|
|
|
|
|
Giuseppe Ciardullo, Leonardo Primavera, Fabrizio Ferrucci, Vincenzo Carbone and Fabio Lepreti
The formation of a cyclonic region in which nonlinear interactions generate turbulence in the form of small-scale vortices can be observed because of the different rotating air masses. Turbulence dynamics in cyclones (specifically hurricanes) has been un...
ver más
|
|
|
|
|
|
|
|
|
|
|
Marcos Ronielly Silva Santos,Maria Isabel Vitorino,Luci Cajueiro Carneiro Pereira
Reliable data on the spatiotemporal variability in precipitation patterns are vital to the development of effective public policies for environmental management. The analysis of the variation in rainfall rates is currently limited severely by the depende...
ver más
|
|
|
|
|
|
|
|
|
|
|
Robert Zakinyan, Arthur Zakinyan, Roman Ryzhkov and Julia Semenova
In the present work, an analytical model of the vortex motion basic state of the dry atmosphere with nonzero air velocity divergence is constructed. It is shown that the air parcel moves along the open curve trajectory of spiral geometry. It is found tha...
ver más
|
|
|
|
|
|
|
|
|
|
|
NELSON J. FERREIRA,A. A. CORREIA,MARÍA C.V. RAMÍREZ
This paper analyzes the synoptic scale features of the upper and lower level tropospheric circulation over tropical South America during the first Atmospheric Mesoscale Campaign in the Wet Season (WETAMC) of the Large Scale Biosphere ? Atmosphere Expe...
ver más
|
|
|
|
|
|
|
|
|
|
|
L. ZAVALA SANSÓN
The evolution of tropical cyclonic vortices on the eastern North Pacific is examined by means of a barotropic model with an idealized continental topography. The aim of the study is to investigate the trajectories of cyclones in...
ver más
|
|
|
|
|
|
|
|
|
|
|
MARÍA C. V. RAMÍREZ,MARY T. KAYANO,NELSON J. FERREIRA
Daily European Centre for Medium Range Weather Forecasts (ECMWF) analyses for the 1980-1989 period are used to study cyclonic vortices at the upper tropospheric levels (CVULs) in the vicinity of northeast Brazil. The occurrence of CVULs shows signific...
ver más
|
|
|
|
|
|