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Earth Observing Laboratory
Field Data Archive

DEEPWAVE: Hokitika Quality Controlled ISS Radiosonde Data

Summary

The National Center for Atmospheric Research/Earth Observing Laboratory (NCAR/EOL) released special radiosondes from its Integrated Sounding System (ISS) site on the west coast of the South Island of New Zealand at Hokitika. During the DEEPWAVE field phase, soundings were released from Hokitika at 00 UTC every day and additional soundings were released at 3 hourly intervals during particular Intensive Observing Periods. This data set includes the quality controlled Hokitika soundings released for the DEEPWAVE field phase (25 May to 28 July 2014). A total of 145 quality-controlled, high vertical resolution (1-second) soundings are contained in the final DEEPWAVE data set.

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Additional information

Identifier
Data Quality final
Versions
  • 1.0 (2015-01-23):

    These Hokitika sounding data in ESC format have been processed from the EOL format data.
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Related projects
Spatial Type point
Frequency 3 hourly
Language English
Categories
Platforms
Instruments
GCMD Science Keywords Expand keywords
Documentation
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Related links

Temporal coverage

Begin datetime 2014-05-25 00:00:00
End datetime 2014-07-27 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: -42.71456, Minimum (South) Latitude: -42.71456
Minimum (West) Longitude: 170.98514, Maximum (East) Longitude: 170.98514

Primary point of contact information

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

Additional contact information

Citation

UCAR/NCAR - Earth Observing Laboratory. 2015. DEEPWAVE: Hokitika Quality Controlled ISS Radiosonde Data. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D61R6NQC. 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.