NOAA/WDS Paleoclimatology - Amundsenisen Dronning Maud Land oxygen isotope and accumulation rate data from 1895-1996 CE
This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Ice Core. The data include parameters of ice cores with a geographic location of Antarctica. The time period coverage is from 55 to -46 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
- Cite as: Oerter, H.; Graf, W.; Wilhelms, F.; Minikin, A.; Miller, H. (2017-11-17): NOAA/WDS Paleoclimatology - Amundsenisen Dronning Maud Land oxygen isotope and accumulation rate data from 1895-1996 CE. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/yztw-8j34. Accessed [date].
- Please refer to Credit tab for full citation information.
- doi:10.25921/yztw-8j34
- noaa-icecore-23235
- NCEI DSI 1200_02
- NCEI DSI 1200_01
noaa-icecore-23235
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Distributor | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | NOAA National Centers for Environmental Information
ncei.info@noaa.gov |
Dataset Point of Contact | Data Center Contact
NOAA World Data Service for Paleoclimatology 828-271-4800 paleo@noaa.gov |
Coverage Description | Date Range: 1895 CE to 1996 CE; Date Range: 55 cal yr BP to -46 cal yr BP; |
Time Period | 1895 to 1996 |
Spatial Bounding Box Coordinates |
N: -74.4094
S: -75.9333
E: 11.35
W: -2.55
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Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns
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Dataset Progress Status | Complete - production of the data has been completed |
Data Update Frequency | Data update frequency not available |
Supplemental Information |
STUDY NOTES: DML data contributed to the PAGES 2k project Provided Keywords: oxygen isotope of water, temperature proxy, accumulation rate
ABSTRACT SUPPLIED BY ORIGINATOR: The paper focuses on studies of snow-pit samples and shallow firn cores taken during the 1995–96 and 1996–97 field seasons at Amundsenisen, Dronning Maud Land, Antarctica. The dating of the firn is based on the artificial tritium distribution in the snow cover and on several reference horizons identified by electrical measurements. The early 1964 through 1965 horizon is marked by the deposition of sulfate released to the atmosphere during the eruption of the Agung volcano in March 1963; this horizon was detected by dielectric profiling and electrical conductivity measurements; the proof by chemical analysis has still to be seen. At the ten investigated sites on Amundsenisen the 1964–65 horizon was identified 4.1–5.7 m below the surface. The accumulation rates on Amundsenisen are 41–91 kg m-2a-1. The cores are up to 100 years old. A relationship between isotope content and the mean air temperature on a regional scale can be based on measurements of firn temperature at 10 m depth at the drilling sites. Between Neumayer station at the coast and Heimefrontfjella, the temperature gradient of the deuterium content is 9.6‰ K-1. South of Heimefrontfjella, on the Amundsenisen plateau, it is only 5.5‰ K-1. Time series of yearly accumulation rates show no significant trend. For the isotope records a significant trend to higher values with gradients of 0.1–0.2 ?2H‰a-1 can be seen in five of the ten time series. |
Purpose | Records of past temperature, precipitation, atmospheric trace gases, and other aspects of climate and environment derived from ice cores drilled on glaciers and ice caps around the world. Parameter keywords describe what was measured in this dataset. Additional summary information can be found in the abstracts of papers listed in the dataset citations. |
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Theme keywords | Global Change Master Directory (GCMD) Science Keywords
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Data Center keywords | Global Change Master Directory (GCMD) Data Center Keywords
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Last Modified: 2024-04-17
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