DEVELOPMENT OF THE ISOTOPE VERSION OF THE FULLY COUPLED CLIMATE MODEL MIROC6-ISO
Author:
Affiliation:
1. Institute of Industrial Science, The University of Tokyo
2. Graduate School of Frontier Sciences, The University of Tokyo
3. Hirosaki University, Hirosaki
Publisher
Japan Society of Civil Engineers
Link
https://www.jstage.jst.go.jp/article/journalofjsce/12/2/12_23-16035/_pdf
Reference19 articles.
1. 1) Craig, H. and Gordon, L. I. : Deuterium and oxygen 18 variations in the ocean and the marine atmosphere, in: Stable Isotopes in Oceanographic Studies and Paleotemperatures, edited by: Tongiogi, E., 9–130, Consiglio nazionale delle richerche, Laboratorio de geologia nucleare, Spoleto, Italy, 1965.
2. 2) Craig, H. : Standard for reporting concentrations of deuterium and oxygen-18 in natural waters, Science, No. 133(3467), pp. 1833-1834, 1961.
3. 3) Guillot, D., Rajaratnam, B., Emile-Geay, J. : Statistical paleoclimate reconstructions via Markov random fields, Ann Appl Stat., No. 9(1), pp. 324-352, 2015.
4. 4) Kageyama, M., Braconnot, P., Harrison, S. P., et al. : The PMIP4 contribution to CMIP6–Part 1: Overview and overarching analysis plan, Geosci. Model Dev., No. 11(3), pp. 1033-1057, 2018.
5. 5) Hu, J., Emile‐Geay, J., Nusbaumer, J., et al. : Impact of Convective Activity on Precipitation δ18O in Isotope‐ Enabled General Circulation Models, J. Geophys. Res. Atmos, No. 123(23), pp. 13, 595-13, 610, 2018.
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