Development of a Quality Controlled Snowstorm Database · • Presented in GIS – Inclusion of...
Transcript of Development of a Quality Controlled Snowstorm Database · • Presented in GIS – Inclusion of...
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Development of a Quality Controlled Snowstorm
DatabaseAnna Wilson
Faculty/NCDC Advisor: Mike Squires
April 2009
Outline
• Background• NESIS, RESIS, the Snowstorm Database
• QC Procedures• Delineate storm, create grid, manual check
• Future Work• Uses for the public, database expansion
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Northeast Snowfall Impact Scale
• NCDC began calculating this index in the 2005-2006 season
• Uses data east of the Rocky Mountains to evaluate Northeast snowstorms
• Constants in the NESIS algorithm are determined by top 30 Northeast storms – Snowfall area, snowfall amount, population
density
Regional Snowfall Impact Scale
• Based on NCDC climate regions for easy integration with other products
• Expressed in percentiles to facilitate historical comparison
• Algorithm is currently in development
• National snowfall index will be computed as well as a separate index for each region
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Snowstorm Database
• Comprised of top 100 storms since 1900
• Used to calculate national index
• Presented in GIS – Inclusion of other information will assist users in
assessment of societal impacts• Hospitals, schools, transportation networks
Data Source
• Automated QC done on databases
• Used newest, “best” data: GHCN-D
• Snowstorm is put in a GIS environment
• Zero values are discarded– Eliminates part of one problem – zero values that
should be reported as missing
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QC Step 1: Delineate the storm.
January 13-16, 1918
QC Step 1: Delineate the storm.
January 12-15, 1982
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Day 1: January 12, 1982
Day 2: January 13, 1982
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Day 3: January 14, 1982
Day 4: January 15, 1982
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QC Step 2: Run Script
• Flags suspiciously different points using Moran’s I statistic
• Removes values of less than 6 inches if any dates have missing values
• Creates grid using an inverse distance weighted technique
QC Step 3
• Manually check the data– Expect basic spatial continuity
– Variation can result from….
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Variation in TopographyJanuary 11-14, 1964
Lake Effect SnowJanuary 6-9, 1988
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Different Observing TechniquesJanuary 6-9, 1996
Temperature VariationDecember 10-13, 1992
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Quality Control Goals
• Use consistent, repeatable procedures so that different analysts get the same results
• Type I or Type II error – Choose to keep points if it is not absolutely clear
they are incorrect
• Questions– Should a zero value actually be reported as
missing?
– Is there an order of magnitude error?
January 15-17, 1945
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January 12-15, 1979
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Conclusions and Future Work
• Rigorous, robust QC important for accuracy– ~1.3% of data taken out per storm
• Range: 0.61% - 3.19%
• Snowstorm database will have widespread applications– Expansion to include other parts of the country
– Assist in development of regional/national indices
– User input will determine new information to include in the GIS interface
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References
• Doesken, N.J., and A. Judson, 1996: The Snow Booklet: A Guide to the Science, Climatology and Measurement of Snow in the United States. Colorado State University, 85 pp.
• Kocin, P.J. and L.W. Uccellini, 2004: A Snowfall Impact Scale Derived From Northeast Storm Snowfall Distributions. Bull. Amer. Meteor. Soc., 85, 177-194
• Kocin, P.J. and L.W. Uccellini. Northeast Snowstorms, vol. 1 and 2. Boston: American Meteorological Society, 2004.
• Squires, M.F. and J.H. Lawrimore, 2006: Development of an Operational Snowfall Impact Scale. 22nd IIPS, Atlanta, GA.
• Squires, M.F., J.H. Lawrimore, et. al., 2008: Development of Operational Regional Snowfall Indices. 24th IIPS, (Atlanta GA?)