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knocker

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Posts posted by knocker

  1. No significant changes with the NH profile this evening. Some slight differences with the structure/alignment of the tpv which impacts to some extent on the position of the surface high cell in relation to the UK and thus some variation vis the detail, Likely very dry and temps around average but perhaps a tad above over the northern half of the country

    ecmwf-deterministic-nhemi-z500_anom_5day-2939200.thumb.png.9d060e38c06e3d962ce3d04d59ec7370.pnggfs-deterministic-nhemi-z500_anom_5day-2939200.thumb.png.b58b8cb7f4c67833c9d30510f87a5cfd.png610day_03.thumb.gif.5f50bb7b232f898232fe25a380df885a.gif

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  2. And a quick preempt of this evening's gfs ext/ec weeklies outputs with a glance at this morning's extended. The salient ppoints: Aleutian low/Alaskan ridge > Siberia adjacent to the tpv lobe northern Canada > northern Russia; strong westerly upper flow exiting the eastern seaboard around the subtropical high, amplifying to some extent in mid Atlantic, to the east European trough. Likely pretty dry with temps around average

    ecmwf-ensemble-avg-nhemi-z500_anom_5day-3241600.thumb.png.73d534b32744ab31d85e846540b24f8b.pnggfs-ensemble-all-avg-nhemi-z500_anom_5day-3241600.thumb.png.d995e71762dfd1784a2a9017e49e200f.png814day_03.thumb.gif.ab214a7a8c66978d1197a5cf12d9625f.gif

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  3. The differences between the gfs/ecm/NOAA this evening still revolve around the amplification and position of the Atlantic HP, and thus the position of the Euro trough. And although high pressure does remain influential over the UK during the period these differences are reflected in the structure and orientation of it. Likely remaining dry with any precipitation in the NW

    ecmwf-deterministic-nhemi-z500_anom_5day-2852800.thumb.png.685968b11f9155f8f634ba676d17ad22.pnggfs-deterministic-nhemi-z500_anom_5day-2852800.thumb.png.8de99343dfdcd565fca8755a5cca3a8d.png610day_03.thumb.gif.0694488fe56966cbcecd580b4ece24cc.gif

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  4. There is some disagreement between the gfs/ecm at the beginning of next week involving the storms along the eastern seaboard and the energy distribution/jet profile across the Atlantic. Particularly involving the amplification of the high pressure and the knock on affect downstream of the plunge of cold air from the Russian tpv lobe down into Europe. This has some relevance as the UK is on the western periphery of this. This is reflected by the medium term anomalies. Obviously the detail still needs nailing down but the percentage play is dry with surface temps below average.

    ecmwf-deterministic-nhemi-z500_anom_5day-2766400.thumb.png.44a117e5400b98a8a8ec82afa3e42045.pnggfs-deterministic-nhemi-z500_anom_5day-2766400.thumb.png.8ab503d0d241d5ab344d03669d053ece.png610day_03.thumb.gif.2b372e4205678282f8216cb990ee8089.gif

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  5. In December 2021, the NINO.3 SST was below normal with a deviation of -1.1°C (Table and Fig.3). SSTs in the equatorial Pacific were above normal in the western part and below normal in the central to eastern parts (Fig.4 and Fig.6). Subsurface temperatures were above normal in the western part and below normal in the central to eastern parts (Fig.5 and Fig.7). In the atmosphere, convective activity near the date line over the equatorial Pacific was below normal and easterlies in the lower troposphere (i.e., trade winds) over the central equatorial Pacific were stronger than normal (Fig.8, Fig.9, Fig.10). These patterns in the atmosphere and ocean are consistent with features commonly seen in past La Niña events and indicate that La Niña conditions continue in the equatorial Pacific.

    The subsurface cold water volume observed in the eastern equatorial Pacific contributed to keeping SSTs below normal. Meanwhile warm water volume in the western equatorial Pacific began to propagrate eastward. JMA's El Niño prediction model predicts that the NINO.3 SST persists to be below -0.5°C until the end of this winter, then it rises and comes closer to normal towards the coming spring in association with eastward propagation of the warm water in the western equatorial Pacific (Fig.11). In conclusion, the La Niña conditions are likely to continue at least until the end of boreal winter (80%) (Fig.1 and Fig.2), and transfer to ENSO-neutral by the end of spring (80%).

    [Western Pacific and Indian Ocean]

    The area-averaged SST in the tropical western Pacific (NINO.WEST) region was near normal in December (Fig.3). The index is likely to be near normal until boreal spring (Fig.12).

    The area-averaged SST in the tropical Indian Ocean (IOBW) region was below normal in December (Fig.3). The index is likely to be below or near normal until boreal spring (Fig.13).

    http://ds.data.jma.go.jp/tcc/tcc/products/elnino/outlook.html

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  6. The ext mean anomalies this morning have a familiar look. The salient points; Aleutian low/NE Pacific ridge extending to Siberia; adjacent to to tpv aligned northern Canada > north Russia; strong westerly upper flow exiting the eastern seaboard south of the Canadian lobe around the subtropical high amplifying to some extent in the eastern Atlantic. Likely quite dry with temps around average,

    ecmwf-ensemble-avg-nhemi-z500_anom_5day-3068800.thumb.png.49b59533379920e698758d110041248f.pnggfs-ensemble-all-avg-nhemi-z500_anom_5day-3068800.thumb.png.250f00354c6f156071ba219ecf152b83.png814day_03.thumb.gif.8945bed0bcaf17fffefddb158df84feb.gif

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  7. The frontal system currently affecting the country should be the last for a while. Today the warm front will track NE briefly introducing milder air whilst tomorrow the cold front will clear Kent during the afternoon whilst the ridge builds from the south west

    ppva.thumb.gif.b714576448876d183c960df863e6a813.gifppvg.thumb.gif.8b0547dfa4c4348eb44081a8cadee08b.gif

    And for the rest of the week high pressure is in charge and thus light winds and likely some morning frost and mist/fog. But a fair amount going on upstream with both the gfs/ecm running a trough up the eastern seaboard, boosting the jet and promoting the subtropical ridge

    ecmwf-deterministic-natl_wide-z300_speed-2258800.thumb.png.6056b706e86bd5b36d40d366f00b1a56.pngecmwf-deterministic-eur-t850_mslp_prcp6hr-2161600.thumb.png.d5c2b8a9dfe6fd40811b996ef2c73a4b.pngecmwf-deterministic-eur-t850_mslp_prcp6hr-2248000.thumb.png.fd79c801e476f0792694450c325724bc.png

     

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