TL;DR: In this article, an analytical model for the so-called footprint of scalar fluxes in the atmospheric boundary layer is proposed, which is a generalization of formulations already given in the literature, which allows to account for thermal stability.
Abstract: We propose an analytical model for the so-called footprint of scalar fluxes in the atmospheric boundary layer. It is the generalization of formulations already given in the literature, which allows to account for thermal stability. Our model is only marginally more complicated than these, and it is therefore simple enough to be applicable for a routine footprint analysis within long-term measurements. The mathematical framework of our model is a stationary gradient diffusion formulation with height-independent crosswind dispersion. It uses the solution of the resulting two-dimensional advection – diffusion equation for power law profiles of the mean wind velocity and the eddy diffusivity. To find the adjoint Monin–Obukhov similarity profile, we propose two different approaches, a purely analytical one and a simplenumerical error minimalization.
TL;DR: In this article, an analytic dispersion model is used to estimate the crosswind-integrated flux footprint, which is defined as the contribution, per unit emission, of each element of a surface area source to the vertical scalar flux measured at height z/z m ≥ 0.
Abstract: The flux footprint is the contribution, per unit emission, of each element of a surface area source to the vertical scalar flux measured at height z
m
; it is equal to the vertical flux from a unit surface point source. The dependence of the flux footprint on crosswind location is shown to be identical to the crosswind concentration distribution for a unit surface point source; an analytic dispersion model is used to estimate the crosswind-integrated flux footprint. Based on the analytic dispersion model, a normalized crosswind-integrated footprint is proposed that principally depends on the single variable z/z
m
, where z is a measure of vertical dispersion from a surface source. The explicit dependence of the crosswind-integrated flux footprint on downwind distance, thermal stability and surface roughness is contained in the dependence of z on these variables. By also calculating the flux footprint with a Lagrangian stochastic dispersion model, it is shown that the normalized flux footprint is insensitive to the analytic model assumption of a self-similar vertical concentration profile.
TL;DR: In this article, a novel take-off and landing system using ground-based power is proposed in the EUFP7 project GABRIEL, where the main focus is the calculation of the impact loads on both aircraft and ground system for a wide range of landing conditions.
Abstract: A novel take-off and landing system using ground based power is proposed in the EUFP7 project GABRIEL. The proposed system has the potential benefit to reduce aircraft weight, emissions and noise. A preliminary investigation of the feasibility of the structural design of the connection mechanism between aircraft and ground system has been performed by simulating the landing procedure on a moving ground system. One of the key challenges is the landing on a moving ground system under high crosswind conditions. The main focus in the current research is the calculation of the impact loads on both aircraft and ground system for a wide range of landing conditions (sink rate, velocity differences between aircraft and ground system, etc.). For comparison, conventional landing procedures with a traditional landing gear have also been simulated. Two different aerodynamic models (empirical and vortex lattice method) have been used and compared in the simulations for verification and validation purposes. The results of this research study are a set of load cases and operational constraints that can be used for the structural design of the ground system and modifications to the aircraft. Detailed values are presented in the paper.
TL;DR: In this paper, the aerodynamic behavior of high speed trains is investigated for both still air conditions and cross-wind conditions, and the flow field is described for a number of flow regions such as around the nose of the train, along the side, roof and underbody of a train, and in the wake of train.