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Addressing Bias in Snow Water Equivalent Measurement Methods

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Presentation on theme: "Addressing Bias in Snow Water Equivalent Measurement Methods"— Presentation transcript:

1 Addressing Bias in Snow Water Equivalent Measurement Methods
Jordan French Special Acknowledgments to: Dr. Jeff Snider, UW Atmospheric Science, WyCEHG, NSF, and Snowmetrix

2 What is the significance of snow?
Largest precipitation type in northwestern US

3 Snowfall Measurement Methods
Snotel Hotplate snow gauge Manual “snowboard” method Scales

4 Project in upstate NY Lake snow effects Discrepancy between methods

5 Hypotheses The scale measurement of weight (precision ± 0.3 %) agrees with the value of a standard weight - within measurement error - and this agreement is apparent regardless of temperature. The manual method measurement of SWE compares well with the hotplate measurement of SWE. Objective: Improved confidence in snowfall measurements is expected to result from this research

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7 Weighing Precision Mean: 𝑥 𝑝 = 1 𝑁 𝑁=1 10 𝑥 𝑖
𝑥 𝑝 = 1 𝑁 𝑁=1 10 𝑥 𝑖 where 𝑥 𝑖 =𝑚𝑒𝑎𝑠𝑢𝑟𝑒𝑚𝑒𝑛𝑡 𝑜𝑓 𝑤𝑒𝑖𝑔ℎ𝑡 Standard Deviation: 𝑥 𝐴 = 1 𝑁 𝑁=1 10 (𝑥 𝑖 − 𝑥 0 ) Relative Precision: 𝜎 𝑃 𝑥

8 Scale Scale 2

9 Scale 3

10 Weighing Accuracy Average departure from reference:
𝑥 𝐴 = 1 𝑁 𝑁=1 10 (𝑥 𝑖 − 𝑥 0 ) Standard Deviation of departure: 𝜎 𝐴 = 1 𝑁−1 𝑁=1 10 ( 𝑥 𝑖 − 𝑥 0 ) 2 where 𝑥 0 =𝑟𝑒𝑓𝑒𝑟𝑒𝑛𝑐𝑒 𝑚𝑎𝑠𝑠

11 Scale Scale 2

12 Scale 3

13 Snowfall Measurements in the Snowy Range

14 Snow Water Equivalent Measurement
Procedure Single snow event Extract snow core with tube Determine weight of snow 𝑆𝑊𝐸= 𝑚 𝑠𝑛𝑜𝑤 𝜌 𝐻 2 𝑂 ∗( 1 𝐴 ) 𝜌= 𝑆𝑊𝐸 𝑑 ∗( 𝜌 𝐻 2 𝑂 )

15 Snowboard Method Results
Tube 1 Tube 2 Tube 3 Snow Depth (mm) 20 SWE (mm) 0.448 0.442 1.329 ρ (kg/m^3) 22.384 22.090 66.452

16 Conclusion More fieldwork to be done


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