一回合
发表于 2025-3-23 12:49:36
http://reply.papertrans.cn/59/5835/583465/583465_11.png
bypass
发表于 2025-3-23 17:18:35
http://reply.papertrans.cn/59/5835/583465/583465_12.png
Bernstein-test
发表于 2025-3-23 18:33:02
http://reply.papertrans.cn/59/5835/583465/583465_13.png
DAFT
发表于 2025-3-24 00:04:26
Analysis of Diffusion Field Experiments,riments. These include gradient transfer, spectral diffusivity, second-order closure, large-eddy simulation, and random perturbation models (Briggs and Binkowski, 1985). These models generally require either detailed meteorological and turbulence measurements or many assumptions about these quantiti
misanthrope
发表于 2025-3-24 02:57:29
http://reply.papertrans.cn/59/5835/583465/583465_15.png
HAIRY
发表于 2025-3-24 08:50:52
http://reply.papertrans.cn/59/5835/583465/583465_16.png
得罪人
发表于 2025-3-24 14:11:06
Dispersion in the Stable Boundary Layer,ow dispersion works rather than particular formulas that can be used to estimate ground-level concentrations. Whenever it is possible, I will make recommendations on the use of available models for dispersion. However, my main objective is to provide the type of understanding of dispersion that will
得体
发表于 2025-3-24 17:19:09
http://reply.papertrans.cn/59/5835/583465/583465_18.png
微生物
发表于 2025-3-24 19:36:34
http://reply.papertrans.cn/59/5835/583465/583465_19.png
GIST
发表于 2025-3-25 01:00:22
Concentration Fluctuations Within a Laboratory Convectively Mixed Layer,(.) in this case is usually clearly defined by the height above which stable stratification commences. The turbulence intensities responsible for the dispersion are rather well known functions of height relative to . (Caughey, 1982) if the convective velocity scale . is known. Also, the wind speed a