Analysis of Broadband Solar Radiation and Albedo over the Ocean Surface at COVE
- 1 October 2002
- journal article
- Published by American Meteorological Society in Journal of Atmospheric and Oceanic Technology
- Vol. 19 (10) , 1585-1601
- https://doi.org/10.1175/1520-0426(2002)019<1585:aobsra>2.0.co;2
Abstract
A coupled atmosphere–ocean radiative transfer model has been applied to analyze a full year of broadband solar irradiances (up and down) measured over an ocean site 25 km east of the coast of Virginia in the Atlantic. The coupled model treats absorption and scattering by layers for both the atmosphere and the ocean explicitly and consistently. Key input parameters for the model (aerosol optical depth, wind speed, and total precipitable water) are also from in situ measurements. Having more observations to specify properties of the atmosphere than of the ocean, better model–observation agreement is obtained for the downwelling irradiance, which depends primarily on the atmospheric optical properties, than for the upwelling irradiance, which depends heavily on the ocean optical properties. The mean model–observation differences for the ocean surface albedo are generally less than 0.01. However, the modeled upwelling irradiances and albedo over the ocean surface are mostly less than the observations... Abstract A coupled atmosphere–ocean radiative transfer model has been applied to analyze a full year of broadband solar irradiances (up and down) measured over an ocean site 25 km east of the coast of Virginia in the Atlantic. The coupled model treats absorption and scattering by layers for both the atmosphere and the ocean explicitly and consistently. Key input parameters for the model (aerosol optical depth, wind speed, and total precipitable water) are also from in situ measurements. Having more observations to specify properties of the atmosphere than of the ocean, better model–observation agreement is obtained for the downwelling irradiance, which depends primarily on the atmospheric optical properties, than for the upwelling irradiance, which depends heavily on the ocean optical properties. The mean model–observation differences for the ocean surface albedo are generally less than 0.01. However, the modeled upwelling irradiances and albedo over the ocean surface are mostly less than the observations...Keywords
This publication has 32 references indexed in Scilit:
- Measurement of Broadband Diffuse Solar Irradiance Using Current Commercial Instrumentation with a Correction for Thermal Offset ErrorsJournal of Atmospheric and Oceanic Technology, 2001
- A flexible inversion algorithm for retrieval of aerosol optical properties from Sun and sky radiance measurementsJournal of Geophysical Research: Atmospheres, 2000
- Characterization of Thermal Effects in Pyranometers: A Data Correction Algorithm for Improved Measurement of Surface InsolationJournal of Atmospheric and Oceanic Technology, 2000
- Seasonal forecastingQuarterly Journal of the Royal Meteorological Society, 1998
- An Examination of the Clear-Sky Solar Absorption over the Central Equatorial Pacific: Observations versus ModelsJournal of Climate, 1997
- Estimation and Model Validation of Surface Solar Radiation and Cloud Radiative Forcing Using TOGA COARE MeasurementsJournal of Climate, 1997
- The CERES/ARM/GEWEX Experiment (CAGEX) for the Retrieval of Radiative Fluxes with Satellite DataBulletin of the American Meteorological Society, 1996
- Bubbles in the close vicinity of breaking waves: Statistical characteristics of the generation and dispersion mechanismJournal of Geophysical Research: Oceans, 1988
- Absorption by dissolved organic matter of the sea (yellow substance) in the UV and visible domains1Limnology and Oceanography, 1981
- Measurement of the Roughness of the Sea Surface from Photographs of the Sun’s GlitterJournal of the Optical Society of America, 1954