Geosci. Model Dev., 11, 3537–3556, 2018 https://doi.org/10.5194/gmd-11-3537-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. A global scavenging and circulation ocean model of thorium-230 and protactinium-231 with improved particle dynamics (NEMO–ProThorP 0.1) Marco van Hulten1,2, Jean-Claude Dutay1, and Matthieu Roy-Barman1 1Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France 2Geophysical Institute, University of Bergen, Bergen, Norway Correspondence: Marco van Hulten (
[email protected]) Received: 1 November 2017 – Discussion started: 8 December 2017 Revised: 16 August 2018 – Accepted: 20 August 2018 – Published: 31 August 2018 Abstract. In this paper we set forth a 3-D ocean model of the can be done based on our model as its source code is readily radioactive trace isotopes 230Th and 231Pa. The interest arises available. from the fact that these isotopes are extensively used for in- vestigating particle transport in the ocean and reconstructing past ocean circulation. The tracers are reversibly scavenged 1 Introduction by biogenic and lithogenic particles. Our simulations of 230Th and 231Pa are based on the Oceanic circulation and the carbon cycle play a major role NEMO–PISCES ocean biogeochemistry general circulation in the regulation of the past and present climate. Heat and model, which includes biogenic particles, namely small and carbon dioxide in the atmosphere tend to equilibrate with the big particulate organic carbon, calcium carbonate and bio- ocean surface and are transported down into the deep ocean genic silica.