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dallen7908

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Posts posted by dallen7908

  1. I would be more discouraged if we wasted a -AO period during February. Sitting at 0.3" entering the New Year seems like the new normal inside the Beltway.  Is it true that BWI is sitting at 0.1" or did they score a few tenths on another storm. 

    Yes the extended range still looks to feature a ++AO, +NAO, neutral EPO, -PNA.  Over days 6-10, 3 of 21 GEFS members and 3 of 51 EPS members give us 1" or more of snow.  One EPS member gives us 7" during the January 2/3 time frame. Our 3 category chance of above normal temperatures is 40-50% for week 2 a far cry from the 70--80% hell we've seen during deep dark abysmal periods (DDAPS). 

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  2. As last Friday's 3-4 week outlook said. 

    "Intraseasonal variability in the tropics remains weak as there are still no strong MJO or other equatorial wave signals. The Indian Ocean Dipole remains strongly positive, although its amplitude has decreased by about 50% since the beginning of December. ENSO neutral conditions also persist; the SST anomalies in the Nino 1+2, 3, and 4 regions haven't changed much over the past month. Since there are no strong intraseasonal signals to use as Week 3/4 predictors, this forecast is based entirely on dynamical model guidance."

    Unfortunately, the EPS and GEFS (the dynamical model guidance) show a +NAO, ++EPO, +AO, and a slightly negative PNA during the first week of January.  Bleak but does it really matter given this is not a window when it makes sense to make a week 3 forecast. 

     

     

     

  3. WRT to the cold CFS ...

    The following is part of the CPC 3-4 week outlook.  Did the forecaster Kyle MacRitchie mean to say "over-forecasts cold in the Northeast" or am I missing something. Anyways they "forecast" a 50% (50%) chance of above (below) normal temperatures during week 3/4.  They do forecast warmer than normal temperatures and precipitation over the southeast.  The weenie in me says we could be on the cold end of something substantial. 

    The ECMWF and JMA models, as well as a number of SubX models, forecast weaker troughing over Canada and suggest a warmer pattern over the eastern CONUS than the CFS does. Our calibration routine also lowers the cold probabilities in the CFS so that they appear more in-line with the ECMWF and JMA, which suggests that the CFS historically over-forecasts warmth in the Northeast.

  4. To mix metaphors, we're punting the 2nd inning.  No reason to be too upset, but its been a while since we've had a good tracking period over the Holidays. 

    Not sure it matters but the ever-reliable GEFS and EPS ensembles predict that the AO and NAO will become positive shortly after the 1st - if true we could have uncooperative indices in both the Atlantic and Pacific. 

    Our odds of getting rain during the next 10 days aren't that much higher than our odds of getting snow; however, the tail end of December and early January could be wet as the ridge relaxes  - maybe a mixed event in there for us? 

     

     

     

     

     

     

  5. ... am at the AGU meeting this week and I "snuck out" of my session to hear a talk on the Unified Forecasting System: Some highlights:

    Version 15.1 of the GFS officially became operational on June 12th of this year.  It has a 13 km horizontal resolution and 64 layers.  Data are assimilated at a 25 km resolution. Version 14 was retired on September 30.  A minor change was made to the GFS in early November.  It is now assimilating additional data sets including information from GOES-17. 

    Version 12 of the GEFS is scheduled to become operational in August 2020.  It will have  the same dynamical core as version 15 of the GFS and its resolution will increase from 40- to 25-km and will include 31 members as opposed to the current 21.  The system will be run 4 times per day with the 00 UT run being 35 days in length and the other runs 16 days in length. 

    Apparently, the ensemble system has skill out to 10.4 days versus 9.8 for the current system with 2-3 hours of the additional skill due to the additional ensemble members. 

    The next version of the GFS (version 16) is scheduled to become operational in January 2021.  It is in the pre-operational stage now but has been frozen.  It should have 127 levels compared to the current 64 and has bias fixes including (hopefully) one for the lower tropospheric cold -bias.  Not sure what the fix is.

    Version 13 of the GEFS is scheduled to become operational in FY2023.  It should be a "fully" coupled system that includes an ocean model, a wave model, an aerosol model etc. 

     

     

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  6. 3 minutes ago, frd said:

    The much anticipated warm December is coming. Simply can not fight the deep tropics. 

    The same concerns last year regarding the MJO that lasted in the warm phases for weeks on end may repeat again this December.

    The latest AO forecast do not look as good today, the NAO going up.  Source regions are warming. The camp that predicted an overall warm December is a step closer to possibly being correct. Early December this year similar to last year, and then we warm.  Whether it lasts two weeks or longer is still hard to pin down. 

    The consistency of the last few years of the pronounced warm up post 12/20 is an increasing risk again this December. 

    There is a repeating pattern of late.... warm Octobers , cold Novembers, Decembers turning  warmer after the first week.    There could be a delay this December with the cold winning out until the 10th, but still looking like we warm once past the 10th.  

    I will  also mention new research reinforces that the idea in which the MJO is spending more time in the warmer phases while racing  through the cold phases. This is pronounced in the time period from 2010 forward.

     

      

    Yes the ensembles hint that the AO may head positive again after sinking to neutral in the mid-range but that is in the hard to forecast 10-15 day the frame. 

    Is the repeating pattern statistically significant?

    Please provide a reference for the new research on MJO cycling. 

     

     

  7. CPC outlook for Nov 26 to Dec 2 calls for above normal temperatures and precipitation for Maryland with higher than normal uncertainty (see below).  I'm curious as to why only the EPS is used in the blend. 
    
    Is this common during uncertain periods because blends are only useful when the ensemble means are similar? 
    ---------------------------------------------------------
    The official 8-14 day 500-hPa height blend consists of: 100% of Today's 0z
    European Ensemble Mean centered on Day 11
     
    FORECAST CONFIDENCE FOR THE 8-14 DAY PERIOD: Below average, 2 out of 5, due to  
    a relatively amplified pattern forecast over the domain, offset by significant  
    differences between today's GEFS ensemble mean and the 0z ECMWF and Canadian  
    ensemble means. 
     
    FORECASTER: Mike C
  8. I noticed recently that the 500 hPA anomalies from the EPS are based on a 1989-2018 mean.  Aren't the GEFS anomalies based on 1980-2009?  Shouldn't make much difference but perhaps shifting the 30-year period annually would make it less "crazy" to predict a colder than normal season.  

    I also like focusing on the 7-10 day period.  It seems like most of our future weather appears then although it doesn't come into focus until the 2.5 to 6.0 day period. Beyond that there are only a few background states where there is any skill at all unless a 52/48 weighted coin helps you. 

    The EPS 15-day snow mean for the DC-area has been around 1" the last several days - all in the last week of course.  What is a winter background value? 2-3"? and when do we typically reach it (last week of November)? 

     

  9. 4 hours ago, Eskimo Joe said:

    Yuck.  The worst.

     

    Disagree.  1989-1990 was one of the most memorable winters since I've been in the area.  Thanksgiving eve snow storm.  Spent Thanksgiving in NYC watching the Macy's parade in the snow.  Early December snow.  Snow loss through sublimation.  Ice skating on NASA-Goddard pond.  Pattern change between XMAS and New Years. 

    On the medium range front, great to see that the number of EPS members supporting a significant snow in the DC area next weekend (yes that real nice Sunday) has risen from 1 to 3 over the last 24 hours.  

     

     

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  10. ... Isn't there a way the NWS could pinpoint their warnings a bit better?  During the last 3-4 weeks, I've been under 5 or 6 severe thunderstorm warnings and have not received a drop of rain from 4 of them

  11. For the most part I was impressed with how well the models did in the 2.5 - 6 day time frame.  The models were mostly useless in the 8-14 day time frame; however, this is a time frame when models only provide useful information during certain windows when teleconnections indicate that a longer range forecast should have skill (certain combinations of the QBO MJO ENSO post-stratospheric warming). 

  12. 3 hours ago, psuhoffman said:

    The real threat still looks good 

    8955E8D9-C794-4CDA-AE6F-7E9ADCDA5187.thumb.png.60193de47703f567e879071b41b783d8.png

     

    Pretty sure you're not serious but hope you're right; obviously, April 1st is very close to the time of year when only the day-10 model climate is cold enough for accumulating snow. It'll be memorable for sure.  Keep the faith ocean temperatures are near their annual minimum. 

    The EPS also has weak support for this "event" - at least north of DC

  13. 8-14 DAY OUTLOOK FOR MAR 26 - APR 01, 2019  
     
    ... calls for above normal temperatures and precipitation
    
     Anomalous southerly low-level winds increase chances of  
    above normal temperatures for parts of the eastern CONUS. ... the  
    largest probabilities of above average precipitation in the East are restricted  
    to near the coast as the storm system predicted in the 6-10 day period shifts  
    eastward during the week-2 period.  
     
    FORECAST CONFIDENCE FOR THE 8-14 DAY PERIOD: Below average, 2 out of 5, due to  
    fairly good model and tool agreement over most of the domain, largely offset by  
    significant differences between today's GEFS and ECMWF ensembles in the Eastern  
    U.S. 
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