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Earth Observing Laboratory
Field Data Archive

NAME: Soundings Multi-Network Composite Highest Resolution Upper Air Data

Summary

The upper air highest resolution sounding data for the North American Monsoon Experiment (NAME) 2004 Tier 3 domain (5°N to 50°N latitude and 125°W to 75°W longitude) are contained within this dataset. The dataset covers the time period 1 June through 30 September 2004. This NAME 2004 Sounding Composite Highest Resolution Upper-Air Dataset contains 24308 soundings from 112 sites. The PIBALs are not previewable and will generate an error when selected.

NOTE: As of 23 March 2010 many of the soundings in this data set have had a correction applied to account for a significant dry bias. See the documentation file for details on the correction(s) applied to this data set. Also see Ciesielski et al 2009 in JTECH.

Data access

  • ORDER data for delivery by FTP
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Additional information

Identifier
Data Quality final
Versions
  • 1.0 (2010-03-25)
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Related projects
Spatial Type point
Frequency no set schedule
Language English
Categories
Platforms
Instruments
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Documentation
Related links

Temporal coverage

Begin datetime 2004-06-01 00:00:00
End datetime 2004-09-30 23:59:00

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 50.00, Minimum (South) Latitude: -5.00
Minimum (West) Longitude: -125.00, Maximum (East) Longitude: -75.00

Primary point of contact information

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

Additional contact information

Citation

UCAR/NCAR - Earth Observing Laboratory. 2010. NAME: Soundings Multi-Network Composite Highest Resolution Upper Air Data. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6KP80GD. Accessed 14 Dec 2024.

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Ancillary information

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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.