Fig. 6From: Surface wind mixing in the Regional Ocean Modeling System (ROMS)Potential temperature with depth during the simulations for the first Baltic Sea cruise (a–i) the observations. The simulations were done with (a–d) 50 levels and (e–h) 25 levels. The results from Nakanishi–Niino are given in (a, e), those from Mellor–Yamada 2.5 in (b, f), those from GLS in (c, g), and Large–McWilliams–Doney in (d, h)Back to article page