CIMA   09099
CENTRO DE INVESTIGACIONES DEL MAR Y LA ATMOSFERA
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
On the genesis and evolution of structure of a bow echo over Northeastern Argentina.
Autor/es:
TORRES BRIZUELA, MARCELA; NICOLINI, MATILDE
Lugar:
Cancun, Mexico
Reunión:
Conferencia; 15th International Conference on Clouds and Precipitation; 2008
Institución organizadora:
IAMAS
Resumen:
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A multicellular storm (Torres Brizuela and Nicolini,
2006) developed over the area of Resistencia (27°27S, 59°03W), Province
of Chaco, Argentina
during the morning of 19 October 2000. A previous paper concluded that this
storm had strong evidences of the typical conditions leading to bow-echo
development and the numerical simulations performed in this study also
evidenced the genesis of this system in the area. The satellite images of this
system displayed the evolution with a pattern and time length similar to the
expected for bow-echoes. A descending rear-inflow jet (RIJ) is frequently responsible for
observed wind damage swaths preferably poleward of the bow apex. This
convective structure more frequently evolves within an environment associated
with elevated moisture (surface dew-point greater than 20C),moderate to strong CAPE
values and with a moderate to strong vertical wind-shear in the lowest 2.5km
AGL.The aim of this work is to study the role of the
Coriolis force on the evolution structure of a bow echo produced over
northeastern Argentina. Two different numerical experiments have been performed
aimed to understand the role of the Coriolis force in organizing the convective
structure of this particular event. The first one (E1) was run without Coriolis force, a second one with the Coriolis
force included (E2). Numerical
simulations of the 19 October 2000 convection using ARPS reproduced correctly
the significant features and arrangement of a bow-echo structure. This bow
convective line comes up more clearly in the E2 experiment. In terms of vertical vorticity, related with
descending motion the southern apex of the system becomes dominant for both
experiments. The rotation in this apex is defined in a smaller area for E2 experiment.
In terms of a stronger magnitude of the RIJ, E1 reproduces it better, but in terms of characteristical lenghts
of a typical bow-echo E2 shows a
better representation. A remarkable pattern of E2 simulation is that mesovortices are insinuated, result already
found by different authors.