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. L. , 1994 : Multiscale four-dimensional data assimilation. J. Appl. Meteor. , 33 , 416 – 434 . 10.1175/1520-0450(1994)033<0416:MFDDA>2.0.CO;2 Steppeler, J. , and Coauthors , 2006 : Prediction of clouds and rain using a z -coordinate nonhydrostatic model. Mon. Wea. Rev. , 134 , 3625 – 3643 . 10.1175/MWR3331.1 Trier, S. , Chen F. , and Manning K. , 2004 : A study of convection initiation in a mesoscale model using high-resolution land surface initial conditions. Mon. Wea
. L. , 1994 : Multiscale four-dimensional data assimilation. J. Appl. Meteor. , 33 , 416 – 434 . 10.1175/1520-0450(1994)033<0416:MFDDA>2.0.CO;2 Steppeler, J. , and Coauthors , 2006 : Prediction of clouds and rain using a z -coordinate nonhydrostatic model. Mon. Wea. Rev. , 134 , 3625 – 3643 . 10.1175/MWR3331.1 Trier, S. , Chen F. , and Manning K. , 2004 : A study of convection initiation in a mesoscale model using high-resolution land surface initial conditions. Mon. Wea
1. Introduction Measuring and modeling of the boundary layer is challenging, especially for the nighttime stable boundary layer (SBL). In particular, high-quality in situ measurements of profiles of mean and turbulent statistics of the nighttime SBL are logistically difficult using instrumented towers or instrumented research aircraft ( Tjernström 1993 ). A suite of fast response turbulence sensors attached to a tethered system can operate effectively under these nighttime conditions. The
1. Introduction Measuring and modeling of the boundary layer is challenging, especially for the nighttime stable boundary layer (SBL). In particular, high-quality in situ measurements of profiles of mean and turbulent statistics of the nighttime SBL are logistically difficult using instrumented towers or instrumented research aircraft ( Tjernström 1993 ). A suite of fast response turbulence sensors attached to a tethered system can operate effectively under these nighttime conditions. The
