Zhang Yaocun,Qian Yongfu.Characteristics of 10-day meansurface sensible heat flux variations in the SCS monsoon regionand possible connections with the SCS summer monsoon onset[J].Acta Meteor Sin,1999,13(1):1-20.Zhang Yaocun,Qian Yongfu.Characteristics of 10-day mean surface sensible heat flux...
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 ...
In this study we developed and examined a hybrid modeling approach integrating physically-based equations and statistical downscaling to estimate fine-scale daily-mean surface turbulent fluxes (i.e., sensible and latent heat fluxes) for a region of southern California that is extensively covered by ...
Surface latent and sensible heat fluxes always force GMST-variations, whilst net surface longwave and solar radiation fluxes have a damping effect, implying that natural GMST-variations are caused by oceanic heat redistribution. In the models an important trigger for a hiatus period on decadal ...
A built-up patch in a city acts as a source of increased sensible heat flux, as well as anthropogenic heat flux due to human activities such as air-conditioning. Likewise, the colder regions between the patches (also referred to as spacing in this work), especially large-scale urban parks...
for the surface latent and sensible heat fluxes, and section 5 discusses the overall global energy budget. 2. Previous energy budget studies The energy budget for the global annual mean is determined by the net radiant flow of energy at dif- ...
It issued as a surface boundary condition to calculate the surface Reynolds stress and the turbulent surface sensible and latent heat fluxes, for example, see Ref. [160–162]. A wide range of studies has employed M-O similarity for considering the effect of the surface roughness in LES (for...
Sensible heat flux shows an increase from approximately 20 to 80 W m 1 during the onset of the monsoon. Surface fluxes of water vapor indicate the importance of water vapor transport over the ship observation region in the central Arabian Sea during active conditions. Onset of the monsoon over...
Sensible heat flux at the surface (Wh/m²)Latent heat flux at the surface (Wh/m²)Accumulated evaporation (mm)Evaporation 24h (mm) Wind, gusts, direction Wind direction and mean wind speed (kph)Gusts, 1h, alternative colors (km/h)Gusts, 3h (kph)Gusts, Ens. average (kph)Gusts, Ens...
These conditions result in a faster increase of Ta in the morning under drier conditions because the sensible heat flux directly heats the air above the surface18. Second, in the afternoon, the surface long-wave cooling effect is more efficient (Fig. 1) in cold seasons because the ...