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Mikael Sjöholm, Nikolas Angelou, Per Hansen, Kasper Hjorth Hansen, Torben Mikkelsen, Steinar Haga, Jon Arne Silgjerd, and Neil Starsmore

Ganti S. , 2012 : A technique to measure optical properties of brownout clouds for modeling terahertz propagation . Appl. Opt. , 51 , 3605 – 3613 . Gottschall, J. , Courtney M. S. , Wagner R. , Jorgensen H. E. , and Antoniou I. , 2012 : Lidar profilers in the context of wind energy—A verification procedure for traceable measurements. Wind Energy, 15, 147–159 , doi:10.1002/we.518 . Hogenboom, D. , and DiMarzio C. , 1998 : Quadrature detection of a Doppler signal . Appl. Opt

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C. R. Wood, R. D. Kouznetsov, R. Gierens, A. Nordbo, L. Järvi, M. A. Kallistratova, and J. Kukkonen

measurements . J. Appl. Meteor. , 28 , 99 – 106 . Grimmond, C. S. B. , and Oke T. , 1999 : Aerodynamic properties of urban areas derived from analysis of surface form . J. Appl. Meteor. , 38 , 1262 – 1292 . Hartogensis, O. K. , Watts C. J. , Rodriguez J.-C. , and de Bruin H. A. R. , 2003 : Derivation of an effective height for scintillometers: La Poza experiment in northwest Mexico . J. Hydrometeor. , 4 , 915 – 928 . Hill, R. J. , 1992 : Review of optical scintillation methods of

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Leslie M. Hartten and Paul E. Johnston

reflectivity, although their relative reflectivity is very good ( Gage et al. 2000 ). If an independent source of rain data is available, however, then a postdeployment calibration is possible. a. Calibrating the profiler An Optical Scientific, Inc., model ORG-815 optical rain gauge (see online at http://opticalscientific.com/pdf/brochures/ORG/ORG815DS130405.pdf ) was deployed on each cruise; data were postprocessed into 10-min rain rates. These can be used to calibrate the profiler, although ship

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