Comparisons between the TAO buoy and NASA scatterometer windvectors

S. Dickinson, K. A. Kelly, M. J. Caruso, M. J. McPhaden

Research output: Contribution to journalArticlepeer-review

26 Scopus citations

Abstract

There was an opportunity to compare 10 months of collocated National Aeronautics and Space Administration scatterometer (NSCAT) wind vectors with those from the Tropical Atmosphere Ocean (TAO) buoy array, located in the tropical Pacific Ocean. Over 5500 data pairs, from nearly 70 buoys, were collocated in the calibration/validation effort for NSCAT. These data showed that the wind speeds produced from the NSCAT-1 model function were low by about 7%-8% compared with TAO buoy winds. The revised model function. NSCAT-2, produces wind speeds with a bias of about 1%. The scatterometer directions were within 20° (rms), meeting accuracy requirements, when compared to TAO data. The mean direction bias between the TAO and the NSCAT vectors (regardless of model function) is about 9° with the scatterometer winds to the right of the TAO winds, which may be due to swell. The statistics of the two datasets are discussed, using component biases in lieu of the speed bias, which is naturally skewed. Using ocean currents and buoy winds measured along the equator, it is shown that the scatterometer measures the wind relative to the moving ocean surface. In addition, a systematic effect of rain on the NSCAT wind retrievals is noted. In all analyses presented here, winds less than 3 m s-1 are removed, due to the difficulty in making accurate low wind measurements.

Original languageEnglish (US)
Pages (from-to)799-806
Number of pages8
JournalJournal of Atmospheric and Oceanic Technology
Volume18
Issue number5
DOIs
StatePublished - May 2001
Externally publishedYes

ASJC Scopus subject areas

  • Ocean Engineering
  • Atmospheric Science

Fingerprint

Dive into the research topics of 'Comparisons between the TAO buoy and NASA scatterometer windvectors'. Together they form a unique fingerprint.

Cite this