20 1846 1145 20 1847 883 20 1848 1093 20 1849 1044 20 1850 1002 20 1851 884 20 1852 994 20 1853 1096 20 1854 895 20 1855 1103 20 1856 934 20 1857 1003 20 1858 1045 20 1859 1016 20 1860 886 20 1861 966 20 1862 928 20 1863 826 20 1864 940 20 1865 1090 20 1866 1021 20 1867 983 20 1868 904 20 1869 1104 20 1870 906 20 1871 1125 20 1872 1101 20 1873 839 20 1874 900 20 1875 937 20 1876 1024 20 1877 1216 20 1878 907 20 1879 1032 20 1880 937 20 1881 1114 20 1882 880 20 1883 961 20 1884 1076 20 1885 1154 20 1886 947 20 1887 747 20 1888 1136 20 1889 1278 20 1890 813 20 1891 1058 20 1892 913 20 1893 731 20 1894 902 20 1895 1077 20 1896 942 20 1897 1308 20 1898 1180 20 1899 869 20 1900 1219 20 1901 1471 20 1902 1138 20 1903 1088 20 1904 715 20 1905 819 20 1906 1087 20 1907 836 20 1908 895 20 1909 862 20 1910 1125 20 1911 876 20 1912 1105 20 1913 973 20 1914 1068 20 1915 1418 20 1916 1036 20 1917 1244 20 1918 956 20 1919 1428 20 1920 852 20 1921 719 20 1922 1042 20 1923 939 20 1924 933 20 1925 1017 20 1926 910 20 1927 831 20 1928 810 20 1929 969 20 1930 1007 20 1931 1118 20 1932 857 20 1933 1173 20 1934 841 20 1935 894 20 1936 1235 20 1937 852 20 1938 883 20 1939 1169 20 1940 1263 20 1941 962 20 1942 852 20 1943 909 20 1944 1020 20 1945 757 20 1946 825 20 1947 817 20 1948 940 20 1949 765 20 1950 1025 20 1951 1051 20 1952 875 20 1953 992 20 1954 1099 20 1955 1024 20 1956 936 20 1957 840 20 1958 1125 20 1959 1142 20 1960 1023 20 1961 976 20 1962 1154 20 1963 1040 20 1964 980 20 1965 1103 20 1966 943 20 1967 845 20 1968 834 20 1969 999 20 1970 1155 20 1971 1155 20 1972 988 20 1973 1135 20 1974 1032 20 1975 1105 20 1976 972 20 1977 865 20 1978 1253 20 1979 1279 20 1980 1078 20 1981 1099 20 1982 1039 20 1983 1096 20 1984 936 20 1985 1100 20 1986 1053 20 1987 889 20 1988 1023 20 1989 766 20 1990 843 20 1991 1096 20 1992 1019 20 1993 934 20 1994 823 20 1995 799 19 1996 1070 18 1997 1030 18 1998 915 18 1999 951 18 2000 1032 18 2001 1247 17 2002 1016 14 2003 563 12 2004 1314 12 2005 1048 12 2006 777 12 2007 863 12 2008 1377 9 2009 1092 2