4.4 Article

Characterizing Sierra Nevada Snowpack Using Variable-Resolution CESM

Journal

JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
Volume 55, Issue 1, Pages 173-196

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JAMC-D-15-0156.1

Keywords

Climate models; Land surface model; Model evaluation; performance; Multigrid models

Funding

  1. National Science Foundation (NSF) via Climate Change, Water, and Society Integrated Graduate Education and Research Traineeship (IGERT) program at the University of California, Davis (NSF) [1069333]
  2. Leland Roy Saxon and Georgia Wood Saxon Fellowship
  3. U.S. Department of Energy Office of Science project Multiscale Methods for Accurate, Efficient, and Scale-Aware Models of the Earth System

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The location, timing, and intermittency of precipitation in California make the state integrally reliant on winter-season snowpack accumulation to maintain its economic and agricultural livelihood. Of particular concern is that winter-season snowpack has shown a net decline across the western United States over the past 50 years, resulting in major uncertainty in water-resource management heading into the next century. Cutting-edge tools are available to help navigate and preemptively plan for these uncertainties. This paper uses a next-generation modeling techniquevariable-resolution global climate modeling within the Community Earth System Model (VR-CESM)at horizontal resolutions of 0.125 degrees (14 km) and 0.25 degrees (28 km). VR-CESM provides the means to include dynamically large-scale atmosphere-ocean drivers, to limit model bias, and to provide more accurate representations of regional topography while doing so in a more computationally efficient manner than can be achieved with conventional general circulation models. This paper validates VR-CESM at climatological and seasonal time scales for Sierra Nevada snowpack metrics by comparing them with the Daymet, Cal-Adapt, NARR, NCEP, and North American Land Data Assimilation System (NLDAS) reanalysis datasets, the MODIS remote sensing dataset, the SNOTEL observational dataset, a standard-practice global climate model (CESM), and a regional climate model (WRF Model) dataset. Overall, given California's complex terrain and intermittent precipitation and that both of the VR-CESM simulations were only constrained by prescribed sea surface temperatures and data on sea ice extent, a 0.68 centered Pearson product-moment correlation, a negative mean SWE bias of <7 mm, an interquartile range well within the values exhibited in the reanalysis datasets, and a mean December-February extent of snow cover that is within 7% of the expected MODIS value together make apparent the efficacy of the VR-CESM framework.

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