Dataset: Elemental and isotopic noble gas ratios and N2/Ar from the North Atlantic: model simulations
Data Citation:
Seltzer, A. M., Barry, P., Jenkins, W. J., Khatiwala, S., Nicholson, D. P., Smethie Jr., W. M., Stanley, R., Stute, M. (2023) Model simulations of elemental and isotopic heavy noble gas ratios using the Transport Matrix Method (TMM). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-02-21 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.890293.1 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
DOI:10.26008/1912/bco-dmo.890293.1
Project:
Principal Investigator:
Alan M. Seltzer (Woods Hole Oceanographic Institution, WHOI)
Co-Principal Investigator:
Peter Barry (Woods Hole Oceanographic Institution, WHOI)
William J. Jenkins (Woods Hole Oceanographic Institution, WHOI)
Samar Khatiwala (University of Oxford, Oxford)
David P. Nicholson (Woods Hole Oceanographic Institution, WHOI)
William M. Smethie Jr. (Lamont-Doherty Earth Observatory, LDEO)
Rachel Stanley (Wellesley College)
Martin Stute (Lamont-Doherty Earth Observatory, LDEO)
BCO-DMO Data Manager:
Shannon Rauch (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2023-02-21
Restricted:
No
Validated:
Yes
Current State:
Final no updates expected
Model simulations of elemental and isotopic heavy noble gas ratios using the Transport Matrix Method (TMM)
Abstract:
This dataset includes model simulations of the following tracers using the Transport Matrix Method (TMM): (i) new observations of heavy noble gas ratios (elemental and isotopic ratios) from the Bermuda Atlantic Time-series (BATS) on cruise 10391 (30 April 2022 - 05 May 2022), and (ii) measurements of Kr/Ar and N2/Ar ratios in stored dissolved gas samples collected in 1981 through the Transient Tracers in the Ocean (TTO) program. Together these measurements and model simulations provide insight into physical processes governing gas exchange in the high-latitude regions of North Atlantic Deep Water formation, and a comparison of physical simulations of N2/Ar ratios to observations in TTO samples reveals excess N2 that arises from benthic denitrification in the deep North Atlantic.