nohrsc challenges of using snow data

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1 NOHRSC NOHRSC Challenges of using Snow Data Carrie Olheiser Office of Hydrologic Development National Weather Service, NOAA U.S. Department of Commerce National Operational Hydrologic Remote Sensing Center www.nohrsc.noaa.g ov

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NOHRSC Challenges of using Snow Data . Carrie Olheiser. National Operational Hydrologic Remote Sensing Center. Office of Hydrologic Development National Weather Service, NOAA U.S. Department of Commerce. www.nohrsc.noaa.gov. Snow Modeling and Data Assimilation. Snow Information Products. - PowerPoint PPT Presentation

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Page 1: NOHRSC  Challenges of using Snow Data

1NOHRSC

NOHRSC Challenges of using Snow Data Carrie Olheiser

Office of Hydrologic DevelopmentNational Weather Service, NOAAU.S. Department of Commerce

National Operational Hydrologic Remote Sensing Center

www.nohrsc.noaa.gov

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National Snow Analyses (NSA)

Ground

Airborne

Satellite

Multi-sensor Snow Observations

Data ProductsInteractive

MapsTime Series

PlotsText

Discussions

Snow Information Products

Snow Modeling and Data Assimilation

Numerical Weather

Prediction Model ForcingsGridded Snow

Characteristics

U.S.1-km2

Hourly

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• Nature of snow observations. Difficult to get “representative” observation.

• Metadata inconstancies between sources.• Data in proper SHEF format including time, amount and

duration.• Snowfall observations are not always published in a standard

format.• Timeliness of data• Reliably and timing of observations.• Adequate training in data collection.• Quality controlling the data, who is responsible?

Challenges of snow data

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• NOHRSC performs 4 automated tests – Reasonable Range– Spatial Consistency– Temporal Consistency– Internal Consistency

• Reasonable range is the only QC test Snowfall data undergoes.

Quality Controlling of Data

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Manual Quality Control Spatial Consistency

These points need to be looked at more closely, not spatially consistent

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Manual Quality Control Temporal Consistency

Bad Observation

Using data operationally does not allow us to see into the future for temporal quality control.

Unstable SNOTEL ObservationIn early season and late season

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Manual Quality Control Internal Consistency

• Density Check

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Station RepresentativenessPoint in Pixel

ESTES PARK RAWS

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Point in Pixel Consistency ? • Elevation

– Differences in station elevation and 1 km X1 km DEM elevation vary as much as 1500 meters, example station KRWW4, • DEM elevation = 1439• Reported elevation = 2910

• Forest Cover Density– Photos from the Northwest SNOTEL sites and

model forest cover density disconnects.– Example from Caribou Maine and station KCAR.

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Disconnects between ground survey coop results for the

March 1 to March 4 SurveyForest Density Issues and Stations not representative of the region.

• Caribou, ME• SWE reported March 1,

2004 is 0.038 meters.• KCAR is a Coop Station

located at the Airport in the large wind swept location that is well exposed with a forest density of ~ 6%.

• Caribou, ME SJ snow survey site .

• SWE reported March 1, 2004 is 0.104 meters.

• This station is reported by the USGS and measured at the medical clinic which is a more heavily wooded area.

Assimilation for the region used KCAR a regular reporter inthe season but turns out it was not representative of the region.This was not the only station with similar issues.

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72 hr Snowfall Observations

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• It was agreed at the NWS 2004 Cold Regions Hydrology Workshop (Kansas City, 2004 November 15-19) that the NOHRSC would develop web-based, real-time, automated, interactive, snowfall maps for the CONUS.

History of NOHRSC Snowfall Products

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National Metadata Sources Over 40 different sources of station metadata

Often redundant, often inconsistent!

NEED ONE-STOP SHOPPING FOR STATION METADATA

National Weather Service Databases

NWSLI, MADIS, CSSA (B44’s), NWS-ICAO, NWS-METAR, HADS, NCDC

NRCS SNOTEL and Snow CoursesUSACE New England District Snow SurveysNew York City Dept. Environmental ProtectionFederal Aviation Administration

California Department of Water ResourcesMaine Cooperative Snow SurveyMesoWest (150 + Smaller mesonets)RAWS Remote Automated Weather Stations

Federal and State Agencies

Weather Forecast Offices, River Forecast Centers and Regional Offices

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Importance of Accurate Metadata • Numerous databases leads to

uncertainties in the station metadata.

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Willow Creek, Wyoming

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99 Miles

Boulder Creek, Oregon

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72 hr SWE Observation

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Quality Control of Data• Internal Quality Control• Manual Quality Control• Point in Pixel Consistency

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Internal Quality Control• Behind the scenes 4 QC tests are run

– Reasonable Range– Spatial Consistency– Temporal Consistency– Internal Consistency

• Problems with losing to much data if we have strict requirements in an automated quality control scheme.

• The nature of snow variability makes qc difficult and as much data is needed as possible.

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• PRODUCTS• Hourly and Daily• 1 km2 Resolution

• INTERNET• Interactive Maps• 3D Visualization

• e.g. Google Earth• Time-series loops• National/Regional

Discussions• Text summaries by

watershed• Point Queries

• DIRECT FEED• Push or Pull• Gridded Data• Flat Binary or GIS-ready

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• It was agreed at the NWS 2004 Cold Regions Hydrology Workshop (Kansas City, 2004 November 15-19) that the NOHRSC would develop web-based, real-time, automated, interactive, snowfall maps for the CONUS.

History of NOHRSC Snowfall Products

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• NOHRSC has seven (7) new snowfall maps to the NOHRSC selection of Physical Elements on the NOHRSC Interactive Snow Information page.

• Daily total snowfall observations (for previous 24 hours) • 2-day total snowfall observations (for previous 48 hours) • 3-day total snowfall observations (for previous 72 hours) • Daily total snowfall interpolation (for previous 24 hours)• 2-day total snowfall interpolation (for previous 48 hours) • 3-day total snowfall interpolation (for previous 72 hours)• 24-hr Raw Snowfall – Only displays 24 hour totals

NOHRSC Snowfall Products

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Interpolated Snowfall 24 hrs

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• Are generated in automated process that uses snowfall data encoded in SHEF and MADIS formats received at the NOHRSC over AWIPS and MADIS Snow Collective.

• The NOHRSC performs only a “reasonable range” quality-control test on the snowfall data.

• Snowfall maps are generated using both– Temporal

• quantization and integration– spatial interpolation

• inverse distance weighting with a search radius of 75km.

NOHRSC Snowfall Products

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Total Observed Snowfall 24 Hrs

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Total Observed Snowfall 72 Hrs

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Total Observed Snowfall 72 Hrs

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Interpolated Snowfall 48 hrs

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Interpolated Snowfall 72 hrs

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Snowfall Text Products

Raw Data Available for Download

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Cumulative Snowfall Product

• Two stations located a couple kilometers apart. Both reporting snowfall, but MITM2 is reporting zero snowfall.

• Some station do not have a continuous record of snowfall, missing significant events. These products need to be used with a watchful eye!