Characterizing Sierra Nevada Snowpack Using Variable-Resolution CESMSource: Journal of Applied Meteorology and Climatology:;2015:;volume( 055 ):;issue: 001::page 173DOI: 10.1175/JAMC-D-15-0156.1Publisher: American Meteorological Society
Abstract: he 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 technique?variable-resolution global climate modeling within the Community Earth System Model (VR-CESM)?at horizontal resolutions of 0.125° (14 km) and 0.25° (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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contributor author | Rhoades, Alan M. | |
contributor author | Huang, Xingying | |
contributor author | Ullrich, Paul A. | |
contributor author | Zarzycki, Colin M. | |
date accessioned | 2017-06-09T16:50:58Z | |
date available | 2017-06-09T16:50:58Z | |
date copyright | 2016/01/01 | |
date issued | 2015 | |
identifier issn | 1558-8424 | |
identifier other | ams-75240.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4217554 | |
description abstract | he 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 technique?variable-resolution global climate modeling within the Community Earth System Model (VR-CESM)?at horizontal resolutions of 0.125° (14 km) and 0.25° (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. | |
publisher | American Meteorological Society | |
title | Characterizing Sierra Nevada Snowpack Using Variable-Resolution CESM | |
type | Journal Paper | |
journal volume | 55 | |
journal issue | 1 | |
journal title | Journal of Applied Meteorology and Climatology | |
identifier doi | 10.1175/JAMC-D-15-0156.1 | |
journal fristpage | 173 | |
journal lastpage | 196 | |
tree | Journal of Applied Meteorology and Climatology:;2015:;volume( 055 ):;issue: 001 | |
contenttype | Fulltext |