|
|
|
|
|
Lakshmi Narayana Phaneendra Peri, Antonella Ingenito and Paolo Teofilatto
The goal of this paper is to investigate the aerodynamic and aerothermodynamic behavior of the Schiaparelli capsule after the deployment of a supersonic disk-gap-band (DGB) parachute during its re-entry phase into the Martian atmosphere. The novelty of t...
ver más
|
|
|
|
|
|
|
|
|
|
|
Dian Li, Zhenyang Peng, Guoqiang Liu and Chenyu Wei
On the edges of rivers where the flow velocity is low, aquatic plants flourish, with emergent rigid herbs being the most common. Since the flow structures of vegetated flow are strongly influenced by vegetation distribution patterns, homogeneous and hete...
ver más
|
|
|
|
|
|
|
|
|
|
|
Gokhan Kirkil and Ching-Long Lin
A high-resolution large eddy simulation (LES) of wind flow over the Oklahoma City downtown area was performed to explain the effect of the building height on wind flow over the city. Wind flow over cities is vital for pedestrian and traffic comfort as we...
ver más
|
|
|
|
|
|
|
|
|
|
|
Tirtha Banerjee and Rodman Linn
Quantifying the impact of natural and anthropogenic disturbances such as deforestation, forest fires and vegetation thinning among others on net ecosystem?atmosphere exchanges of carbon dioxide, water vapor and heat?is an important aspect in the context ...
ver más
|
|
|
|
|
|
|
|
|
|
|
Gerardo Caroppi, Paola Gualtieri, Nicola Fontana and Maurizio Giugni
This laboratory study aimed at investigating the mean and turbulent characteristics of a densely vegetated flow by testing four different submergence ratios. The channel bed was covered by a uniform array of aligned metallic cylinders modeling rigid subm...
ver más
|
|
|
|
|
|
|
|
|
|
|
Hermann Knaus, Martin Hofsäß, Alexander Rautenberg and Jens Bange
A model for the simulation of wind flow in complex terrain is presented based on the Reynolds averaged Navier?Stokes (RANS) equations. For the description of turbulence, the standard k-e, the renormalization group (RNG) k-e, and a Reynolds stress turbule...
ver más
|
|
|
|
|
|
|
|
|
|
|
DANIELE MASSERONI,CHIARA CORBARI,MARCO MANCINI
Pág. 335 - 352
The use of energy fluxes data to validate land surface models requires that energy balance closure conservationis satisfied, but usually this condition is not verified when the available energy is bigger than the sumof turbulent vertical fluxes. In this ...
ver más
|
|
|
|
|
|