Abstract

AbstractDirect covariance flux (DCF) measurements taken from floating platforms are contaminated by wave-induced platform motions that need to be removed before computation of the turbulent fluxes. Several correction algorithms have been developed and successfully applied in earlier studies from research vessels and, most recently, by the use of moored buoys. The validation of those correction algorithms has so far been limited to short-duration comparisons against other floating platforms. Although these comparisons show in general a good agreement, there is still a lack of a rigorous validation of the method, required to understand the strengths and weaknesses of the existing motion-correction algorithms. This paper attempts to provide such a validation by a comparison of flux estimates from two DCF systems, one mounted on a moored buoy and one on the Air–Sea Interaction Tower (ASIT) at the Martha’s Vineyard Coastal Observatory, Massachusetts. The ASIT was specifically designed to minimize flow distortion over a wide range of wind directions from the open ocean for flux measurements. The flow measurements from the buoy system are corrected for wave-induced platform motions before computation of the turbulent heat and momentum fluxes. Flux estimates and cospectra of the corrected buoy data are found to be in very good agreement with those obtained from the ASIT. The comparison is also used to optimize the filter constants used in the motion-correction algorithm. The quantitative agreement between the buoy data and the ASIT demonstrates that the DCF method is applicable for turbulence measurements from small moving platforms, such as buoys.

Highlights

  • Direct covariance flux (DCF) measurements are widely performed over land from fixed towers and other platforms (Stull 1988)

  • DCF measurements are usually taken from land-based towers close to the sea or from offshore towers in shallow water, such as the Swedish Östergarnsholm tower (Smedman et al 1999; Högström et al 2008); the U.S Air Sea Interaction Tower (ASIT) off Martha’s Vineyard, Massachusetts (Austin et al 2002; Edson et al 2007); and the German Forschungsplattformen in Corresponding author address: Joachim Reuder, Geophysical Institute, University of Bergen, P.O

  • This paper presents a comparison of DCF measurements performed from a surface buoy and the Air–Sea Interaction Tower at the Martha’s Vineyard Coastal Observatory (MVCO)

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Summary

Introduction

Direct covariance flux (DCF) measurements are widely performed over land from fixed towers and other platforms (Stull 1988). To investigate the quality of the DCF measurements from small floating platforms, a surface buoy was moored approximately 500 m southwest of the ASIT (Fig. 1).

Results
Conclusion
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