OCTOBER 2017 C O R R I G E N D U M 3491 MOSTAFA MOMEN Department of Earth System Science, Stanford University, Stanford, California, and Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey ELIE BOU-ZEID Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey (Manuscript received 26 July 2017, in ﬁnal form 14 August 2017) In Momen and Bou-Zeid (2016, p. 30), the second term on the right-hand side of Eq. (10) has a sign error and must be corrected as follows: ›u › 0 0 52f (V 2 y)2 (u w ), c g ›t ›z ›y › 0 0 5 f (U 2 u)2 (y w ). c g ›t ›z Following this change, Eq. (11) also requires a modiﬁcation as › › ›u ›n ›u › u 0 0 2 (u w ) ’ n 5 1n 52a(z, t)u(z, t), T T ›z ›z ›z ›z ›z ›z ›n › › ›y ›y › y 0 0 2 (y w ) ’ n 5 1n 52a(z, t)y(z, t). T T 2 ›z ›z ›z ›z ›z ›z The two sign changes cancel out and the subsequent equations and results remain unchanged. REFERENCE Momen, M., and E. Bou-Zeid, 2016: Large-eddy simulations and damped-oscillator models of the unsteady Ekman boundary layer. J. Atmos. Sci., 73, 25–40, doi: 10.1175/JAS-D-15-0038.1. Corresponding author: Elie Bou-Zeid, firstname.lastname@example.org DOI: 10.1175/JAS-D-17-0209.1 2017 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www. ametsoc.org/PUBSReuseLicenses).
Journal of the Atmospheric Sciences – American Meteorological Society
Published: Oct 26, 2017
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