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Earth Observing Laboratory
Field Data Archive

CFACT: NCAR/EOL ISFS High Rate Surface Meteorology and Flux Products - winds in planar geographic and tilt corrected coordinates

Summary

High rate surface meteorology and flux products collected by the EOL/Integrated Surface Flux System team during the Cold Fog Amongst Complex Terrain (CFACT) field campaign in Heber Valley, Utah. These data have been quality controlled and are available in netCDF format. The winds reported by the sonic anemometers have been rotated into geographic coordinates and corrected for the orientation of the instrument. The orientation and tilt corrections applied were determined by the using the planar fit method from Wilczak, Oncley, and Stage (2001). Data were collected from 11 sites (2 towered Supersites + 9 Satellite sites) located around Heber Valley. That data have been merged in time increments that vary by sensor from 50 ms for 20 Hz sensors to 1 s for 1 Hz sensors.

Data access

Additional information

Identifier
Data Quality final
Versions
  • 1.0 (2022-11-18)
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Language English
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Temporal coverage

Begin datetime 2021-12-04 00:00:00
End datetime 2022-03-02 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 42.00, Minimum (South) Latitude: 37.00
Minimum (West) Longitude: -114.00, Maximum (East) Longitude: -109.00

Primary point of contact information

EOL Data Support <datahelp@eol.ucar.edu>

Additional contact information

Citation

NSF NCAR/EOL ISFS Team, Oncley, S. 2022. CFACT: NCAR/EOL ISFS High Rate Surface Meteorology and Flux Products - winds in planar geographic and tilt corrected coordinates. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.26023/V6YS-HG3P-HJ0G. Accessed 04 Dec 2024.

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NSF

This material is based upon work supported by the NSF National Center for Atmospheric Research, a major facility sponsored by the U.S. National Science Foundation and managed by the University Corporation for Atmospheric Research. Any opinions, findings and conclusions or recommendations expressed in this material do not necessarily reflect the views of the U.S. National Science Foundation.