Over the leads and coastal polynyas, an upward sensible heat flux of 100 to 300 W/mwas typical, except in summer when the air temperature was close to the sea surface temperature. Over the continental shelf ice, the sensible heat flux was predominantly downwards (15 to 20 W/m), ...
The vertical transport of energy from the surface to the atmosphere consists of the flux of sensible heat from the surface Fh and the evaporative water loss from the surface Fe. Thus, we write (8.5.5)Fυ(0)=LFe+Fh, where L is the coefficient for the latent heat of evaporation. On the...
Therefore, the long – term annual mean net heat flux is about 6Wm2 (negative sign means upward heat flux) and shows a very good agreement with the direct measured advective value through the Hormuz Strait. The spatial distribution of the surface heat fluxes, which has not been investigated ...
In contrast, in the nearby area of the Arabian Gulf there is a yearly average of an upward flux at the sea surface, which is compensated by an advective heat flow of approximately 25 W m 2 through the strait of Hormuz. Some of the heat in the Gulf of Oman is transported into the ...
The annual mean values of upward heat transfer due to solar radiation, sensible heat, latent heat and infrared radiation fluxes are 212, 1, 168 and 66 W m2, respectively. Based on the surface inflow and subsurface outflow through the Strait of Hormuz, the annual average heat transport into ...
12 Expanding on it, the diabatic heating terms can be further subdivided into net shortwave radiation, downward longwave radiation, surface latent heat flux, surface sensible heat flux, and ground heat exchange, the relative importance of which varies depending on the region and the type of ...
The climatology, trends and leading modes of land surface latent heat flux (LHF) and sensible heat flux (SHF) as well as their responses to monsoon and precipitation in global land monsoon domains are presented. During the past three decades, LHF and SHF have generally undergone a rising and...
Warm (moist) air near the surface is transported upward by secondary circulations, which leads to a positive sensible (latent) heat flux that cannot be capture by single-tower measurements, if these structures are not carried along the EC system by the mean wind within the flux-averaging time...
Satellite-based hybrid gridded heat flux products include surface sensible heat flux (SHF) and latent heat flux (LHF) from the Goddard Satellite-Based Surface Turbulent Fluxes (GSSTF) [Chou et al., 2003], the Japanese Ocean Flux Data Sets with use of Remote Sensing Observations (J-OFURO) ...
The upward and downward short wave radiations were neglected when the solar altitude was less than zero (Bass et al., 2010).Rn=Rs↓+Rs↑+Rl↓+Rl↑ Sensible heat flux and latent heat flux The sensible heat flux (H) and latent heat flux (LE) were calculated by EdiRe software (developed...