Evolution Equation for Bidirectional Surface Waves in a Convecting Fluid

In particular, variations in the quasi‐stationary planetary waves and their interaction with the zonal flow have been shown to determine the northern annular

In the “big picture” perspective of the recent years that we have described in Brazil, Spain, Portugal and Puerto Rico there are some similarities and important differences,

- The drastic reduction of the fluid flow, associated with the better results of surface roughness and roundness errors of the workpiece, and the decrease of the wheel wear caused

 The expansionary monetary policy measures have had a negative impact on net interest margins both via the reduction in interest rates and –less powerfully- the flattening of the

Jointly estimate this entry game with several outcome equations (fees/rates, credit limits) for bank accounts, credit cards and lines of credit. Use simulation methods to

The fluctuations of the complex amplitude, measured for a given spatial frequency as a function of wavelength (top panel), can be related to the different values of the corresponding

This thesis centers on the study of two different problems of partial differential equations arising from geophysics and fluid mechanics: the surface quasi-geostrophic equation and

Indeed, this work is focused on the study of in- duced flow by natural convection in convergent and inclined channels (described on Figure 1) in the laminar,