# Crystal Cave, California 1150 Year d18O Data and SST Reconstruction #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # # Online_Resource: https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_STUDY_ID:14652 # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611 # # Original_Source_URL: http://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/northamerica/usa/california/crystal2013.txt # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Speleothems #-------------------- # Contribution_Date # Date: 2013-07-11 #-------------------- # Title # Study_Name: Crystal Cave, California 1150 Year d18O Data and SST Reconstruction #-------------------- # Investigators # Investigators: McCabe-Glynn, S.; Johnson, K.R.; Strong, C.; Berkelhammer, M.; Sinha, A.; Cheng, H.; Edwards, R.L.; #-------------------- # Description_and_Notes # Description: Speleothem oxygen isotope (d18O) record and Kuroshio Extension (KE) SST anomalies reconstructed from the isotope data. The record spans 854 - 2007 AD and is based on a speleothem (CRC-3) collected from Crystal Cave, located in Sequoia National Park, California. #-------------------- # Publication # Authors: McCabe-Glynn, S.; Johnson, K.R.; Strong, C.; Berkelhammer, M.; Sinha, A.; Cheng, H.; Edwards, R.L.; # Published_Date_or_Year: 2013-07-07 # Published_Title: Variable North Pacific influence on drought in southwestern North America since AD 854 # Journal_Name: Nature Geoscience # Volume: Published online 07 July 2013 # Edition: # Issue: # Pages: # DOI: 10.1038/ngeo1862 # Online_Resource: # Full_Citation: Staryl McCabe-Glynn, Kathleen R. Johnson, Courtenay Strong, Max Berkelhammer, Ashish Sinha, Hai Cheng and R. Lawrence Edwards. 2013. Variable North Pacific influence on drought in southwestern North America since AD 854. Nature Geoscience, DOI: 10.1038/ngeo1862. Published online 07 July 2013. # Abstract: Precipitation in southwestern North America has exhibited significant natural variability over the past few thousand years. This variability has been attributed to sea surface temperature regimes in the Pacific and Atlantic oceans, and to the attendant shifts in atmospheric circulation patterns. In particular, decadal variability in the North Pacific has influenced precipitation in this region during the twentieth century, but links to earlier droughts and pluvials are unclear. Here we assess these links using d18O data from a speleothem from southern California that spans AD 854-2007. We show that variations in the oxygen isotopes of the speleothem correlate to sea surface temperatures in the Kuroshio Extension region of the North Pacific, which affect the atmospheric trajectory and isotopic composition of moisture reaching the study site. Interpreting our speleothem data as a record of sea surface temperatures in the Kuroshio Extension, we find a strong 22-year periodicity, suggesting a persistent solar influence on North Pacific decadal variability. A comparison with tree-ring records of precipitation during the past millennium shows that some droughts occurred during periods of warmth in the Kuroshio Extension, similar to the instrumental record. However, other droughts did not and instead must have been influenced by other factors. Finally, we find a significant increase in sea surface temperature variability over the past 150 years, which may reflect an influence of greenhouse gas concentrations on variability in the North Pacific. #------------------ # Authors: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G.J., Noone, D., Perkins, W.A., and E. Steig # Published_Date_or_Year: 2018 # Published_Title: Additions to the last millennium reanalysis multi-proxy database # Journal_Name: Data Science Journal # Volume: # Edition: # Issue: # Pages: # Report_Number: # DOI: # Online_Resource: # Full_Citation: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G., J., Noone, D., Perkins, W.A., and E. Steig, submitted. Additions to the last millennium reanalysis multi-proxy database. Data Science Journal. # Abstract: Progress in paleoclimatology increasingly occurs via data syntheses. We describe additions to a collection prepared for use in paleoclimate state estimation, specifically the Last Millennium Reanalysis (LMR). The 2290 additional series include 2152 tree ring chronologies and 138 other series. They supplement the collection used previously and together form a database titled LMRdb 1.0.0. The additional data draws from lake core, ice core, coral, speleothem, and tree ring archives, using published data primarily from the NOAA Paleoclimatology archive and a set of tree ring width chronologies standardized from raw International Tree Ring Data Bank ring width series. In contrast to many previous paleo compilations, the data were not selected (screened) on the basis of their environmental correlation, multi-century length, or other attributes. The inclusion of proxies sensitive to moisture and other environmental variables expands their use in data assimilation. A preliminary calibration using linear regression with mean annual temperature reveals characteristics of the proxy series and their relationship to temperature, as well as the noise and error characteristics of the records. The additional records are structured as individual files in the NOAA Paleoclimatology format and archived at NOAA Paleoclimatology (Anderson et al. 2018) and will continue to be improved and expanded as part of the LMR Project. The additions represent a four-fold increase in the number of records available for assimilation, provide expanded geographic coverage, and add additional proxy variables. Applications include data assimilation, proxy system model development, and paleoclimate reconstruction using climate field reconstruction and other methods. #------------------ # Funding_Agency # Funding_Agency_Name: Newkirk Center for Science and Society, University of California, Irvine # Grant: 0823554, 1103360 #------------------ # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: 0823554, 1103360 #------------------ # Funding_Agency # Funding_Agency_Name: National Science Foundation of China # Grant: 41230524 #------------------ # Funding_Agency_Name: National Science Foundation # Grant:AGS-1304263 # Funding_Agency_Name: National Oceanic and Atmospheric Administration # Grant:NA14OAR4310176 #------------------ # Site_Information # Site_Name: Crystal Cave, California # Location: North America>United States Of America>California # Country: United States of America # Northernmost_Latitude: 36.57 # Southernmost_Latitude: 36.57 # Easternmost_Longitude: -118.78 # Westernmost_Longitude: -118.78 # Elevation: 1640 m #------------------ # Data_Collection # Collection_Name: 13cali01a # Earliest_Year: 854 # Most_Recent_Year: 2007 # Time_Unit: y_ad # Core_Length: m # Notes: {"database":"LMR"} #------------------ # Chronology: Supplementary Table 2. 230Th dating results for stalagmite CRC-3. # # Sample Depth 238U 232Th 230Th/232Th d234U* 230Th/238U 230Th Age (yr) 230Th Age (yr) d234Uinitial** 230Th Age (yr BP) # ID (mm) (ppb) (ppt) atomic x10-6 (measured) (activity) (uncorrected) (corrected) (corrected) (corrected) # CRC-3-1 9 220.0/- 0.4 933/- 19 14/- 1 -8.8/- 2.0 0.0035/- 0.0002 391/- 21 164/- 45 -9/- 2 105/- 45 # CRC-3-1A 23 187.7/- 0.2 546/- 11 24/- 3 -6.6/- 1.9 0.0043/- 0.0005 474/- 57 319/- 63 -7/- 2 259/- 63 # CRC-3-2 29 193.6/- 0.3 1563/- 31 14/- 1 -10.8/- 1.9 0.0068/- 0.0003 757/- 30 324/- 82 -11/- 2 265/- 82 # CRC-3-2B 48 190.8/- 0.2 1204/- 24 20/- 1 -11.8/- 1.8 0.0078/- 0.0004 862/- 49 523/- 78 -12/- 2 463/- 78 # CRC-3-3 55 166.8/- 0.3 732/- 15 27/- 1 -11.0/- 2.0 0.0073/- 0.0003 805/- 38 570/- 56 -11/- 2 511/- 56 # CRC-3-3C 65 169.6/- 0.2 1377/- 28 21/- 1 -13.6/- 2.2 0.0102/- 0.0007 1134/- 75 698/- 108 -14/- 2 638/- 108 # CRC-3-8 68 191.0/- 0.3 2706/- 54 17/- 1 -10.7/- 2.1 0.0143/- 0.0003 1592/- 39 832/- 141 -11/- 2 773/- 141 # CRC-3-4D 74 159.3/- 0.2 1250/- 25 24/- 2 -14.3/- 2.0 0.0114/- 0.0007 1266/- 79 844/- 109 -14/- 2 784/- 109 # CRC-3-4 77 153.5/- 0.3 1158/- 23 25/- 1 -6.0/- 2.2 0.0115/- 0.0005 1272/- 52 869/- 89 -6/- 2 810/- 89 # CRC-3-5 95 207.1/- 0.3 1826/- 37 26/- 1 -11.0/- 1.8 0.0137/- 0.0004 1525/- 42 1052/- 94 -11/- 2 993/- 94 # # *d234U = ([234U/238U]activity - 1)x1000. # "** d234Uinitial was calculated based on 230Th age (T), i.e., d234Uinitial = d234Umeasured x eLambda234xT." # Corrected 230Th ages assume the initial 230Th/232Th atomic ratio of 8 /- 1 x10-6. # # # # # # # # #---------------- # Variables # # Data variables follow that are preceded by "##" in columns one and two. # Data line variables format: Variables list, one per line, shortname-tab-longname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) # ##age age, , , Years AD, , , , ,N ##d18O delta 18 Oxygen, , , permil VPDB, , Speleothems, , ,N ##sst Sea Surface Temperature anomaly - Kuroshio Extension, , , deg C, , , SST anomaly vs. Kaplan SST AD 1857-2007, ,N #---------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Values: NAN # age 18O sst 854 -8.69 0.16 855 -8.69 0.16 856 -8.76 0.13 857 -8.77 0.13 858 -8.87 0.09 859 -8.98 0.06 860 -9.04 0.03 861 -8.98 0.06 862 -9.03 0.04 863 -9.21 -0.02 864 -9.18 -0.01 865 -9.04 0.03 866 -9 0.05 867 -9.13 0 868 -9 0.05 869 -9.2 -0.02 870 -9.12 0.01 871 -9.2 -0.02 872 -9.23 -0.03 873 -9.05 0.03 874 -8.9 0.08 875 -8.77 0.13 876 -8.68 0.16 877 -8.69 0.16 878 -8.6 0.19 879 -8.55 0.2 880 -8.67 0.16 881 -8.62 0.18 882 -8.61 0.18 883 -8.61 0.18 884 -8.55 0.2 885 -8.91 0.08 886 -8.98 0.06 887 -8.91 0.08 888 -8.99 0.05 889 -9.08 0.02 890 -9.14 0 891 -8.98 0.06 892 -8.47 0.23 893 -8.63 0.18 894 -8.65 0.17 895 -8.38 0.26 896 -8.37 0.27 897 -8.3 0.29 898 -8.38 0.26 899 -8.38 0.26 900 -8.41 0.25 901 -8.7 0.15 902 -9.03 0.04 903 -9.16 -0.01 904 -9.26 -0.04 905 -9.22 -0.03 906 -9.15 0 907 -9.18 -0.01 908 -9.07 0.02 909 -9.07 0.02 910 -9.11 0.01 911 -9.1 0.01 912 -8.96 0.06 913 -8.76 0.13 914 -8.7 0.15 915 -8.74 0.14 916 -8.72 0.15 917 -8.65 0.17 918 -8.6 0.19 919 -8.63 0.18 920 -8.86 0.1 921 -9.14 0 922 -9.29 -0.05 923 -9.26 -0.04 924 -9.25 -0.04 925 -9.27 -0.05 926 -9.23 -0.03 927 -9.18 -0.01 928 -9.12 0.01 929 -9.16 -0.01 930 -9.17 -0.01 931 -9.22 -0.03 932 -9.33 -0.07 933 -9.34 -0.07 934 -9.29 -0.05 935 -9.36 -0.08 936 -9.24 -0.03 937 -9.49 -0.12 938 -9.41 -0.09 939 -9.48 -0.12 940 -9.49 -0.12 941 -9.49 -0.12 942 -9.37 -0.08 943 -9.24 -0.03 944 -9.14 0 945 -9.07 0.02 946 -9.09 0.02 947 -9.02 0.04 948 -8.97 0.06 949 -8.9 0.08 950 -9.12 0.01 951 -8.86 0.1 952 -9.11 0.01 953 -8.8 0.12 954 -8.87 0.09 955 -8.67 0.16 956 -8.7 0.15 957 -8.62 0.18 958 -8.56 0.2 959 -8.55 0.2 960 -8.72 0.15 961 -8.81 0.11 962 -8.84 0.1 963 -8.88 0.09 964 -8.88 0.09 965 -9.02 0.04 966 -8.96 0.06 967 -8.9 0.08 968 -8.88 0.09 969 -8.88 0.09 970 -8.89 0.09 971 -8.78 0.12 972 -8.85 0.1 973 -8.84 0.1 974 -8.92 0.08 975 -8.95 0.07 976 -9.01 0.04 977 -9.1 0.01 978 -9.24 -0.03 979 -9.36 -0.08 980 -9.33 -0.07 981 -9.18 -0.01 982 -9.12 0.01 983 -9 0.05 984 -8.8 0.12 985 -8.97 0.06 986 -8.61 0.18 987 -8.78 0.12 988 -8.61 0.18 989 -8.58 0.19 990 -8.52 0.21 991 -8.49 0.22 992 -8.46 0.24 993 -8.42 0.25 994 -8.36 0.27 995 -8.29 0.29 996 -8.3 0.29 997 -8.32 0.28 998 -8.31 0.29 999 -8.36 0.27 1000 -8.34 0.28 1001 -8.67 0.16 1002 -8.65 0.17 1003 -8.67 0.16 1004 -8.88 0.09 1005 -8.91 0.08 1006 -8.75 0.13 1007 -8.85 0.1 1008 -9.02 0.04 1009 -8.97 0.06 1010 -8.98 0.06 1011 -8.94 0.07 1012 -8.88 0.09 1013 -8.86 0.1 1014 -8.75 0.13 1015 -8.59 0.19 1016 -8.58 0.19 1017 -8.61 0.18 1018 -8.76 0.13 1019 -8.53 0.21 1020 -8.54 0.21 1021 -8.47 0.23 1022 -8.53 0.21 1023 -8.54 0.21 1024 -8.65 0.17 1025 -8.69 0.16 1026 -8.75 0.13 1027 -8.91 0.08 1028 -9.03 0.04 1029 -9.11 0.01 1030 -9.26 -0.04 1031 -9.35 -0.07 1032 -9.23 -0.03 1033 -9.08 0.02 1034 -9.26 -0.04 1035 -9.18 -0.01 1036 -9.2 -0.02 1037 -9.04 0.03 1038 -8.88 0.09 1039 -8.79 0.12 1040 -8.63 0.18 1041 -8.47 0.23 1042 -8.44 0.24 1043 -8.44 0.24 1044 -8.37 0.27 1045 -8.47 0.23 1046 -8.55 0.2 1047 -8.6 0.19 1048 -8.72 0.15 1049 -8.7 0.15 1050 -8.73 0.14 1051 -8.77 0.13 1052 -8.78 0.12 1053 -8.76 0.13 1054 -8.77 0.13 1055 -8.96 0.06 1056 -9.21 -0.02 1057 -9.19 -0.02 1058 -9.07 0.02 1059 -9.07 0.02 1060 -9.04 0.03 1061 -8.89 0.09 1062 -8.88 0.09 1063 -8.95 0.07 1064 -8.9 0.08 1065 -8.88 0.09 1066 -8.87 0.09 1067 -8.92 0.08 1068 -9.06 0.03 1069 -9.11 0.01 1070 -9.02 0.04 1071 -8.9 0.08 1072 -8.81 0.11 1073 -8.9 0.08 1074 -8.92 0.08 1075 -8.97 0.06 1076 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1138 -9.5 -0.12 1139 -9.66 -0.18 1140 -9.7 -0.19 1141 -9.78 -0.22 1142 -9.59 -0.16 1143 -9.33 -0.07 1144 -9.12 0.01 1145 -8.86 0.1 1146 -8.83 0.11 1147 -8.86 0.1 1148 -8.92 0.08 1149 -9.04 0.03 1150 -8.98 0.06 1151 -8.85 0.1 1152 -8.94 0.07 1153 -8.94 0.07 1154 -8.86 0.1 1155 -8.75 0.13 1156 -8.8 0.12 1157 -9.14 0 1158 -9.1 0.01 1159 -9.12 0.01 1160 -9.43 -0.1 1161 -9.5 -0.12 1162 -9.51 -0.13 1163 -9.54 -0.14 1164 -9.56 -0.15 1165 -9.6 -0.16 1166 -9.67 -0.18 1167 -9.66 -0.18 1168 -9.72 -0.2 1169 -9.48 -0.12 1170 -9.52 -0.13 1171 -9.53 -0.13 1172 -9.51 -0.13 1173 -9.48 -0.12 1174 -9.46 -0.11 1175 -9.43 -0.1 1176 -9.37 -0.08 1177 -9.31 -0.06 1178 -9.37 -0.08 1179 -9.35 -0.07 1180 -9.3 -0.06 1181 -9.29 -0.05 1182 -9.22 -0.03 1183 -9.13 0 1184 -9.2 -0.02 1185 -9.28 -0.05 1186 -9.25 -0.04 1187 -9.29 -0.05 1188 -9.34 -0.07 1189 -9.24 -0.03 1190 -9.05 0.03 1191 -8.93 0.07 1192 -8.73 0.14 1193 -8.65 0.17 1194 -8.64 0.17 1195 -8.69 0.16 1196 -8.63 0.18 1197 -8.55 0.2 1198 -8.72 0.15 1199 -8.74 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-8.49 0.22 1883 -8.29 0.29 1884 -8.24 0.31 1885 -8.26 0.3 1886 -8.3 0.29 1887 -8.33 0.28 1888 -8.26 0.3 1889 -8.21 0.32 1890 -8.41 0.25 1891 -8.64 0.17 1892 -8.88 0.09 1893 -8.98 0.06 1894 -9.04 0.03 1895 -9.04 0.03 1896 -9.03 0.04 1897 -9.01 0.04 1898 -9.08 0.02 1899 -9.17 -0.01 1900 -9.42 -0.1 1901 -9.71 -0.2 1902 -10.15 -0.35 1903 -10.41 -0.44 1904 -10.38 -0.43 1905 -10.34 -0.42 1906 -10.29 -0.4 1907 -10.12 -0.34 1908 -9.74 -0.21 1909 -9.41 -0.09 1910 -9.19 -0.02 1911 -9.02 0.04 1912 -9.01 0.04 1913 -9.04 0.03 1914 -9.29 -0.05 1915 -9.54 -0.14 1916 -9.72 -0.2 1917 -9.88 -0.26 1918 -9.92 -0.27 1919 -9.9 -0.26 1920 -9.93 -0.27 1921 -10 -0.3 1922 -10.01 -0.3 1923 -9.79 -0.22 1924 -9.57 -0.15 1925 -9.56 -0.15 1926 -9.56 -0.15 1927 -9.46 -0.11 1928 -9.27 -0.05 1929 -9.15 0 1930 -9.32 -0.06 1931 -9.48 -0.12 1932 -9.54 -0.14 1933 -9.59 -0.16 1934 -9.65 -0.18 1935 -9.75 -0.21 1936 -9.85 -0.25 1937 -9.87 -0.25 1938 -9.9 -0.26 1939 -9.89 -0.26 1940 -9.86 -0.25 1941 -9.82 -0.24 1942 -9.67 -0.18 1943 -9.52 -0.13 1944 -9.39 -0.09 1945 -9.28 -0.05 1946 -9.17 -0.01 1947 -9.15 0 1948 -9.12 0.01 1949 -9.09 0.02 1950 -9.05 0.03 1951 -9.02 0.04 1952 -8.97 0.06 1953 -8.92 0.08 1954 -8.8 0.12 1955 -8.66 0.17 1956 -8.53 0.21 1957 -8.44 0.24 1958 -8.35 0.27 1959 -8.35 0.27 1960 -8.35 0.27 1961 -8.34 0.28 1962 -8.3 0.29 1963 -8.27 0.3 1964 -8.31 0.29 1965 -8.35 0.27 1966 -8.44 0.24 1967 -8.53 0.21 1968 -8.56 0.2 1969 -8.56 0.2 1970 -8.63 0.18 1971 -8.81 0.11 1972 -8.96 0.06 1973 -8.98 0.06 1974 -9.03 0.04 1975 -9.18 -0.01 1976 -9.3 -0.06 1977 -9.13 0 1978 -9.01 0.04 1979 -8.72 0.15 1980 -8.64 0.17 1981 -8.67 0.16 1982 -8.82 0.11 1983 -9.24 -0.03 1984 -9.6 -0.16 1985 -9.38 -0.08 1986 -9.39 -0.09 1987 -9.64 -0.17 1988 -9.82 -0.24 1989 -10.02 -0.3 1990 -10.02 -0.3 1991 -9.58 -0.15 1992 -9.42 -0.1 1993 -9.19 -0.02 1994 -9.19 -0.02 1995 -9.03 0.04 1996 -8.96 0.06 1997 -8.94 0.07 1998 -8.82 0.11 1999 -8.69 0.16 2000 -8.66 0.17 2001 -8.52 0.21 2002 -8.85 0.1 2003 -8.79 0.12 2004 -9 0.05 2005 -8.72 0.15 2006 -8.55 0.2 2007 -8.39 0.26