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Earth Observing Laboratory
Field Data Archive

DEEPWAVE: Multi-Network Composite Highest Resolution Upper Air Data

Summary

This data set contains a composite of the highest vertical resolution (i.e. the “native resolution”) upper air sounding data from all sources for the Deep-Propagating Gravity Wave Experiment (DeepWave).  The composite includes 853 soundings from  five sources around New Zealand and the surrounding ocean:

  • NSF/NCAR Gulfstream-V dropsondes (282 soundings)
  • Australian Bureau of Meteorology radiosondes from Hobart (137 soundings) and Macquarie Island (140 soundings)
  • NIWA (National Institute of Water and Atmospheric Research) radiosondes from Haast, New Zealand (51 soundings)
  • DLR radiosondes from Lauder, New Zealand (98 soundings)
  • NCAR/EOL radiosondes from Hokitika, New Zealand (145 soundings)

Data access

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Additional information

Identifier
Data Quality final
Versions
  • 1.0 (2016-12-06)
  • 2.0 (2016-12-20):

    This version corrects a temperature dependent dry bias that was present in the Vaisala RD94 dropsonde relative humidity measurements. 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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Temporal coverage

Begin datetime 2014-05-25 01:00:00
End datetime 2014-08-01 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: -42.715, Minimum (South) Latitude: -54.50
Minimum (West) Longitude: 147.50, Maximum (East) Longitude: 170.985

Primary point of contact information

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

Additional contact information

Citation

UCAR/NCAR - Earth Observing Laboratory. 2016. DEEPWAVE: Multi-Network Composite Highest Resolution Upper Air Data. Version 2.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6X34VVD. Accessed 08 Nov 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.