# Kose - Payanburnu - PINI - ITRDB TURK053 #----------------------------------------------------------------------- # 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/22358 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/europe/turk053r-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk053r.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 - Payanburnu - PINI - ITRDB TURK053 #------------------- # 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 1538 920 1 1539 1484 1 1540 728 1 1541 1271 1 1542 1644 1 1543 1292 1 1544 963 1 1545 1395 1 1546 857 1 1547 1026 1 1548 1285 2 1549 720 2 1550 1121 2 1551 1084 2 1552 1059 2 1553 952 2 1554 1245 2 1555 1235 2 1556 1413 2 1557 976 2 1558 1122 2 1559 1184 2 1560 961 2 1561 719 2 1562 1121 2 1563 1215 2 1564 883 2 1565 1247 2 1566 830 2 1567 902 2 1568 703 2 1569 899 2 1570 870 2 1571 849 2 1572 763 2 1573 969 2 1574 899 2 1575 842 2 1576 959 2 1577 915 2 1578 698 2 1579 846 2 1580 858 2 1581 1089 2 1582 625 2 1583 969 2 1584 937 2 1585 589 2 1586 1055 2 1587 903 2 1588 851 2 1589 890 2 1590 1069 2 1591 1001 2 1592 629 2 1593 928 2 1594 1331 2 1595 1090 2 1596 701 2 1597 1105 2 1598 1016 2 1599 831 2 1600 778 2 1601 1227 2 1602 1189 2 1603 827 2 1604 1078 2 1605 971 2 1606 1221 2 1607 633 2 1608 1020 2 1609 1079 2 1610 878 2 1611 848 2 1612 934 2 1613 1066 2 1614 1205 2 1615 843 2 1616 824 2 1617 1008 2 1618 1099 2 1619 907 2 1620 972 2 1621 1267 2 1622 623 2 1623 672 2 1624 969 2 1625 1124 2 1626 782 2 1627 1088 2 1628 817 2 1629 1108 2 1630 775 2 1631 1013 2 1632 932 2 1633 996 2 1634 942 2 1635 846 2 1636 1127 2 1637 1039 2 1638 1053 2 1639 764 2 1640 1403 2 1641 1093 2 1642 1234 2 1643 1188 2 1644 865 2 1645 762 2 1646 1431 2 1647 1077 2 1648 1194 2 1649 1321 2 1650 887 2 1651 1295 2 1652 1252 2 1653 1249 2 1654 750 2 1655 1254 2 1656 1092 2 1657 1396 2 1658 1137 2 1659 1124 2 1660 702 2 1661 1084 2 1662 1035 2 1663 936 2 1664 904 2 1665 984 2 1666 977 2 1667 1182 2 1668 857 2 1669 1350 2 1670 1194 2 1671 947 2 1672 666 2 1673 1248 2 1674 886 2 1675 788 2 1676 883 2 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