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. Campbell , L. S. , W. J. Steenburgh , P. G. Veals , T. W. Letcher , and J. R. Minder , 2016 : Lake-effect precipitation enhancement over the Tug Hill Plateau during OWLeS IOP2b . Mon. Wea. Rev. , 144 , 1729 – 1748 , doi: 10.1175/MWR-D-15-0412.1 . Crewell , S. , K. Ebell , U. Löhnert , and D. Turner , 2009 : Can liquid water profiles be retrieved from passive microwave zenith observations? Geophys. Res. Lett. , 36 , L06803 , doi: 10.1029/2008GL036934 . Eichenlaub , V
. Campbell , L. S. , W. J. Steenburgh , P. G. Veals , T. W. Letcher , and J. R. Minder , 2016 : Lake-effect precipitation enhancement over the Tug Hill Plateau during OWLeS IOP2b . Mon. Wea. Rev. , 144 , 1729 – 1748 , doi: 10.1175/MWR-D-15-0412.1 . Crewell , S. , K. Ebell , U. Löhnert , and D. Turner , 2009 : Can liquid water profiles be retrieved from passive microwave zenith observations? Geophys. Res. Lett. , 36 , L06803 , doi: 10.1029/2008GL036934 . Eichenlaub , V
representation of the large-scale atmospheric flow conditions (e.g., Alcott and Steenburgh 2010 ; Kennedy et al. 2011 ; Walters et al. 2014 ). Snow depth and snowpack SWE analyses were obtained from the National Operational Hydrologic Remote Sensing Center (NOHRSC) Snow Data Assimilation System (SNODAS; National Operational Hydrologic Remote Sensing Center 2004 ). SNODAS uses RUC/RAP snowfall analysis data, ground observations, data from airborne platforms, and spaceborne microwave remote sensing to
representation of the large-scale atmospheric flow conditions (e.g., Alcott and Steenburgh 2010 ; Kennedy et al. 2011 ; Walters et al. 2014 ). Snow depth and snowpack SWE analyses were obtained from the National Operational Hydrologic Remote Sensing Center (NOHRSC) Snow Data Assimilation System (SNODAS; National Operational Hydrologic Remote Sensing Center 2004 ). SNODAS uses RUC/RAP snowfall analysis data, ground observations, data from airborne platforms, and spaceborne microwave remote sensing to
