Atmospheric water vapor and geoid measurements in the open ocean with GPS

Details Atmospheric water vapor and geoid measurements in the open ocean with GPS Atmospheric water vapor and geoid measurements in the open ocean with GPS

Jun 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005georl..3212813r&link_type=abstract

Geophysical Research Letters, Volume 32, Issue 12, CiteID L12813

Mathematics

Logic

8

Geodesy And Gravity: Atmosphere Monitoring With Geodetic Techniques (6952), Geodesy And Gravity: Ocean Monitoring With Geodetic Techniques (1225, 1641, 3010, 4532, 4556, 4560, 6959), Geodesy And Gravity: Instruments And Techniques

Scientific paper

We have conducted two experiments to determine precipitable water vapor (PWV) and sea surface heights from a cruising ship in the open ocean. During the first experiment (July 7-13, 02) GPS and radiosonde PWV agreed at the 2 mm rms level. During the second experiment (Aug 23-30, 03) GPS compared at 1.5 mm rms (1.1 mm GPS high bias) with eight ship-launched radiosondes and at 2.8 mm rms (1.2 mm GPS high bias) to a ship-based water vapor radiometer (WVR). We estimate that the vertical position of the GPS antenna in the open ocean was determined to better than 10 cm rms. After correcting for ocean tides GPS estimated sea surface heights from the second cruise compared to the CARIB97 geoid at the 32 cm level in the vertical. Because space based observations of PWV over the oceans generally require cloudless conditions and are accurate to about 5-10% we conclude that ship based GPS observations can provide additional useful meteorological information. Based on the 10-cm vertical position rms and the high horizontal resolution of ship-based positions we further conclude that useful geodetic information can be obtained from high accuracy GPS observations from ships in the open oceans.

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