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The 9th International Workshop on Modeling the Ocean (IWMO 2017) was held in the modern campus of Yonsei University, Seoul, Korea, from July 3–6 2017. The workshop was attended by about 80 participants from countries all around the world, many of whom were young and earliercareer scientists: students and postdocs. Papers were presented covering a broad range of topics on field observations, analyses, and modeling: wave and air-sea interaction dynamics, climate variability, basin-scale processes and coastal oceanography, sea-ice dynamics, sediment transport, tropical cyclones, biogeochemical-physical coupling, boundary currents, sea-level rise, extreme events, ocean prediction and others. We were pleased to witness very high-quality research and presentations, many from young students and scientists. Thirty three (33) young scholars participated in the Outstanding Young Scientist Award (OYSA) competition; congratulations to all of them! The finalists of the IWMO-2017 OYSAwere: R. Olson (Yonsei University, Korea), Y. Ushijima (Kyoto University, Japan), Y. Choi (Yonsei University, Korea), and Y. J. Tak (Seoul National University, Korea). The 8 papers in this Topical Collection were selected from a total of about 30 submitted papers after they underwent the usual process of reviews and revisions. There were at least 2 reviewers for each paper. The reviews were solicited from both the workshop attendees and the scientific community at large. Below are short summaries of the papers in the topical collection (alphabetically ordered). Berntsen et al. (2018) conducted high-resolution model experiments of dense water cascading down a continental slope, focusing on bottom boundary layer dynamics. The authors used a terrain-following model and found that with quadratic drag law and bottom drag coefficient calculated to fit the logarithmic law of the wall, the model could efficiently simulate bottom Ekman layer dynamics in good agreements with very fine-grid modeling using the no-slip bottom boundary condition. Hong et al. (2018) applied a current and wave coupled model to conduct model sensitivity, with and without coupling, in predicting waves and surges induced by Typhoon Bolaven (2012) that made landfall upon the Korean Peninsula. With coupling, ocean currents reduced significantly the wave height on the right-hand side of the advancing storm, improving the peak height and timing compared with the uncoupled simulation. Surge peak was improved using a wind stress formula that incorporated the storm-induced wave height. Kim et al. (2018) conducted idealized experiments to study the role of cold-water formation and planetary vorticity gradient (β effects) in the generation of the East Korea warm current—a western boundary current—in the East/Japan Sea. Cold water was shown to control the strength of the East Korea warm current, followed by the β effects, consistent with observations. Rusdiansyah et al. (2018) applied a finite-volume unstructured grid numerical model at high resolution (horizontal grid ~ 25 m) to assess the potential impacts of the construction of a “giant sea wall” on the three-dimensional circulation of Jakarta Bay, Indonesia. They demonstrated the feasibility of Responsible Editor: Jörg-Olaf Wolff

The 9th International Workshop on Modeling the Ocean (IWMO 2017) in Seoul, Korea, July 3–6, 2017