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Synoptic

  1. Summary Issued Monday 12:26 EDT

    • Synoptic outlook for Australia on Sat 24 Jan 2015

      Saturday 22:00 EDT

      A low pressure system and trough will deepen over eastern NSW and QLD causing widespread rain and possible storms. A trough in the tropics will trigger thundery showers about the Top End. A low pressur...
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    • Synoptic outlook for Australia on Sun 25 Jan 2015

      Sunday 22:00 EDT

      A trough in the east should edge slightly notheastward. The trough will direct hot NW winds across QLD. a cooler southerly change will move up the NSW coast. SW'ly flow around a high in the south will ...
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    • Synoptic outlook for Australia on Mon 26 Jan 2015

      Monday 22:00 EDT

      The trough over QLD should move eastwards off the coast bringing a late southerly change in southeastern QLD. A high will keep much of the southeast dry with cool SE'ly winds along the east coast. A tr...
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    • Synoptic outlook for Australia on Tue 27 Jan 2015

      Tuesday 22:00 EDT

      Moist, SE'ly winds should feed moisture into the trough over the east triggering showers and storms. Another trough in the west will bring a few thundery showers to WA. A high will keep SA clear while ...
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    • Synoptic outlook for Australia on Wed 28 Jan 2015

      Wednesday 22:00 EDT

      A ridge of high pressure will begin to build in the southeast causing dry conditions in SA and showers to ease in eastern VIC and southern NSW. A trough will trigger widespread showers and some storms ...
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    • Synoptic outlook for Australia on Thu 29 Jan 2015

      Thursday 10:00 EDT

      Moist onshore winds will cause a few showers along the east. Troughs over QLD and northern NSW will trigger a few showers and thunderstorms. A low will bring rain and some storms to eastern VIC and TAS...
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    Synoptic outlook for Australia on Sat 24 Jan 2015

    Saturday 22:00 EDT Issued Monday 12:26 EDT

    A low pressure system and trough will deepen over eastern NSW and QLD causing widespread rain and possible storms. A trough in the tropics will trigger thundery showers about the Top End. A low pressure system over northern WA will cause showers. Back to summary ›

    Synoptic outlook for Australia on Sun 25 Jan 2015

    Sunday 22:00 EDT Issued Tuesday 11:41 EDT

    A trough in the east should edge slightly notheastward. The trough will direct hot NW winds across QLD. a cooler southerly change will move up the NSW coast. SW'ly flow around a high in the south will keep SA, VIC and TAS cool. The trough in WA will trigger showers. Back to summary ›

    Synoptic outlook for Australia on Mon 26 Jan 2015

    Monday 22:00 EDT Issued Wednesday 11:01 EDT

    The trough over QLD should move eastwards off the coast bringing a late southerly change in southeastern QLD. A high will keep much of the southeast dry with cool SE'ly winds along the east coast. A trough in the west will trigger isolated storms across interior WA. Back to summary ›

    Synoptic outlook for Australia on Tue 27 Jan 2015

    Tuesday 22:00 EDT Issued Thursday 12:06 EDT

    Moist, SE'ly winds should feed moisture into the trough over the east triggering showers and storms. Another trough in the west will bring a few thundery showers to WA. A high will keep SA clear while directing a few showers to TAS and western VIC. Back to summary ›

    Synoptic outlook for Australia on Wed 28 Jan 2015

    Wednesday 22:00 EDT Issued Friday 11:33 EDT

    A ridge of high pressure will begin to build in the southeast causing dry conditions in SA and showers to ease in eastern VIC and southern NSW. A trough will trigger widespread showers and some storms over northern NSW and QLD. A trough in the west will cause a few thunderstorms. Back to summary ›

    Synoptic outlook for Australia on Thu 29 Jan 2015

    Thursday 10:00 EDT Issued Friday 11:36 EDT

    Moist onshore winds will cause a few showers along the east. Troughs over QLD and northern NSW will trigger a few showers and thunderstorms. A low will bring rain and some storms to eastern VIC and TAS. Heat will build in the west under the influence of a heat trough. Back to summary ›