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Darwin Regional Specialised Meteorological
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Darwin RSMC - FAQWhat is TLAPS and GASP? TLAPS is the Tropical Limited Area Prediction System, part of the Bureau of Meteorology's limited area numerical weather prediction (NWP) model family.GASP is the Global Assimilation Prognosis scheme, the Bureau's spectral global model. TLAPS and GASP are the numerical weather prediction models used by Darwin RSMC to generate analyses and forecasts over the RSMC domain. These models are run twice daily at 00 and 12 UTC on the Bureau of Meteorology's NEC SX5 supercomputer. Why can't I see the charts? All charts are currently only available through Registered User Access, so you require a user-name and password to access them. Access for meteorological organisations can be arranged by contacting Darwin RSMC. For other users please refer to the Registered User Services page for access details.What is RadioFax? Many of the black and white charts on the RSMC web page are broadcast
over a HF radio facsimile service now called VMC and VMW. This replaced
AXI and AXM, which was operated by the Royal Australian Navy on 1
July 2002. More details are available in the
RadioFax Guide and A Guide to
Marine Radio Services pages.
Analyses (ANAL) are drawn from weather observations
taken at a particular nominal time (0000, 0600, 1200, 1800 UTC)
and therefore describe the weather pattern as it occurs. Computer
generated charts are usually only for 0000 and 1200 UTC. Prognoses (PROG) depict forecast patterns
at selcted times, usually at +12, +24, +36 and +48 hours from
the analysis time. Isobars connect points of equal surface pressure
and are represented by numbered solid lines. Streamlines represent the wind flow direction
and are represented by arrowed lines. Isotachs represent points of equal wind speed and are drawn using dashed lines. All wind speeds are 10-minute averages. Wind Barbs indicate the strength and direction from which the wind is blowing. Mean Sea
Level Pressure (MSLP) Analysis & Prognosis Gradient Level Wind Analysis The gradient level lies 1000 metres above the earth's surface and is chosen as the level most representative of the lower atmosphere. The wind at the gradient level, whilst being representative of the surface wind, is less likely to be. modified by topographic and surface friction effects. Also included on these charts are tropical cyclone positions, including information on their names, maximum wind speeds, central pressures and speeds and directions of movement. Upper Wind Analysis & Prognosis Sea Surface Temperature (SST) Analysis Current Warning Summary The Darwin office does not modify these warnings from other agencies but collates them into a unified bulletin. Occasionally an advisory message will be appended to a Current Warnings Summary if there exists an unwarned system for which the Darwin office feels a warning is appropriate. |
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