The combination of the modified parameterization of the Brutsaert equation for incoming atmospheric radiation and of similarity theory-based bulk parameterization algorithms for latent and sensible surface heat fluxes provided the most accurate SurHF estimates. When optimized for one lake temperature profile...
L. Liang, "Estimating surface energy fluxes using a dual-source data assimilation approach adjoined to the heat diffusion equation," J. Geophys. Res. 117(117), 17118 (2012).Estimating surface energy fluxes using a dual-source data assimilation approach adjoined to the heat diffusion equation[J...
surface heat flux parameterizations and tropical pacific sea surface temperature simulations bulk formulae for latent flux typically differ by 20 w m -2 BS Giese,DR Cayan 被引量: 0发表: 0年 Generalized Inverse of a Reduced Gravity Primitive Equation Ocean Model and Tropical Atmosphere–Ocean Data...
Processes that drive the rate of change (tendency) of SST, often referred to as the terms of the heat-budget equation, are horizontal advection, horizontal and vertical mixing, entrainment and net surface heat flux. Mathematically these processes are represented as follows (See Methods). $$\...
This can be interpreted from the following equation- (2)Δp=4f(Ldi)ρμ22 where L is a characteristic length, ρ and μ are density and dynamic viscosity, and f is known as a friction factor which depends on the surface roughness. If the deposition of the fouling layer increases this ...
We have just derived a useful equation for the heat flux between two black, diffuse surfaces q1 − 2 = A1F1 − 2(Eb1 − Eb2). In analogy to Ohm's law, this can be rewritten in the form of a resistance to heat transfer as q1 − 2 = (Eb 1 − Eb2)/Rspatial where R...
An equation for the daily sensible heat flux ( H d ) having a form analogous to Dalton 's evaporation formula was derived from surface energy budget considerations. This equation discriminates well between relatively homogeneous, low-cover surfaces where surface exchange characteristics can be assumed...
To understand how the very large seasonal surface heat loss over the warm KE water affects the strength of the SST front, we calculate the surface heat flux and oceanic terms in the frontogenesis/frontolysis equation (3). To estimate the meridional gradients across the front, we compute the...
In order to estimate deleterious effects caused by heating in continuous﹚ave end﹑umped solid﹕tate lasers, the heat equation has been solved for an axial... ME Innocenzi,HT Yura,CL Fincher,... - 《Applied Physics Letters》 被引量: 312发表: 1998年 Very Short Wavelength (621.4 nm) Room...
5 m), these processes can be jointly reproduced by a linear downslope diffusion equation applied to the evolving topography in response to the tectonic strain4,7,47,50. The sediment flux at the surface, \({{\rm{q}}}_{s}\), is related to the local slope, ...