Abstract
A comparison of momentum fluxes determined by the eddy-correlation method(ECM) and the inertial dissipation method (IDM) has been performed using longterm measurements over the sea. The measurements were made on the island ofÖstergarnsholm in the middle of the Baltic Sea. The results show that a`classical' form of the inertial dissipation method, i.e., assuming that the transportterms are negligible, and using an effective value for the Kolmogorov constant of0.55, can be used with a mean relative difference between the two methods of about15% for -1 < z/L < 0.5 (z being height and L the Obukhov length). The IDMmethod works best for high wind speeds and neutral conditions. For low windspeeds (U < 6 m s-1) the relation between the two methods is morecomplex. IDM then gives higher values than ECM on the average (about 20%),especially for swell conditions, indicating the need for an imbalance function inthe turbulent kinetic energy budget. Calculations of the effective Kolmogorovconstant, αa, suggest a dependence upon the wave age, αa increasing with increasing wave age, where the value 0.59 fits the data well for saturated waves.
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Anctil, F. and Donelan, M. A.: 1996, 'Air-Water Momentum Flux Observations over Shoaling Waves', J. Phys. Oceanog. 26, 1344-1352.
Anderson, R. J.: 1993, 'A Study of Wind Stress and Heat Flux over the Open Ocean by the Inertial-Dissipation Method', J. Phys. Oceanog. 23, 2153-2161.
Bergström, H. and Smedman, A.: 1994, 'Stably Stratified Flow in a Marine Atmospheric Surface Layer', Boundary-Layer Meteorol. 72, 239-265.
Deacon, E. L.: 1988, 'The Streamwise Kolmogoroff Constant', Boundary-Layer Meteorol. 42, 9-17.
DeCosmo, J., Katsaros, K. B., Smith, S. D., Anderson, R. J. Oost, W. A., Bumke, K., and Chadwick, H.: 1996, 'Air-Sea Exchange of Water Vapor and Sesible Hat: The Humidity Exchange over the Sea (HEXOS) Results', J. Geophys. Res. 101, 12001-12016.
Donelan, M. A., Drennan, W. M., and Katsaros, K. B.: 1997, 'The Air-SeaMomentum Flux in Wind Sea and Swell', J. Phys. Oceanog. 27, 2087-2099.
Drennan, W. M., Graber, H. C., and Donelan, H. C.: 1999, 'Evidence for the Effects of Swell and Unsteady Winds on Marine Wind Stress', J. Phys. Oceanog. 29, 1853-1864.
Dupuis, H., Taylor, P. K., Weill, A., and Katsaros, K.: 1997, 'Inertial Dissipation Method Applied to Derive Turbulent Fluxes over the Ocean during the Surface of the Ocean, Fluxes and Interactions with the Atmosphere/Atlantic Stratocumulus Transition Experiment (SOFIA/ASTEX) and Structure des Echanges Mer-Atmosphere, Proprietes des Heterogeneites Oceaniques: Recherche Experimentale (SEMAPHORE) Experiments with Low to Moderate Wind Speeds', J. Geophys. Res. 102, 21115-21129.
Edson, J. B., Fairall, C. W., Mestayer, P. G., and Larsen, S. E.: 1991, 'A Study of the Inertial-Dissipation Method for Computing Air-Sea Fluxes', J. Geophys. Res. 96, 10689-10711.
Fairall, C. W., Edson, J. B., Larsen, S. E., and Mestayer, P. G.: 1990, 'Inertial-Dissipation Air-Sea Flux Measurements: A Prototype System Using Realtime Spectral Computations', J. Atmos. Oceanic Tech. 7, 425-453.
Grachev, A. A. and Fairall, C. W.: 2001, 'Upward Momentum Transfer in the Marine Boundary Layer', J. Phys. Oceanog. 31, 1698-1711.
Grelle, A. and Lindroth, A.: 1994, 'Flow istortion by a Solent Sonic Anemometer: Wind Tunnel Calibration and its Assessment for Flux Measurements over Forest and Field', J. Atmos. Oceanic Tech. 11, 1529-1542.
Högström, U.: 1990, 'Analysis of Turbulence Structure in the Surface Layer with a Modified Similarity Formulation for Near Neutral Conditions', J. Atmos. Sci. 47, 1949-1972.
Högström, U.: 1996, 'Review of Some Basic Characteristics of the Atmospheric Surface Layer', Boundary-Layer Meteorol. 78, 215-246.
Josey, S. A., Kent, E. C., and Taylor, P. K.: 1999, 'New Insights into the Ocean Heat Budget Closure Problem from Analysis of the SOC Air-Sea Flux Climatology', J. Climate 12, 2856-2880.
Kaimal, J. C. and Gaynor, J. E.: 1991, 'Another Look at Sonic Thermometry', Boundary-Layer Meteorol. 56, 401-410.
Katsaros, K. B., Smith, S. D., and Oost, W. A.: 1987, 'HEXOS-Humidity Exchange over the Sea, A Program for Research on Water-Vapor and Droplet Fluxes from Sea to Air at Moderate to High Wind Speeds', Bull. Amer. Meteorol. Soc. 68, 466-476.
Large, W. G. and Pond, S.: 1981, 'Open Ocean Momentum Flux Measurements in Moderate to Strong Winds', J. Phys. Oceanog. 11, 324-336.
Large, W. G. and Pond, S.: 1982, 'Sensible and Latent Heat Flux Measurements over the Ocean', J. Phys. Oceanog. 12, 464-482.
Maat, N., Kraan, C., and Oost, W. A.: 1991, 'The Roughness of Wind Waves', Boundary-Layer Meteorol. 54, 89-103.
Oost, W. A., Fairall, C. W., Edson, J. B., Smith, S. D., Anderson, R. J., Wills, J. A. B., Katsaros, K. B., and DeCosmo, J.: 1994, 'Flow Distortion Calculations and their Application in HEXMAX', J. Atmos. Oceanic Tech. 11, 366-386.
Paquin, J. E. and Pond, S.: 1971, 'The Determination of the Kolmogoroff Constants for Velocity, Temperature and Humidity Fluctuations from Second-and Third-Order Structure Functions', J. Fluid. Mech. 50, 257-269.
Pierson, Jr., W. J. and Moskowitz, L.: 1964, 'A Proposed Spectral Form for Fully Developed Wind Seas Based on the Similarity Theory of S. A. Kitaigorodskii', J. Geophys. Res. 69, 5181-5190.
Rieder, K. F. and Smith, J. A.: 1998, 'Removing Wave Effects from the Wind Stress Vector', J. Geophys. Res. 103, 1363-1374.
Schacher, G. E., Davidson, K. L., Houlihan, T., and Fairall, C. W.: 1981, 'Measurements of the Rate of Dissipation of Turbulent Kinetic Energy, ∈, over the Ocean', Boundary-Layer Meteorol. 20, 321-330.
Sjöblom, A. and Smedman, A.-S.: 2002, 'The Turbulent Kinetic Energy Budget in the Marine Atmospheric Surface Layer', J. Geophys. Res. 107(C10).
Sjöblom, A. and Smedman, A.-S.: 2003, 'Vertical Structure in the Marine Atmospheric Boundary Layer and its Implication for the Inertial Dissipation Method', Boundary-Layer Meteorol. 109, 1-25.
Smedman, A., Högström, U., Bergström, H., Rutgersson, A., Kahma, K. K., and Pettersson, H.: 1999, 'A Case Study of Air-Sea Interaction during Swell Conditions', J. Geophys. Res. 104, 25833-25851.
Smedman, A., Tjernström, M., and Högström, U.: 1994, 'The Near-Neutral Marine Atmospheric Boundary Layer with No Surface Shearing Stress: A Case Study', J. Atmos. Sci. 51, 3399-3411.
Smith, S. D.: 1988, 'Coefficients for Sea Surface Wind Stress, Heat Flux, and Wind Profiles as a Function of Wind Speed and Temperature', J. Geophys. Res. 93, 15467-15472.
Smith, S. D., Anderson, R. J., Oost, W. A., Kraan, C., Maat, N., DeCosmo, J., Katsaros, K., Davidson, K., Bumke, K., Hasse, L., and Chadwick, H. M.: 1992, 'Sea Surface Wind Stress and Drag Coefficients: the HEXOS Results', Boundary-Layer Meteorol. 60, 109-142.
Taylor, P. K. and Yelland, M. J.: 2000, 'On the Apparent “Imbalance” Term in the Turbulent Kinetic Energy Budget', J. Atmos. Oceanic Tech. 17, 82-89.
van Atta, C. W. and Chen, W. Y.: 1970, 'Structure Functions of Turbulence in the Atmospheric Boundary Layer over the Ocean', J. Fluid Mech. 44, 145-159.
Volkov, Y. A.: 1970, 'Turbulent Flux of Momentum and Heat in the Atmospheric Surface Layer over a Disturbed Sea-Surface', Izv. Acad. Sci, USSR Atmos. Oceanic Phys., Engl. Transl. 6, 770-774.
Yelland, M. J. and Taylor, P. K.: 1996, 'Wind Stress Measurements from the Open Ocean', J. Phys. Oceanog. 26, 541-558.
Yelland, M. J., Moat, B. I., Taylor, P. K., Pascal, R. W., Hutchings, J., and Cornell, V. C.: 1998, 'Wind Stress Measurements from the Open Ocean Corrected for Airflow Distortion by the Ship', J. Phys. Oceanog. 28, 1511-1526.
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Sjöblom, A., Smedman, AS. Comparison Between Eddy-Correlation and Inertial Dissipation Methods in the Marine Atmospheric Surface Layer. Boundary-Layer Meteorology 110, 141–164 (2004). https://doi.org/10.1023/A:1026006402060
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DOI: https://doi.org/10.1023/A:1026006402060