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Análise Sinótica – 22/07/2009




        Na análise da carta sinótica de superfície das 00Z do dia 22/07 observa-se um intenso
sistema frontal atuando entre o Paraguai, nordeste da Argentina, oeste do RS e leste do
Uruguai, com ciclone extratropical associado de 990hPa, posicionado em 39S/57W, a leste da
Província de Buenos Aires. Um anticiclone de 1021hPa posiciona-se sobre a Atlântico, em
25S/39W, já adquirindo características da Alta Subtropical do Atlântico Sul (ASAS), que tem
núcleo de 1037, centrada em 45S/05W. A sul de 40S sobre o Atlântico observa-se dois sistemas
frontais transientes. A Alta Subtropical do Pacífico Sul (ASPS), com núcleo de 1038 hPa, está
posicionada em torno de 47S/87W. A Zona de Convergência Intertropical (ZCIT) oscila em
torno de 7N e 9N sobre o Pacífico, e sobre o Atlântico este sistema oscila em torno de 8N e
10N. O cavado equatorial atua sobre o norte da Colômbia, Venezuela e Guiana.

       Elaborado pelo Meteorologista Carlos Moura.
Na análise da carta sinótica de superfície das 06Z do dia 22/07 observa-se um intenso
sistema frontal atuando entre o Paraguai, extremo sudoeste do PR, oeste de SC e nordeste do
RS, com ciclone extratropical associado de 978hPa, posicionado em 41S/56W, na altura da
Província de Rio Negro, sobre o Atlântico. Um anticiclone de 1020hPa posiciona-se sobre a
Atlântico, em 25S/39W, com características da Alta Subtropical do Atlântico Sul (ASAS), que
tem núcleo de 1037, centrada em 45S/05W. A sul de 40S sobre o Atlântico observa-se dois
sistemas frontais transientes. A Alta Subtropical do Pacífico Sul (ASPS), com núcleo de 1039
hPa, está posicionada em torno de 45S/88W. A Zona de Convergência Intertropical (ZCIT)
oscila em torno de 8N e 9N sobre o Pacífico, e sobre o Atlântico este sistema oscila em torno
de 8N e 10N. O cavado equatorial atua sobre o norte da Colômbia, Venezuela e Guiana.

        Elaborado pelo Meteorologista Carlos Moura.

        Observação: A análise da carta sinótica é feita exclusivamente com base nos dados
observados. Ressalta-se que o traçado das línhas de pressão e das linhas de espessura é automático,
derivado de modelos numéricos e, sem a intervenção do meteorologista previsor.

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Analise220709

  • 1. Análise Sinótica – 22/07/2009 Na análise da carta sinótica de superfície das 00Z do dia 22/07 observa-se um intenso sistema frontal atuando entre o Paraguai, nordeste da Argentina, oeste do RS e leste do Uruguai, com ciclone extratropical associado de 990hPa, posicionado em 39S/57W, a leste da Província de Buenos Aires. Um anticiclone de 1021hPa posiciona-se sobre a Atlântico, em 25S/39W, já adquirindo características da Alta Subtropical do Atlântico Sul (ASAS), que tem núcleo de 1037, centrada em 45S/05W. A sul de 40S sobre o Atlântico observa-se dois sistemas frontais transientes. A Alta Subtropical do Pacífico Sul (ASPS), com núcleo de 1038 hPa, está posicionada em torno de 47S/87W. A Zona de Convergência Intertropical (ZCIT) oscila em torno de 7N e 9N sobre o Pacífico, e sobre o Atlântico este sistema oscila em torno de 8N e 10N. O cavado equatorial atua sobre o norte da Colômbia, Venezuela e Guiana. Elaborado pelo Meteorologista Carlos Moura.
  • 2. Na análise da carta sinótica de superfície das 06Z do dia 22/07 observa-se um intenso sistema frontal atuando entre o Paraguai, extremo sudoeste do PR, oeste de SC e nordeste do RS, com ciclone extratropical associado de 978hPa, posicionado em 41S/56W, na altura da Província de Rio Negro, sobre o Atlântico. Um anticiclone de 1020hPa posiciona-se sobre a Atlântico, em 25S/39W, com características da Alta Subtropical do Atlântico Sul (ASAS), que tem núcleo de 1037, centrada em 45S/05W. A sul de 40S sobre o Atlântico observa-se dois sistemas frontais transientes. A Alta Subtropical do Pacífico Sul (ASPS), com núcleo de 1039 hPa, está posicionada em torno de 45S/88W. A Zona de Convergência Intertropical (ZCIT) oscila em torno de 8N e 9N sobre o Pacífico, e sobre o Atlântico este sistema oscila em torno de 8N e 10N. O cavado equatorial atua sobre o norte da Colômbia, Venezuela e Guiana. Elaborado pelo Meteorologista Carlos Moura. Observação: A análise da carta sinótica é feita exclusivamente com base nos dados observados. Ressalta-se que o traçado das línhas de pressão e das linhas de espessura é automático, derivado de modelos numéricos e, sem a intervenção do meteorologista previsor.