Yaocun, Zhang, Yongfu, Qian (1999) Characteristics of 10-day mean surface latent heat flux variations in the SCS monsoon region and possible connections with the SCS summer monsoon onset. Acta Meteor. Sinica 13: pp. 414-425ZHANG Yaocun, QIAN Yongfu. Characteristics of 10-day mean surface ...
Surface latent heat flux (LHF) is an important component in the heat exchange between ocean and atmosphere. Seasonal mean LHF changes are often interpreted using seasonal mean wind changes. The present study analyzes the high-frequency wind-induced seasonal mean LHF changes. The changes in daily ...
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 ...
(throughcon-servationofmoisture)indeterminingtheannualglobalmeansurfacelatentheatflux.Despitetheseimportantimprovementsinourunderstanding,anum-berofkeytermsintheenergybudgetremainuncer-tain,inparticular,thenetabsorbedshortwaveandlongwavesurfacefluxes.Withregardtotheradiativeenergycomponent,thereisalsoawiderangeinthe...
Firstly, the weaker descending velocity leads to an undermined southwesterly surface wind response (Fig. 4a–c) in the central Pacific. These surface wind changes reduce the anomalous surface wind speeds, restricting the surface latent heat flux (Fig. 4d–f), and therefore contributing to the ...
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 ...
(thetradewindinversion)isnotconfinedtothestratocumulusregimes,buthasbeenobservedovermostpartsofthesubtropical–tropicalPacificOcean.Inthispaper,theauthorstesttheabilityofasimplebulkboundarylayermodel(BBLM)todiagnoseentrainmentvelocity,cumulusmassflux,andsurfacelatentheatfluxfrommonthlymeanreanalysisdata.ThePBLdepthis...
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...
Under the scenario in which the GMT overshoots an increase of 1.5 °C, the decrease of mid-level clouds leads to increased downwards solar radiation in the SC and warms the surface, resulting in increases in both outgoing longwave radiation and latent heat flux into the atmosphere and ...