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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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Dynamic and Synoptic Fe<strong>at</strong>ures of a Cold Outbreak during Wet-Season on Southwestern<strong>Amazon</strong>Marcos LongoMaria Assunção Faus da Silva DiasRicardo de CamargoInstituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São PauloRua do M<strong>at</strong>ão 1226, Cidade Universitária, 05508-900, São Paulo, SPTel.: +55 +11 3091 4808 FAX: +55 +11 3091 4808E-mail: marcos@master.iag.usp.brThe aim of this work is to analyse a cold outbreak, or “friagem”, event th<strong>at</strong> reachedSouth-western <strong>Amazon</strong> and Sou<strong>the</strong>rn and Middle Brazil on November 9 th , 1999. Usings<strong>at</strong>ellite images, CPTEC-INPE analysis and surface and sounding d<strong>at</strong>a, it was found th<strong>at</strong> thisevent induced, on South-western <strong>Amazon</strong> <strong>Basin</strong>, decrease of temper<strong>at</strong>ure — reaching about12°C — and specific humidity — as low as 8 g/kg — and increase of wind magnitude — to 7m/s sou<strong>the</strong>rlies. Convection activity, which was intensified before cold front interaction, wassuppressed for 2-3 days after <strong>the</strong> cold outbreak.Since vorticity advection <strong>at</strong> middle to high troposphere is rel<strong>at</strong>ed to temper<strong>at</strong>ureadvection <strong>at</strong> low levels, it was verified th<strong>at</strong> <strong>the</strong> anticyclonic advection induces pressureincrease <strong>at</strong> west side of trough and pressure decrease <strong>at</strong> east side of trough. This fe<strong>at</strong>ure inpressure field gener<strong>at</strong>es cold advection in low levels, which intensifies <strong>the</strong> trough.Cold advection was <strong>the</strong> most important term in <strong>the</strong> temper<strong>at</strong>ure budget equ<strong>at</strong>ion, andan equilibrium was found between adiab<strong>at</strong>ic cooling and diab<strong>at</strong>ic he<strong>at</strong>ing. While it movednorthward, <strong>the</strong> layer which has cold advection became shallower.

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