14 citations as recorded by crossref.

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2. A Three-Dimensional Model of the Marine Nitrogen Cycle during the Last Glacial Maximum Constrained by Sedimentary Isotopes C. Somes et al. 10.3389/fmars.2017.00108
3. Glacial Ice Sheet Extent Effects on Modeled Tidal Mixing and the Global Overturning Circulation S. Wilmes et al. 10.1029/2019PA003644
4. Climate Process Team on Internal Wave–Driven Ocean Mixing J. MacKinnon et al. 10.1175/BAMS-D-16-0030.1
5. Internal Tides Drive Nutrient Fluxes Into the Deep Chlorophyll Maximum Over Mid‐ocean Ridges R. Tuerena et al. 10.1029/2019GB006214
6. Coupling of oceanic carbon and nitrogen facilitates spatially resolved quantitative reconstruction of nitrate inventories N. Glock et al. 10.1038/s41467-018-03647-5
7. The K 1 internal tide simulated by a 1/10° OGCM Z. Li et al. 10.1016/j.ocemod.2017.04.002
8. The use of tidally induced vertical-mixing schemes in simulating the Pacific deep-ocean state S. Osafune et al. 10.1007/s10872-021-00591-9
9. Overlooked Role of Mesoscale Winds in Powering Ocean Diapycnal Mixing Z. Jing et al. 10.1038/srep37180
10. Community Integrated Earth System Model (CIESM): Description and Evaluation Y. Lin et al. 10.1029/2019MS002036
11. Glacial Atlantic overturning increased by wind stress in climate models J. Muglia & A. Schmittner 10.1002/2015GL064583
12. Glacial ocean overturning intensified by tidal mixing in a global circulation model A. Schmittner et al. 10.1002/2015GL063561
13. Combined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial Ocean J. Muglia et al. 10.1002/2016PA003077
14. Weak overturning circulation and high Southern Ocean nutrient utilization maximized glacial ocean carbon J. Muglia et al. 10.1016/j.epsl.2018.05.038