Editorial Type:
Article
Article Type:
Research Article

Downscaling and Bias Correcting a Cold Season Precipitation Climatology over Coastal Southern British Columbia Using the Regional Atmospheric Modeling System (RAMS)

B. Ainslie University of Northern British Columbia, Prince George, British Columbia, Canada

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P. L. Jackson University of Northern British Columbia, Prince George, British Columbia, Canada

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Print Publication:
01 May 2010
DOI:
https://doi.org/10.1175/2010JAMC2315.1
Page(s):
937–953
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Abstract

Thirty years of the North American Regional Reanalysis (NARR) are dynamically downscaled to an 8-km grid spacing using the Regional Atmospheric Modeling System (RAMS) to generate a climatology of glacier winter accumulation over the southern Coast Mountains in British Columbia (BC), Canada. RAMS precipitation fields are bias corrected using observations from Environment Canada (EC) synoptic and climate stations and BC provincial snow pillow stations. Raw and bias-corrected model output is compared with observations from EC Reference Climate Network stations, BC provincial Ministry of Transportation and Highways stations, BC Hydro stations, snow course data, and glacier mass balance studies. A water balance is also applied to 12 drainage basins located within the modeling domain to test the consistency of both the raw and bias-corrected precipitation fields with observed streamflow. Model output is compared with the Parameter-Elevation Regressions on Independent Slopes Model (PRISM) and bias-corrected NARR. Isotropic spectral power densities are examined to compare the effective spatial resolution of the various precipitation fields. The spatial distribution of the bias-correction field suggests that RAMS underpredicts precipitation on the western edge of Vancouver Island, Canada, and overpredicts along the southern Coast Mountains. The bias correction helps close the water balance budgets in all basins except the Somass on Vancouver Island. The bias correction generally improves the agreement between RAMS and observed snow water equivalent amounts at the glacier and snow course sites, and observed precipitation amounts at the synoptic, climate, and snow pillow stations. The RAMS and NARR isotropic spectral power densities show a loss of variability at approximately 45 and 63 km, while PRISM shows little falloff down to 16 km.

Corresponding author address: B. Ainslie, Environmental Science and Engineering Program, University of Northern British Columbia, Prince George BC V2N 4Z9, Canada. Email: ainslie@unbc.ca

Abstract

Thirty years of the North American Regional Reanalysis (NARR) are dynamically downscaled to an 8-km grid spacing using the Regional Atmospheric Modeling System (RAMS) to generate a climatology of glacier winter accumulation over the southern Coast Mountains in British Columbia (BC), Canada. RAMS precipitation fields are bias corrected using observations from Environment Canada (EC) synoptic and climate stations and BC provincial snow pillow stations. Raw and bias-corrected model output is compared with observations from EC Reference Climate Network stations, BC provincial Ministry of Transportation and Highways stations, BC Hydro stations, snow course data, and glacier mass balance studies. A water balance is also applied to 12 drainage basins located within the modeling domain to test the consistency of both the raw and bias-corrected precipitation fields with observed streamflow. Model output is compared with the Parameter-Elevation Regressions on Independent Slopes Model (PRISM) and bias-corrected NARR. Isotropic spectral power densities are examined to compare the effective spatial resolution of the various precipitation fields. The spatial distribution of the bias-correction field suggests that RAMS underpredicts precipitation on the western edge of Vancouver Island, Canada, and overpredicts along the southern Coast Mountains. The bias correction helps close the water balance budgets in all basins except the Somass on Vancouver Island. The bias correction generally improves the agreement between RAMS and observed snow water equivalent amounts at the glacier and snow course sites, and observed precipitation amounts at the synoptic, climate, and snow pillow stations. The RAMS and NARR isotropic spectral power densities show a loss of variability at approximately 45 and 63 km, while PRISM shows little falloff down to 16 km.

Corresponding author address: B. Ainslie, Environmental Science and Engineering Program, University of Northern British Columbia, Prince George BC V2N 4Z9, Canada. Email: ainslie@unbc.ca

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