# Dome Fuji Ice Core 340KYr (2500m) d18O Data #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite original reference 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:6076 # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611 # # Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/domefuji/df-d18o-340ka-dfo2006.txt # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Ice Cores # -------------------- # Contribution_date # Date: 2007 # -------------------- # Title # Study_Name: Dome Fuji Ice Core 340KYr (2500m) d18O Data # -------------------- # Investigators # Investigators: Kawamura, K.; Parrenin, F.; Lisiecki, L.; Uemura, R.; Vimeux, F.; Severinghaus, J.P.; Hutterli, M.A.; Nakazawa, T.; Aoki, S.; Jouzel, J.; Raymo, M.E.; Matsumoto, K.; Nakata, H.; Motoyama, H.; Fujita, S.; Goto-Azuma, K.; Fuji, Y.; Watanabe, O. # -------------------- # Description_and_Notes # Description: d18O data of the first Dome Fuji ice core (DF1) for 0-2500 m (340 kyr). # # Raw data were obtained from measurements of continuous 10-cm samples # for 0-2300 m (~255 kyr), and of discontinuous 25-cm samples # (25-cm gap between two samples) for 2300-2500 m, with uncertainty of # 0.05 per mil. The data were put on DFO-2006 age scale and then averaged # at 250 yr intervals (for 0-254.5 kyr b2k) and 500 yr intervals # (for 254.5-339.5 kyr b2k, where raw data are discontinuous). # The depth at the top of intervals was re-interpolated from the age. # For plotting the data, use staircase (cityscape) function using # 'Top age', or linear function using 'Center age'. Note that age is # given in b2k (before AD 2000). See also temperature reconstruction # based on this data and delta D data of the Dome Fuji core. # # -------------------- # Publication # Authors: K. Kawamura, F. Parrenin, L. Lisiecki, R. Uemura, F. Vimeux, J.P. Severinghaus, M. A. Hutterli, T. Nakazawa, S. Aoki, J. Jouzel, M. E. Raymo, K. Matsumoto, H. Nakata, H. Motoyama, S. Fujita, K. Goto-Azuma, Y. Fujii, and O. Watanabe # Published_Date_or_Year: 2007 # Published_Title: Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years # Journal_Name: Nature # Volume: 448 # Edition: # Issue: # Pages: 912-916 # DOI: 10.1038/nature06015 # Online_Resource: # Full_Citation: # Abstract: The Milankovitch theory of climate change proposes that glacial- interglacial cycles are driven by changes in summer insolation at high northern latitudes. The timing of climate change in the Southern Hemisphere at glacial-interglacial transitions (which are known as terminations) relative to variations in summer insolation in the Northern Hemisphere is an important test of this hypothesis. So far, it has only been possible to apply this test to the most recent termination, because the dating uncertainty associated with older terminations is too large to allow phase relationships to be determined. Here we present a new chronology of Antarctic climate change over the past 360,000 years that is based on the ratio of oxygen to nitrogen molecules in air trapped in the Dome Fuji and Vostok ice cores. This ratio is a proxy for local summer insolation, and thus allows the chronology to be constructed by orbital tuning without the need to assume a lag between a climate record and an orbital parameter. The accuracy of the chronology allows us to examine the phase relationships between climate records from the ice cores and changes in insolation. Our results indicate that orbital-scale Antarctic climate change lags Northern Hemisphere insolation by a few millennia, and that the increases in Antarctic temperature and atmospheric carbon dioxide concentration during the last four terminations occurred within the rising phase of Northern Hemisphere summer insolation. These results support the Milankovitch theory that Northern Hemisphere summer insolation triggered the last four deglaciations. # -------------------- # 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: Grant-in-Aid for Creative Scientific Research # Grant: # -------------------- # Funding_Agency # Funding_Agency_Name: The Gary Comer Abrupt Climate Change Fellowship # Grant: 2122102 # -------------------- # Funding_Agency_Name: National Science Foundation # Grant:AGS-1304263 # Funding_Agency_Name: National Oceanic and Atmospheric Administration # Grant:NA14OAR4310176 #------------------ # Site_Information # Site_Name: Dome Fuji # Location: Antarctica # Country: # Northernmost_Latitude: -77.31667 # Southernmost_Latitude: -77.31667 # Easternmost_Longitude: 38.70 # Westernmost_Longitude: 38.70 # Elevation: 3810 m # -------------------- # Data_Collection # Collection_Name: 07Fuji01 # Earliest_Year: 339500 # Most_Recent_Year: 125 # Time_Unit: yb_2000 # Notes: 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