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Earth Observing Laboratory
Field Data Archive

NCAR/EOL ISS Surface Meteorology Data

Project:

Summary

This dataset contains final surface meteorology data collected by the NCAR/EOL Integrated Sounding System (ISS) located at the Dugway Proving Ground in Utah during the Instabilities, Dynamics, and Energetics accompanying Atmospheric Layering (IDEAL) field campaign. These data are available in daily netCDF files and have been minimally quality-controlled. We found these data to be complete and have no major issues in quality. We did note that occasionally the wind directions on the Lufft's seem to be reversed. This occurs infrequently and primarily in the 2-m winds data. 

Data access

  • ORDER data to made available for download

Additional information

Identifier
Data Quality preliminary
Versions
  • 1.0 (2017-12-01):

    These data are being released as the final dataset, having been minimally quality-controlled. These are the exact same data as in the earlier, preliminary release.
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Related projects
Spatial Type point
Frequency daily
Language English
Categories
Platforms
Instruments
GCMD Science Keywords Expand keywords
Related links

Temporal coverage

Begin datetime 2017-10-16 00:00:00
End datetime 2017-11-16 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 40.12, Minimum (South) Latitude: 40.12
Minimum (West) Longitude: -113.13, Maximum (East) Longitude: -113.13

Primary point of contact information

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

Additional contact information

Citation

UCAR/NCAR - Earth Observing Laboratory. 2017. NCAR/EOL ISS Surface Meteorology Data. Version 1.0 [PRELIMINARY]. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D63N226P. Accessed 26 Jan 2025.

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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.