MultirésolutionA multiresolution analysis (MRA) or multiscale approximation (MSA) is the design method of most of the practically relevant discrete wavelet transforms (DWT) and the justification for the algorithm of the fast wavelet transform (FWT). It was introduced in this context in 1988/89 by Stephane Mallat and Yves Meyer and has predecessors in the microlocal analysis in the theory of differential equations (the ironing method) and the s of as introduced in 1981/83 by Peter J. Burt, Edward H. Adelson and James L.
Continuous wavelet transformIn mathematics, the continuous wavelet transform (CWT) is a formal (i.e., non-numerical) tool that provides an overcomplete representation of a signal by letting the translation and scale parameter of the wavelets vary continuously. The continuous wavelet transform of a function at a scale (a>0) and translational value is expressed by the following integral where is a continuous function in both the time domain and the frequency domain called the mother wavelet and the overline represents operation of complex conjugate.
Vertical-axis wind turbineA vertical-axis wind turbine (VAWT) is a type of wind turbine where the main rotor shaft is set transverse to the wind while the main components are located at the base of the turbine. This arrangement allows the generator and gearbox to be located close to the ground, facilitating service and repair. VAWTs do not need to be pointed into the wind, which removes the need for wind-sensing and orientation mechanisms. Major drawbacks for the early designs (Savonius, Darrieus and giromill) included the significant torque ripple during each revolution, and the large bending moments on the blades.
Morlet waveletIn mathematics, the Morlet wavelet (or Gabor wavelet) is a wavelet composed of a complex exponential (carrier) multiplied by a Gaussian window (envelope). This wavelet is closely related to human perception, both hearing and vision. Wavelet#History In 1946, physicist Dennis Gabor, applying ideas from quantum physics, introduced the use of Gaussian-windowed sinusoids for time-frequency decomposition, which he referred to as atoms, and which provide the best trade-off between spatial and frequency resolution.
Convective instabilityIn meteorology, convective instability or stability of an air mass refers to its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements (such as in orographic lifting, where an air mass is displaced upwards as it is blown by wind up the rising slope of a mountain range) tend to become larger, resulting in turbulent airflow and convective activity.
ÉolienneUne éolienne est un dispositif qui transforme l'énergie cinétique du vent en énergie mécanique, dite énergie éolienne, laquelle est ensuite le plus souvent transformée en énergie électrique. Les éoliennes produisant de l'électricité sont appelées « aérogénérateurs », tandis que les éoliennes qui pompent directement de l'eau sont parfois dénommées « éoliennes de pompage » ou « pompes à vent ». Une forme ancienne d'éolienne est le moulin à vent.
Wind gradientIn common usage, wind gradient, more specifically wind speed gradient or wind velocity gradient, or alternatively shear wind, is the vertical component of the gradient of the mean horizontal wind speed in the lower atmosphere. It is the rate of increase of wind strength with unit increase in height above ground level. In metric units, it is often measured in units of meters per second of speed, per kilometer of height (m/s/km), which reduces to the standard unit of shear rate, inverse seconds (s−1).
Hadley cellThe Hadley cell, also known as the Hadley circulation, is a global-scale tropical atmospheric circulation that features air rising near the equator, flowing poleward near the tropopause at a height of above the Earth's surface, cooling and descending in the subtropics at around 25 degrees latitude, and then returning equatorward near the surface. It is a thermally-direct circulation within the troposphere that emerges due to differences in insolation and heating between the tropics and the subtropics.
VentLe vent est le mouvement d'une partie du gaz constituant une atmosphère planétaire située à la surface d'une planète. Les vents sont globalement provoqués par un réchauffement inégalement réparti à la surface de la planète provenant du rayonnement stellaire (énergie solaire) et par la rotation de la planète. Sur Terre, ce déplacement est essentiel à l'explication de tous les phénomènes météorologiques. Le vent est mécaniquement décrit par les lois de la dynamique des fluides, comme les courants marins.
Matrice (mathématiques)thumb|upright=1.5 En mathématiques, les matrices sont des tableaux d'éléments (nombres, caractères) qui servent à interpréter en termes calculatoires, et donc opérationnels, les résultats théoriques de l'algèbre linéaire et même de l'algèbre bilinéaire. Toutes les disciplines étudiant des phénomènes linéaires utilisent les matrices. Quant aux phénomènes non linéaires, on en donne souvent des approximations linéaires, comme en optique géométrique avec les approximations de Gauss.
