Our Skill in Modeling Mountain Rain and Snow is Bypassing the Skill of Our Observational Networks
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- Jessica Lundquist
- Civil and Environmental Engineering, University of Washington, Seattle, Washington
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- Mimi Rose Abel
- NOAA/Earth Sciences Research Laboratory/Physical Sciences Division, Boulder, Colorado
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- Ethan Gutmann
- National Center for Atmospheric Research, Boulder, Colorado
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- Sarah Kapnick
- NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey
書誌事項
- 公開日
- 2019-12
- DOI
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- 10.1175/bams-d-19-0001.1
- 公開者
- American Meteorological Society
この論文をさがす
説明
<jats:title>Abstract</jats:title> <jats:p>In mountain terrain, well-configured high-resolution atmospheric models are able to simulate total annual rain and snowfall better than spatial estimates derived from in situ observational networks of precipitation gauges, and significantly better than radar or satellite-derived estimates. This conclusion is primarily based on comparisons with streamflow and snow in basins across the western United States and in Iceland, Europe, and Asia. Even though they outperform gridded datasets based on gauge networks, atmospheric models still disagree with each other on annual average precipitation and often disagree more on their representation of individual storms. Research to address these difficulties must make use of a wide range of observations (snow, streamflow, ecology, radar, satellite) and bring together scientists from different disciplines and a wide range of communities.</jats:p>
収録刊行物
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- Bulletin of the American Meteorological Society
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Bulletin of the American Meteorological Society 100 (12), 2473-2490, 2019-12
American Meteorological Society