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H. J. S. Fernando, E. R. Pardyjak, S. Di Sabatino, F. K. Chow, S. F. J. De Wekker, S. W. Hoch, J. Hacker, J. C. Pace, T. Pratt, Z. Pu, W. J. Steenburgh, C. D. Whiteman, Y. Wang, D. Zajic, B. Balsley, R. Dimitrova, G. D. Emmitt, C. W. Higgins, J. C. R. Hunt, J. C. Knievel, D. Lawrence, Y. Liu, D. F. Nadeau, E. Kit, B. W. Blomquist, P. Conry, R. S. Coppersmith, E. Creegan, M. Felton, A. Grachev, N. Gunawardena, C. Hang, C. M. Hocut, G. Huynh, M. E. Jeglum, D. Jensen, V. Kulandaivelu, M. Lehner, L. S. Leo, D. Liberzon, J. D. Massey, K. McEnerney, S. Pal, T. Price, M. Sghiatti, Z. Silver, M. Thompson, H. Zhang, and T. Zsedrovits

: Daytime boundary-layer evolution over mountainous terrain. Part I: Observations of the dry circulations . Mon. Wea. Rev. , 112 , 340 – 356 , doi: 10.1175/1520-0493(1984)112<0340:DBLEOM>2.0.CO;2 . Banta , R. M. , Y. L. Pichugina , N. D. Kelley , R. M. Hardesty , and W. A. Brewer , 2013 : Wind energy meteorology: Insight into wind properties in the turbine-rotor layer of the atmosphere from high-resolution Doppler lidar . Bull. Amer. Meteor. Soc ., 94 , 883 – 902 , doi: 10.1175/BAMS

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Manuela Lehner, C. David Whiteman, Sebastian W. Hoch, Derek Jensen, Eric R. Pardyjak, Laura S. Leo, Silvana Di Sabatino, and Harindra J. S. Fernando

temperature deficit in the slope-inversion layer, θ 0 is a reference potential temperature above the inversion, and α is the slope angle. Using typical values for the east slope of Granite Mountain during the period between 1900 and 2200 MST [ d j = 30 m, h c = 0.3 m, = −0.05 m 2 s −2 , α = 2.5°, and Δ θ max / θ 0 = 0.03], the above expression results in a jet maximum height of 4.5 m, which is in good agreement with the observations. Fig . 14. Radial wind velocities from lidar scans up the

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