# Kose - Kayseri - PINI - ITRDB TURK051 #----------------------------------------------------------------------- # 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/22356 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/europe/turk051r-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk051r.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 - Kayseri - PINI - ITRDB TURK051 #------------------- # 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 1533 1658 1 1534 1575 2 1535 567 2 1536 1121 2 1537 894 2 1538 791 2 1539 1189 2 1540 811 2 1541 1008 2 1542 805 2 1543 757 2 1544 1130 2 1545 1175 2 1546 1173 2 1547 1007 2 1548 848 2 1549 1013 2 1550 1610 2 1551 907 2 1552 899 2 1553 1137 2 1554 957 2 1555 1180 2 1556 1042 2 1557 918 2 1558 1049 2 1559 1455 2 1560 1177 2 1561 798 2 1562 970 2 1563 1352 2 1564 1160 2 1565 1100 2 1566 1414 2 1567 681 2 1568 833 2 1569 1055 2 1570 666 2 1571 921 2 1572 940 2 1573 914 2 1574 1020 2 1575 1139 2 1576 1175 2 1577 837 2 1578 1075 2 1579 960 2 1580 873 2 1581 1305 2 1582 969 2 1583 946 2 1584 981 2 1585 800 2 1586 1257 2 1587 1020 2 1588 663 2 1589 971 2 1590 915 2 1591 885 2 1592 970 2 1593 874 2 1594 522 2 1595 803 2 1596 840 2 1597 839 2 1598 931 2 1599 759 2 1600 740 2 1601 873 2 1602 1136 2 1603 962 2 1604 1038 2 1605 1125 2 1606 1284 2 1607 591 2 1608 629 2 1609 822 3 1610 784 3 1611 1018 3 1612 1176 3 1613 761 3 1614 873 3 1615 872 3 1616 893 3 1617 1257 3 1618 939 3 1619 1065 3 1620 1127 3 1621 1215 3 1622 1063 3 1623 695 3 1624 960 3 1625 1090 3 1626 817 3 1627 889 3 1628 893 3 1629 1028 3 1630 1024 3 1631 1070 3 1632 933 3 1633 653 3 1634 906 3 1635 832 3 1636 892 3 1637 773 3 1638 1052 3 1639 971 3 1640 1337 3 1641 1022 3 1642 1007 3 1643 1251 3 1644 905 4 1645 719 4 1646 1166 4 1647 780 4 1648 803 4 1649 1105 4 1650 668 4 1651 952 4 1652 926 4 1653 895 4 1654 978 4 1655 886 4 1656 855 4 1657 1042 4 1658 1156 4 1659 1037 5 1660 828 5 1661 967 5 1662 879 5 1663 1174 5 1664 711 5 1665 1030 5 1666 976 5 1667 1032 5 1668 776 5 1669 1210 5 1670 933 5 1671 869 5 1672 703 5 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