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Here, we develop a novel large\u2010eddy simulation model setup to enable the modeling of the very SBL, avoiding the use of the Monin\u2013Obukhov similarity theory at its lower boundary condition, as it breaks down in these conditions in agreement with previous studies. The new approach requires very fine grids in the vertical direction, in the order of a few centimeters. A series of Ekman\u2010layer\u2010type boundary layers under weak\u2010wind conditions ( and 2\u2009ms), and strong surface cooling rates (1 and 3\u2009Khr) at high latitude is studied using isotropic grids of 0.05 and 0.10\u2009m resolution. The low\u2010order statistics show some sensitivity to the grid resolution; for example, both the SBL height and the low\u2010level jet position decrease with increasing grid resolution. In general, some differences are spotted regarding the shape of the wind speed and temperature vertical profiles, compared with weakly to moderately stratified conditions, suggesting that the structure and characteristics of the SBL evolve with increasing stratification. Moreover, the wind turning is significant from the surface, where the surface wind angle relative to the geostrophic wind is about 50. Lastly, two regimes within very stable conditions can be qualitatively identified primarily based on the gradient Richardson number () profiles: In the less stable regime,  increases almost linearly with height and a quasi\u2010steady state is achieved; however, in the most stable regime,  sharply increases near the surface and remains constant throughout the SBL while increasing with time up to . Thus, a quasi\u2010steady state is not achieved; and although turbulence does not collapse, it remains weak.<\/jats:p>","DOI":"10.1002\/qj.4279","type":"journal-article","created":{"date-parts":[[2022,4,5]],"date-time":"2022-04-05T09:09:06Z","timestamp":1649149746000},"page":"1805-1823","update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":10,"title":["Large\u2010eddy simulation of very stable boundary layers. 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