Determination of Longwave Heat Flux at the Air-Sea Interface Using Measurements from Buoy Platforms

Abstract

A theory for pyrgeometer operation is utilized for determining downwelling longwave radiation. Errors in downwelling longwave radiation measurements are due to differences in pyrgeometer body and dome temperatures compared to that of the atmosphere. Additionally, incident shortwave radiation fluxes may be important. Using the present theory along with laboratory and field observations, it appears that downwelling longwave heat fluxes can be measured with errors less than 6 W m?2. Longwave heat flux observations from surface buoys deployed in four different oceanic regions suggest that 1) incoming longwave measurements from buoys are repeatable, 2) uncertainties in radiometer calibration are significant and systematic, and 3) pyrgeometers are affected by direct and indirect solar heating. A hybrid measurement method for the determination of net longwave heat flux at the air-sea interface is described. The authors recommend improvement in calibration procedures as well as development of a radiometer to be used as a transfer standard to compare with in situ measurements. Uncertainties in sea surface skin temperature and emissivity are contributors to the error in the net longwave heat flux. However, a targeted error limit goal of ±10 W m?2 for the monthly mean net longwave heat flux appears to be achievable.