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Earth Observing Laboratory
Field Data Archive

DYNAMO: NOAA P-3 Dropsonde High Resolution L3 Data

Summary

This is one of the upper air data sets developed for the Dynamics of the Madden-Julian Oscillation (DYNAMO) 2011-2012 project. This data set contains 469 high vertical resolution dropsondes released from the NOAA P-3 between 9 November and 13 December 2011. This data set is the same as NOAA P-3 Dropsonde High Resolution L3 Data (EOL format) but with the format converted to the EOL Sounding Composite (ESC) format to match the L2 DYNAMO sounding data sets.

Data access

  • ORDER data to made available for download
  • Preview dataset (plots/images)

Additional information

Identifier
Data Quality final
Versions
  • 1.0 (2012-09-12)
  • 2.0 (2017-01-04):

    This version corrects a temperature dependent dry bias that was present in the Vaisala RD94 dropsonde.  Both the relative humidity and dew point values have been corrected.

(Only the current version of the data is available to order. If you have questions about a prior version, please email us.)
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Spatial Type point
Frequency criteria
Language English
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Temporal coverage

Begin datetime 2011-11-09 07:00:00
End datetime 2011-12-13 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 0.992, Minimum (South) Latitude: -14.362
Minimum (West) Longitude: 70.234, Maximum (East) Longitude: 82.915

Primary point of contact information

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

Additional contact information

Citation

UCAR/NCAR - Earth Observing Laboratory. 2017. DYNAMO: NOAA P-3 Dropsonde High Resolution L3 Data. Version 2.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D63J3B5W. Accessed 23 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.