# 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/turk051a-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk051a.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,ARSTAN,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1532 974 1 1533 1641 1 1534 2009 2 1535 1250 2 1536 1291 2 1537 1091 2 1538 853 2 1539 1090 2 1540 872 2 1541 921 2 1542 752 2 1543 589 2 1544 852 2 1545 1075 2 1546 1224 2 1547 1159 2 1548 956 2 1549 983 2 1550 1599 2 1551 1312 2 1552 1110 2 1553 1212 2 1554 1101 2 1555 1248 2 1556 1210 2 1557 1060 2 1558 1090 2 1559 1516 2 1560 1527 2 1561 1155 2 1562 1075 2 1563 1403 2 1564 1433 2 1565 1393 2 1566 1681 2 1567 1142 2 1568 929 2 1569 1007 2 1570 671 2 1571 698 2 1572 736 2 1573 735 2 1574 840 2 1575 1030 2 1576 1196 2 1577 969 2 1578 1054 2 1579 997 2 1580 871 2 1581 1217 2 1582 1115 2 1583 1024 2 1584 997 2 1585 798 2 1586 1120 2 1587 1101 2 1588 731 2 1589 789 2 1590 772 2 1591 730 2 1592 787 2 1593 730 2 1594 339 2 1595 355 2 1596 403 2 1597 435 2 1598 549 2 1599 453 2 1600 369 2 1601 446 2 1602 761 2 1603 800 2 1604 902 2 1605 1059 2 1606 1324 2 1607 810 2 1608 501 2 1609 484 3 1610 434 3 1611 635 3 1612 929 3 1613 713 3 1614 678 3 1615 654 3 1616 658 3 1617 1026 3 1618 957 3 1619 1035 3 1620 1151 3 1621 1317 3 1622 1278 3 1623 883 3 1624 881 3 1625 1010 3 1626 824 3 1627 770 3 1628 737 3 1629 850 3 1630 922 3 1631 1018 3 1632 945 3 1633 616 3 1634 646 3 1635 592 3 1636 616 3 1637 513 3 1638 722 3 1639 783 3 1640 1190 3 1641 1151 3 1642 1110 3 1643 1325 3 1644 1125 4 1645 803 4 1646 1033 4 1647 802 4 1648 669 4 1649 881 4 1650 587 4 1651 672 4 1652 704 4 1653 694 4 1654 771 4 1655 731 4 1656 673 4 1657 820 4 1658 1034 4 1659 1060 5 1660 869 5 1661 878 5 1662 796 5 1663 1036 5 1664 735 5 1665 851 5 1666 875 5 1667 947 5 1668 740 5 1669 1034 5 1670 956 5 1671 839 5 1672 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