# Kose - Artvin - ABNO - ITRDB TURK048 #----------------------------------------------------------------------- # 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/22352 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/europe/turk048r-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk048r.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 - Artvin - ABNO - ITRDB TURK048 #------------------- # 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 1507 1038 1 1508 990 1 1509 966 1 1510 923 1 1511 1080 1 1512 725 1 1513 984 1 1514 815 1 1515 1111 1 1516 936 1 1517 1095 1 1518 1279 1 1519 1017 1 1520 1026 1 1521 569 1 1522 693 1 1523 877 1 1524 535 1 1525 730 1 1526 772 2 1527 927 2 1528 1394 2 1529 1280 2 1530 1191 2 1531 887 3 1532 971 3 1533 1217 3 1534 1062 3 1535 1069 3 1536 1038 3 1537 916 3 1538 1002 3 1539 837 3 1540 704 3 1541 1366 3 1542 888 3 1543 993 3 1544 1237 3 1545 1036 3 1546 1375 3 1547 905 3 1548 1142 4 1549 1078 4 1550 1015 4 1551 745 4 1552 863 4 1553 995 4 1554 1149 4 1555 1049 4 1556 946 4 1557 952 4 1558 1043 4 1559 1134 4 1560 1047 4 1561 968 4 1562 1112 4 1563 1006 4 1564 878 4 1565 1104 4 1566 1112 4 1567 920 4 1568 952 4 1569 914 5 1570 895 5 1571 1142 5 1572 939 5 1573 1035 5 1574 919 5 1575 1027 5 1576 1085 5 1577 788 5 1578 1043 5 1579 968 5 1580 869 5 1581 1029 5 1582 982 5 1583 1082 5 1584 878 5 1585 1082 5 1586 987 5 1587 1116 5 1588 1134 5 1589 1050 5 1590 908 5 1591 1073 5 1592 912 5 1593 1082 5 1594 1120 5 1595 910 5 1596 976 5 1597 1024 5 1598 905 5 1599 939 5 1600 1130 5 1601 1062 5 1602 901 5 1603 881 6 1604 806 7 1605 976 7 1606 966 7 1607 1085 7 1608 1184 7 1609 987 7 1610 1353 7 1611 1024 7 1612 1152 8 1613 1059 8 1614 1040 9 1615 1242 10 1616 913 10 1617 746 10 1618 968 10 1619 834 10 1620 916 10 1621 1047 10 1622 1109 10 1623 951 10 1624 924 12 1625 952 12 1626 991 12 1627 972 13 1628 875 13 1629 1009 13 1630 998 13 1631 931 13 1632 942 13 1633 864 14 1634 1008 14 1635 1060 14 1636 963 14 1637 1012 14 1638 1063 14 1639 942 14 1640 1034 15 1641 937 15 1642 1010 15 1643 760 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