Index of /arm-iop-file/2022/guc/sail/beutler-stakes

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SAIL Storm Boards 2022-2023

Overview:

“Storm Boards” are simple installations comprised of a horizontal white plastic board that is placed in situ on the surface of the snowpack with a 1 m vertical marker pole for identifying the board center and approximate new snow height. Storm boards allow newly fallen snow to accumulate on them while staying separated from moisture and energy exchange with the snowpack, thus creating a discrete sample of newly fallen snow depth & SWE (snow water equivalent) that can be measured to calculate the net moisture input of individual or multiple storm events to the seasonal snowpack.

Samples are measured with a 2” diameter plastic tube that allows the observer to non destructively take a snow core of the newly deposited snow; this core is weighed with a small hand scale - then the mass of the sample is converted to SWE. Depth of the snow sample is obtained with a snow depth probe or from graduated marks on the plastic tube. 3 or more replicate samples are taken for each board measurement and averaged. Total snow height (HS) of the snowpack is measured with a snow depth probe for each site & timepoint to track snowpack accumulation/ablation.

Metadata Creator:
Name: Curtis Beutler
Email: cbeutler@lbl.gov Phone:
Street: 1 Cyclotron Road City: Berkeley
State: CA Postal: 94720
Contact Info:
Name: Curtis Beutler
Email: cbeutler@lbl.gov Phone:
Street: 1 Cyclotron Road City: Berkeley
State: CA Postal: 94720
Investigator(s): Curtis Beutler (cbeutler@lbl.gov) 0000-0003-0740-3112
Alex Newman (alexnewman760@gmail.com) 0000-0002-1574-8754
Data Citation:https://doi.org/10.5439/2319185
Data Format:csv
Abstract:

“Storm Boards” are simple installations comprised of a horizontal white plastic board that is placed in situ on the surface of the snowpack with a 1 m vertical marker pole for identifying the board center and approximate new snow height. Storm boards allow newly fallen snow to accumulate on them while staying separated from moisture and energy exchange with the snowpack, thus creating a discrete sample of newly fallen snow depth & SWE (snow water equivalent) that can be measured to calculate the net moisture input of individual or multiple storm events to the seasonal snowpack.

Samples are measured with a 2” diameter plastic tube that allows the observer to non destructively take a snow core of the newly deposited snow; this core is weighed with a small hand scale - then the mass of the sample is converted to SWE. Depth of the snow sample is obtained with a snow depth probe or from graduated marks on the plastic tube. 3 or more replicate samples are taken for each board measurement and averaged. Total snow height (HS) of the snowpack is measured with a snow depth probe for each site & timepoint to track snowpack accumulation/ablation.

Purpose:

This dataset was collected for the purpose of quantifying the snowpack snow water equivalent (SWE) input of individual storm events and/or time periods; height and mass calculations also allow the calculation of new snow density (m/v) although the height (and therefore volume) of newly fallen snow can change quickly after deposition due to the thermodynamic properties of recently deposited snow crystals.  This dataset provides fundamental validation of the total SWE of frozen precipitation that occurred during storms at SAIL.  Therefore, this dataset will validate SAIL's Surface Quantitative Precipitation Estimate (SQUIRE) product.

Data Usage:Please use this data to assess the net SWE inputs of winter weather events, all sites were collocated with meteorological stations to quantify the weather conditions for each precipitation event.
Data Credit:Watershed Function Scientific Focus Area, Rocky Mountain Biological Laboratory, Daniel Feldman
Arm Sites: guc
Other Sites:
SitesNorthWestSouthEast
X1: External Data (satellites and others)0000
Content Time Range: Begin: 2022-02-23 End: 2023-04-27
Instrument(s):Storm Boards
Data Type:Surface Atmosphere Integrated Field Laboratory (SAIL)
Scientific Measurements(s):
Measurement nameVariables
Depth of new snow
Snow water equivalent of new snow
Total height of snow on ground
Stratum Keyword(s):
Precipitation, Snowpack, Hydrology, Mountain Meteorology
Data Quality:
Attribute Accuracy: No formal uncertainty assessments were conducted and no estimates of uncertainty are reported.
Positional Accuracy: Horizontal Accuracy: 1m Vertical Accuracy: 2-3m (due to depth of snowpack)
Consistency and Completeness Report: Data set is considered complete for the information presented, as described in the abstract. Users are advised to read the rest of the metadata record carefully for additional details.
Factor Affecting the Research: Antecedent weather conditions and weather conditions at the time of measurement have the ability to change sample attributes due to: snow compaction, wind redistribution, sublimation, melt, & debris landing on board. Observers made note of these conditions whenever they were obvious.
Use Restrictions: No use constraints are associated with this data.
Distribution Info:
Organization Name: ARM Archive User Services
Email: armarchive[at]ornl.gov Phone: 1-888-ARM-DATA
Street: Oak Ridge National Laboratory City: Oak Ridge
State: Tennessee Postal: 37831-6290
Additional Missing Info: Kettle Ponds (Winter/Spring 2022 only) The “Kettle Ponds” meteorological station and SAIL study site at an elevation of 2858 m (38.941553, -106.973010). SNI-2 (Winter/Spring 2022 and 2023) (aka “Middle Snodgrass”) Open Meadow meteorological station operated by Mark Raleigh (Oregon State University) located at 3132.24 m ASL on Snodgrass Mountain (38.926571550, -106.978929234). SNI-4 (Winter/Spring 2022 and 2023) (aka “Snodgrass Summit”) Forested meteorological station located approximately 350m south of the summit of Snodgrass Mountain in subalpine Spruce/Fir forest at 3363.7 m ASL (327834.00, 4311155.00).