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Matthew E. Jeglum, Sebastian W. Hoch, Derek D. Jensen, Reneta Dimitrova, and Zachariah Silver

zone 12T) of the study area at DPG with the southern part of Granite Mountain detailed in the inset. The color-coded circles indicate the daily frequency of LTFs at various sites at DPG. Elevation contours are 80 m in the main plot and 30 m in the inset, with the 1315-m contour annotated in both. The transect in the inset marked L1–L4 is the primary slope transect in this study. The location of the flux tower ES2 and the Granite Ridge and West slope sites are annotated in the inset. An extensive

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Jeffrey D. Massey, W. James Steenburgh, Sebastian W. Hoch, and Jason C. Knievel

.1175/1520-0493(2002)130<0921:MFDBLC>2.0.CO;2 . Rife , D. L. , C. A. Davis , Y. Liu , and T. T. Warner , 2004 : Predictability of low-level winds by mesoscale meteorological models . Mon. Wea. Rev. , 132 , 2553 – 2569 , doi: 10.1175/MWR2801.1 . Robock , A. , and Coauthors , 2003 : Validation of North American Land Data Assimilation Systems retrospective forcing over the southern Great Plains . J. Geophys. Res. , 108 , 8846, doi: 10.1029/2002JD003245 . Schaefer , G. L. , M. H. Cosh , and T. J. Jackson

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