JANUARY 2018 C O R R I G E N D U M 267 MELISSA L. WRZESIEN AND MICHAEL T. DURAND School of Earth Sciences, and Byrd Polar and Climate Research Center, The Ohio State University, Columbus, Ohio TAMLIN M. PAVELSKY Department of Geological Sciences, University of North Carolina, Chapel Hill, North Carolina IAN M. HOWAT School of Earth Sciences, and Byrd Polar and Climate Research Center, The Ohio State University, Columbus, Ohio STEVEN A. MARGULIS AND LAURIE S. HUNING Department of Civil and Environmental Engineering, University of California, Los Angeles, Los Angeles, California (Manuscript received and in ﬁnal form 12 September 2017) Because of an incorrect assumption about the spatial resolution of the National Weather Service’s Snow Data Assimilation System (SNODAS), the authors have identiﬁed an im- portant error in our recent paper comparing various estimates of SWE in the Sierra Nevada (Wrzesien et al. 2017). The assumed SNODAS spatial resolution of 1 km (gridcell area of 1km ) should have been 30 arc s. At the latitudes where SNODAS is available, this as- sumption leads to gridcell areas considerably smaller than 1 km (Fig. 1). Though Carroll et al. (2001) and much of the literature erroneously identify
Journal of Hydrometeorology – American Meteorological Society
Published: Jan 12, 2018
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