Supporting Information for The potential of 233U/236U as a water mass tracer in the Arctic Ocean
File content: Texts 1 and 2; Figures S1 and S2 Dataset published as supplementary material of Chamizo et al. (2022), http://doi.org/10.1029/2021JC017790. This supporting material includes two Texts with further explanations on two points given in the manuscript: Text 1 explains the calculations used...
Main Authors: | , , , , , |
---|---|
Other Authors: | , |
Format: | Dataset |
Language: | English |
Published: |
John Wiley & Sons
2022
|
Subjects: | |
Online Access: | http://hdl.handle.net/10261/310297 https://doi.org/10.1029/2021JC017790 |
Summary: | File content: Texts 1 and 2; Figures S1 and S2 Dataset published as supplementary material of Chamizo et al. (2022), http://doi.org/10.1029/2021JC017790. This supporting material includes two Texts with further explanations on two points given in the manuscript: Text 1 explains the calculations used to model the input function of the 233U/236U ratio in the Atlantic Layer of the Arctic Ocean; Text 2 presents the adopted calculations to estimate the 233U/236U ratio in the surface of the rocks due to natural production processes, and the adopted number for the U present in Deep and Bottom Waters in the Amerasian Basin. Figure S1 compares the obtained ICP-MS 238U results in this work with the predicted ones based on salinity data using the empirical formula given in (Owens et al., 2011). Figure S2 shows how the modelled 233U/236U ratios for the Atlantic Layer in Text 2 compares with the obtained values in this work. Peer reviewed |
---|