HR: 0830h
AN: C41B-0949 INVITED     [PDF]
TI: Methods to Identify and Correct Snow Water Equivalent Pressure Sensor Measurement Errors to Improve Estimates of Water Stored as Snow
AU: * Johnson, J B
EM: Jerome.B.Johnson@erdc.usace.army.mil
AF: USA ERDC-CRREL, P.O. Box 35170, Fairbanks, AK 99703 United States
AU: Marks, D
EM: danny@nwrc.ars.usda.gov
AF: USDA ARS, 800 Park Blvd. Plaza Suite 105, Boise, ID 80526 United States
AB: Snow water equivalent (SWE) pressure sensor measurement errors significantly reduce the ability of water resource managers to accurately predict the amount of available SWE or snowmelt water runoff. SWE errors may occur when the snow/soil interface is at the melting temperature and the differential snowmelt rate between a SWE sensor and the soil exceeds the snow creep rate. A cold, dry snow cover overlying frozen soil will not exhibit SWE sensor errors because the snow and soil temperatures are both below the melting temperature. A delayed SWE sensor response may occur when the SWE accumulation rate exceeds the snow creep rate. Cold snow covers with many ice layers will have a relatively low creep rate while isothermal wet snow will have a relatively high creep rate. This is why a SWE sensor that exhibits a large error just before the onset of wet isothermal conditions will suddenly start to accurately measure SWE. By understanding the physical mechanisms that affect SWE sensor performance the occurrence of SWE errors can be identified and a variety of approaches to correcting them are possible. When only SWE sensor data are available, the occurrence of SWE errors can be identified by excursions in SWE, which can be corrected by interpolating from data on either side of the excursion. A delayed SWE sensor response to a snowstorm is related to the snow creep rate and can be corrected by shifting the SWE record to ensure that the start of the SWE increase and the storm agree. The SWE accumulation rate midway between the beginning and end of the storm should provide a good approximation of the storm's accumulation rate. When additional information on precipitation, snow depth, and snow core SWE are available then relatively simple comparison and interpolation methods can be used to correct errors. Ground temperature or heat flux data can be used to predict SWE sensor performance and correct SWE errors. Air temperature data and a heat flux model of snow and soil may be used to estimate data needed to correct SWE errors.
DE: 1860 Runoff and streamflow
DE: 1863 Snow and ice (1827)
DE: 1884 Water supply
DE: 1894 Instruments and techniques
SC: Cryosphere [C]
MN: 2003 Fall Meeting