# 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/turk048a-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/europe/turk048a.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,ARSTAN,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1502 1018 1 1503 615 1 1504 519 1 1505 794 1 1506 963 1 1507 921 1 1508 918 1 1509 955 1 1510 916 1 1511 1036 1 1512 726 1 1513 889 1 1514 759 1 1515 1019 1 1516 878 1 1517 1052 1 1518 1268 1 1519 1132 1 1520 1068 1 1521 639 1 1522 617 1 1523 723 1 1524 391 1 1525 420 1 1526 508 2 1527 689 2 1528 1163 2 1529 1267 2 1530 1260 2 1531 1009 3 1532 1066 3 1533 1280 3 1534 1170 3 1535 1118 3 1536 1115 3 1537 1007 3 1538 1012 3 1539 848 3 1540 658 3 1541 1230 3 1542 939 3 1543 936 3 1544 1194 3 1545 1168 3 1546 1403 3 1547 1061 3 1548 1232 4 1549 1191 4 1550 1137 4 1551 781 4 1552 837 4 1553 940 4 1554 1105 4 1555 1022 4 1556 955 4 1557 955 4 1558 1049 4 1559 1137 4 1560 1083 4 1561 1005 4 1562 1140 4 1563 1075 4 1564 908 4 1565 1078 4 1566 1160 4 1567 967 4 1568 933 4 1569 923 5 1570 879 5 1571 1070 5 1572 944 5 1573 1008 5 1574 914 5 1575 1019 5 1576 1072 5 1577 814 5 1578 971 5 1579 966 5 1580 851 5 1581 939 5 1582 968 5 1583 1056 5 1584 873 5 1585 1047 5 1586 1003 5 1587 1123 5 1588 1154 5 1589 1130 5 1590 963 5 1591 1096 5 1592 961 5 1593 1073 5 1594 1129 5 1595 974 5 1596 962 5 1597 1034 5 1598 924 5 1599 894 5 1600 1089 5 1601 1091 5 1602 914 5 1603 855 6 1604 784 7 1605 892 7 1606 885 7 1607 1013 7 1608 1159 7 1609 1042 7 1610 1372 7 1611 1178 7 1612 1257 8 1613 1170 8 1614 1174 9 1615 1312 10 1616 1058 10 1617 790 10 1618 929 10 1619 830 10 1620 814 10 1621 932 10 1622 1077 10 1623 943 10 1624 895 12 1625 930 12 1626 977 12 1627 936 13 1628 838 13 1629 950 13 1630 973 13 1631 901 13 1632 887 13 1633 830 14 1634 939 14 1635 1011 14 1636 946 14 1637 977 14 1638 1063 14 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