East Asian Monsoon behaviour reflected in the stable isotope hydrology of Lake Suigetsu and surrounding catchment, Japan

1429 22 5760 2 30800 document 5760 RexetalSuigetsuModernIsotopesDatasetREADME.txt text/plain 09b36be0039fbe8b45a98127e0c73fc2 MD5 1168 2023-04-28 14:32:57 https://researchdata.gla.ac.uk/1429/2/RexetalSuigetsuModernIsotopesDatasetREADME.txt 1429 2 2 text/plain Text en public cc_by_4

RexetalSuigetsuModernIsotopesDatasetREADME.txt

readme 5762 1 30810 document 5762 indexcodes.txt text/x-c c58141c0247923d7d1f45b9fb0ba0d47 MD5 769 2023-04-28 14:43:02 https://researchdata.gla.ac.uk/1429/3/indexcodes.txt 1429 3 3 text/x-c other Generate index codes conversion from Text to indexcodes en public

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RexetalSuigetsuModernIsotopesDataset.xlsx

data archive 32960 disk0/00/00/14/29 2023-10-03 12:41:48 2024-04-11 11:59:45 2023-10-03 12:41:48 data_collection show Rex Charlie 52294 0000-0003-2068-4836 Tyler Jonathan L Nagaya Kazuyoshi Staff Richard A Leng Melanie J Yamada Keitaro Kitaba Ikuko Kitagawa Junko Kojima Hideaki Nakagawa Takeshi glaresearchdata:2023-04-28-1429 East Asian Monsoon behaviour reflected in the stable isotope hydrology of Lake Suigetsu and surrounding catchment, Japan 30000000 This research was funded by the IAPETUS2 Doctoral Training Partnership, the Australian Research Council Discovery Project (DP200101768) and the JSPS KAKENHI Grant (19K20442) Stable oxygen and hydrogen isotope composition of water samples from the Five Lakes of Mikata catchment, central Japan. Samples consist of rainwater, river water and lake water. Sampling information and accompanying weather data are also provided. (Sheet 1) Temperature and salinity variations with depth within Lake Suigetsu across six sampling dates. (Sheet 2) 2023-04-28 University of Glasgow 10.5525/gla.researchdata.1429 Spreadsheet Charlie L Rex FALSE English 2011-03-01 2022-07-22 https://theses.gla.ac.uk/84032/ thesis 2033-04-28 R email FALSE FALSE The contemporary stable isotope hydrology of Lake Suigetsu and surrounding catchment (Japan) and its implications for sediment-derived palaeoclimate records https://eprints.gla.ac.uk/id/eprint/309801