Skip to data content Skip to data search
Earth Observing Laboratory
Field Data Archive

WISP04: Winter Icing and Storms Project, 2004

Summary

The 2004 Winter Icing and Storms Project, or WISP-04, sought to understand how hazardous in-flight icing conditions form within clouds, and how we can remotely detect those conditions. In-flight icing occurs when an aircraft flies through super-cooled liquid cloud drops. WISP-04 ran from February 15th through March 31st, 2004.

The NOAA Environmental Technology Laboratory (ETL) deployed its Ground-based Remote Icing Detection System (GRIDS) at a field site near Erie, Colorado, which is approximately 35 km northwest of Denver. GRIDS combines a very sensitive, polarimetric Doppler cloud radar with a microwave radiometer and temperature profile information from the NOAA Rapid Update Cycle analysis, to find liquid within clouds and determine if it is super-cooled liquid.

NOAA-ETL collaborated with the National Center for Atmospheric Research (NCAR) and the University of North Dakota. NCAR employed a dual-frequency radar system, balloons and computerized icing forecast tools, whereas UND flew their Citation aircraft to provide in-situ confirmation of cloud conditions.

WISP-04 followed closely on the heals of the second Alliance Icing Research Study (AIRS-II), which was held from November 3 through December 12th, 2003 in Montreal Canada. Though larger in scope than WISP-04, AIRS-II shared similar objectives.

Data access

Datasets from this project

Additional information

GCMD Name V - Z > WISP > Winter Icing and Storms Project > a0d64b73-fb48-4d27-b1a5-601fe18af09e
Related links

Temporal coverage

Begin Date 2004-02-17 00:00:00
End Date 2004-04-04 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 40.00, Minimum (South) Latitude: 40.00
Minimum (West) Longitude: -105.00, Maximum (East) Longitude: -105.00

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.