components are: netheatflux–Qnet; shortwave radiation–Qsw; longwave radiation–Qlw ... The resulting netradiationflux was -31 W m-2, roughly comparable with the mean netheat ... Table 5 gives simple statistics for the east (Tx) and north (Ty) wind stress and the heatfluxcomponents for Leg 2.
Fk + Fq + FΦ T g Equation 3 states that the net TOA radiativeflux is the sum ... radiativecomponent associated with the turbulent exchange of latent heat (LH ... where ∂E/∂t is the energy storage, FTOA:NET is the TOA netradiative energy
is available to go into warming the atmosphere (QH). During the day, the sensible heatflux ... flux allows more energy to be used for sensible heating of the air compared ... from these wet surfaces. The smallest ground heatflux occurred in the sedge wetland
into its sensible and latent heatfluxcomponents. The mean Bowen ratio over the period 08:00 ... to have higher latent heatfluxes than observed seasonally averaged values. Other sources ... season and observations of the sensible heatflux [Fisch et al., 2004] show maximum
where QO is the surface heatflux. The monthly mean QO of is computed ... variation of spatially averaged QO (i.e., long-wave radiation, sensible and latent fluxes) and short-wave radiation Qs. Surface salinity flux, W s is calculated
~" IT ~ -~, ~ ~ 3L~LI ~rl~l ~ _ ' m ~rr'rl~rj -J, Or) I Julian Days, 1993 NetRadiation Sensible HeatFlux o Soil HeatFlux • LatentHeatFlux ... 01 mm day -~) in comparison with the average daily evaporation rate. Bowen ratio measurements of evaporation were conducted from 20 to 24 June 1993. Negative Bowen ratios ... Bowen ratio measurements of evaporation on playa surfaces, the technique, combined
megajoules per square meter; Rn, netradiation; G, subsurface heatflux; H, sensible heatflux; LE, latent heatflux] Rn G H LE Measurement period Bowen ratio (MJ/m2) (MJ/m2 ... was that subsurface heatflux was small in comparison to the remaining fluxes. Measured subsurface heatflux was less than 3 percent of the latent heatflux during 24 hours. At the dry prairie site, daytime subsurface heatflux was approximately 18 percent ... hour ......... Daytime ........ 1Subsurface heatflux at the marsh site
of all components of the energy balance, particularly of soil heatflux, are difficult to perform in wetlands. We therefore do not know the ratio of (H + λE)/Ra for the two study sites and have not adjusted the fluxes for closure, with the consequence