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FrenchScotPilot1

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Posts posted by FrenchScotPilot1

  1. On behalf of one of my estimated twitter user, find below something about Global wind Oscillation (GWO).

     

    GWO is arguably the best all round measure of atmosphere because it encompasses GLAAM (see above), Rossby waves, responses to torques (which include global patterns like nao, pna, etc...) and MJO if coherent.

     

    What is missing now is a composite comparison height anomaly set of charts.

     

    Another bit on Atmospheric Angular Momentum (AAM) and espacially its calculated tendency relative

    It includes (Gravity Wave Drag + Coriolis + Mountain + Frictional) Torques + Relative AAM Flux Convergence

    It is shown at the bottom of the page: http://www.esrl.noaa.gov/psd/map/clim/aam.90day.total.shtml

  2. Great link here to teleconnections technical papers http://forum.netweather.tv/topic/73911-technical-teleconnective-papers/ but it would take years to read them all and summarise findings.

     

    What I had in mind was (and I hope it is not too naive/utopistic) AMO, PDO, MJO, ENSO, AAM, etc have the following effects on European weather:

    AMO: effects

    PDO: effects

    MJO: effects

    ENSO: effects

    AAM: effects

    etc...

  3. On behalf of one of my estimated twitter user, find below a random bit on Globally Averaged Angular Momentum (GLAAM). It's assessed as a global (averaged in latitude and longitude) anomaly of AAM.

    • [*]+AM in late summer normally equates to neutral NAO with ridge in mid latitudes [*]+AM can help develop ridges at high latitudes in winter months [*]-AM can help develop ridges in high latitudes in summer months

    For info, last March ('13), which was ended up the coldest in 50 years, had a very defined positive GLAAM.

    Climate indices, monthly atmospheric and Ocean Time Series: http://www.esrl.noaa.gov/psd/data/climateindices/list/

     

    Note: This post will be edited as and when.

     

  4. Thanks Supercell89.

     

    Ok, what do Iknow so far when it comes to global influences.

     

    It's a bit like paper rock scissors:

    Sun influences SST.

    Atmosphere and Ocean influence each other (ENSO).

    ENSO influences MJO.

    MJO influences upper/lower tropical winds.

    Upper winds influence pressure patterns (e.g. jet stream drives NAO)

    Oceans drive PDO and AMO.

     

    AAM is the result of frictional torque (surface friction) and mountain torque (pressure difference on W and E side of mountains).

    AAM is conserved therefore changes are done through torques above.

    Stronger W'lies = Atm AM increase = Earth AM decrease

    Atm AM increase with E'lies in the Tropics, decrease with W'lies in mid latitudes. There is therefore a poleward trasfer of AM.

     

    ENSO changes E'ly trades into W'ly trades. Atm AM increases, Earth AM decreases.

     

    This is what I have so far. My next read is on GWO vs MJO.

  5. I'm creating this topic as some sort of research thread to try to establish how we could improve long range forecasting (1-3 months in advance) using teleconnections and variability indices:

    QBO, ENSO, PDO, GWO, AMO, AAM, Mountain/Frictional torque, etc...

     

    Some analysis/forecasting sites to start with:

     

    AAM, Mountain/frictional torque: http://www.esrl.noaa.gov/psd/map/clim/aam.90day.total.shtml

    GWO, MJO composites: http://www.esrl.noaa.gov/psd/map/clim/gsdm.composites.shtml

    GWO: http://www.atmos.albany.edu/student/nschiral/gwo.html

    MJO: http://www.daculaweather.com/4_mjo_phase_forecast.php

    TIGGE MJOhttp://tparc.mri-jma.go.jp/TIGGE/tigge_MJO.html

    MJO composites: http://www.americanwx.com/raleighwx/MJO/MJO.html

    Various: http://www.cpc.ncep.noaa.gov/products/precip/CWlink/MJO/climwx.shtml

    Various: http://www.ncdc.noaa.gov/teleconnections/index.php

     

    And there are many many more. We could also include SSW.

     

    I've laid out the foundations, please start building the walls :-)

     

    Let's make it a great place to learn...

  6. Aye, it looks quite unsettled, but perhaps the odd nice day in between? Friday looks not too bad at least down here. Tomorrow looks a little breezy for a large chunk of the population across the central belt, and very wet for some too.

    I've started looking ahead at the long range charts for the 12th May as I'm getting married...so far each time I've looked the forecast is for rain! I haven't told the soon to be proper Mrs Catch yet, hopefully the charts are wrong but only time will tell smile.png

    Congratulations! You haven't told her about the weather or about getting married ;)

  7. April sun provides quite mild conditions during the day (circa 8C) but the very cold 850hPa air (-7/-8C) makes them drop again below freezing at night.

    The consequence could be one new (last?) snow/sleet attack tonight from the cold front moving from the N.

    During the day, the last few hundred feet temperature profile is positive but, at night, the whole profile is in the negative range.

    Mid month onwards, 850 hPa temps look to get positive and stay around 0. Tentative spring is likely to appear at this point.

    AO and NAO becoming neutral should ensure that no further incursions of cold air disturb the spring plan.

    Ideally, they both need to be positive to see proper spring temperatures.

    As explained above, moderate sleet/snow has started over Aberdeen 30 min ago. Nice to see flakes again. Ok after this, spring warmth, promise :)

  8. April sun provides quite mild conditions during the day (circa 8C) but the very cold 850hPa air (-7/-8C) makes them drop again below freezing at night.

    The consequence could be one new (last?) snow/sleet attack tonight from the cold front moving from the N.

    During the day, the last few hundred feet temperature profile is positive but, at night, the whole profile is in the negative range.

    Mid month onwards, 850 hPa temps look to get positive and stay around 0. Tentative spring is likely to appear at this point.

    AO and NAO becoming neutral should ensure that no further incursions of cold air disturb the spring plan.

    Ideally, they both need to be positive to see proper spring temperatures.

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