512  
FXUS10 KWNH 050645  
PMDHMD  
MODEL DIAGNOSTIC DISCUSSION  
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD  
244 AM EDT SUN APR 05 2020  
 
VALID APR 05/0000 UTC THRU APR 08/1200 UTC  
 
...SEE NOUS42 KWNO (ADMNFD) FOR THE STATUS OF THE UPPER AIR  
INGEST...  
 
00Z MODEL EVALUATION WITH PREFERENCES AND CONFIDENCE  
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
   
..OVERALL PATTERN ACROSS THE CONUS
 
 
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
PREFERENCE: GENERAL MODEL BLEND  
EXCEPTION: NON-NAM FROM NORTHERN HIGH PLAINS TO GREAT LAKES  
MON-WED  
CONFIDENCE: SLIGHTLY ABOVE AVERAGE  
 
19Z UPDATE: THE 00Z UKMET WAS A TAD FASTER AND NORTH RELATIVE TO  
THE CLOSED LOW AND ITS PRIOR RUN BUT STILL WELL WITHIN AN  
ACCEPTABLE ENVELOPE, BUT ALSO BUILDS SOME CONFIDENCE TOWARD THE  
FASTER NAM/GFS SOLUTION...STILL BELIEVE A GENERAL MODEL BLEND WILL  
WORK FOR THE CLOSED LOW.  
 
THE NORTHERN STREAM SHORTWAVE AND ASSOCIATED SURFACE LOW/FRONTAL  
ZONE THROUGH THE OHIO VALLEY/GREAT LAKES ON DAY 3, SAW LITTLE  
SIZABLE CHANGE WITH EXCEPTION OF THE ECMWF TRENDING EVEN SLIGHTLY  
FASTER. THIS REDUCES CONFIDENCE IN THIS SOLUTION AS IT MAY BE TOO  
WEAK AND FAST. STILL, SO WILL REDUCE SOME OF THE ECMWF INFLUENCE  
IN A PREFERRED BLEND HERE, BUT STILL A NON-NAM BLEND IS BEST.  
 
---PRIOR DISCUSSION---  
EXPANDING/DEEPENING CLOSED LOW ALONG THE WEST COAST DOMINATES THE  
LARGE SCALE CONUS MASS FIELDS, WITH A STRONG/WELL DEFINED  
SUBTROPICAL JET STREAMING ACROSS NORTHERN OLD MEXICO INTO/ALONG  
THE GULF COAST STATES. A SHEAR AXIS/PAIR OF SHORTWAVES ARE WELL  
NORTH OF THE US/CANADIAN BORDER AT THIS POINT; THOUGH IT WILL  
CONTINUE TO EXTEND EASTWARD UNDER THE STRONG ARCTIC ANTICYCLONE,  
EVENTUALLY THE WAVE CONSOLIDATES AND CLIPS NORTHERN NEW ENGLAND  
MONDAY, BROADENING AND MAINTAINING NW FLOW INFLUENCE THROUGH THE  
REMAINDER OF THE PERIOD. WHILE THE 12Z CMC IS INITIALLY SLOWER IT  
IS NOT TERRIBLY SO AND THE OVERALL EVOLUTION THROUGH THE NORTHEAST  
CAN BE SUPPORTED BY A GENERAL MODEL BLEND.  
 
BACK TO THE WEST, THE CLOSED LOW HAS ALSO STARTED TO CONSOLIDATE  
IN MODEL SPREAD/EVOLUTION; AND WHILE THERE REMAINS SOME INTERNAL  
SHORTWAVE/VORTICITY CENTER DIFFERENCES, THE EVOLUTION IS ONLY  
SLIGHTLY DIFFERENT. THE GFS HAD BEEN MUCH MORE PHASED TO THE  
NORTHERN STREAM, BOTH MAKING IT GENERALLY WEAKER BUT ALSO  
PROGRESSING IT FASTER, BUT THE 00Z RUN HAS TEMPERED THIS A BIT. IT  
REMAINS A FASTER SOLUTION IN THE OVERALL SUITE, BUT MORE IN THE  
REALM OF ACCEPTABLE BIAS, ESPECIALLY COMBINED WITH TYPICAL  
ACCEPTABLE BIASES BEING SLOWER IN THE ECMWF/CMC AND TOO STRONG  
(TAD FAST) WITH THE 00Z NAM. AS SUCH A GENERAL MODEL BLEND IS  
SUPPORTED BUT STILL A TAD LOWER WEIGHT TO THE GFS.  
 
THE SHARP NORTHERN STREAM TROF ACROSS BC/ALBERTA WILL BE PRESSED  
EASTWARD BY THE STRONGER UPSTREAM PACIFIC JET, WITH SOME SMALL  
TIMING DIFFERENCES. MAINLY THE 00Z NAM IS A BIT STRONGER AND  
SLOWER WITH ITS EASTWARD PROGRESSION AND SOUTHEASTWARD  
HEIGHT-FALLS ACROSS THE NORTHERN PLAINS. THE RESULTANT COLD  
FRONT/SURFACE LOWS MATCH INITIALLY BUT EVENTUALLY TRACK WELL SOUTH  
AND SLOW IN THE SURFACE LOW CLUSTER SUITE TO REMOVE IT FROM ANY  
PREFERENCE AT THIS TIME. THE 00Z GFS, AS ALLUDED TO BEFORE, IS  
MORE DISCONNECTED WITH THE SOUTHERN STREAM CLOSED LOW AND BECOME  
MORE PROGRESSIVE LIKE THE ECMWF, EVEN SURPASSING THE 12Z  
UKMET/CMC. STILL, WITH THE ECMWF BEING FASTEST, THAT IS A  
UNCHARACTERISTIC POSITION WITHIN THE SUITE, SO WILL HEDGE A BIT  
TOWARD A NON-NAM BLEND OVERALL.  
 
SO TO ENCAPSULATE THE CONUS PREFERENCE, A GENERAL MODEL BLEND IS  
SUPPORTED WITH THE EXCEPTION OF THE 00Z NAM ACROSS THE NORTHERN  
TIER TO THE GREAT LAKES FROM MON TO WED. WITH PERHAPS A TAD LESS  
WEIGHTING TO THE GFS BY THE END OF DAY 3 IN S CA. CONFIDENCE IS  
SLIGHTLY ABOVE AVERAGE IN THIS BLEND FOR THE MASS FIELDS; HOWEVER,  
THE QPF ACROSS THE MID-MS VALLEY TO GULF COAST IS NOT. THE RETURN  
MOISTURE UNDER INFLUENCE OF THE HEIGHT-FALLS/SURFACE CYCLONE  
ACROSS THE PLAINS INTO THE MS VALLEY IS NOT WELL AGREED UPON BOTH  
IN MAGNITUDE AND TIMING, SO CONVECTIVE ACTIVATION IS A BIT LESS  
CERTAIN, AND SO BELOW AVERAGE WITH QPF PLACEMENT.  
 
MODEL TRENDS AT WWW.WPC.NCEP.NOAA.GOV/HTML/MODEL2.SHTML  
500 MB FORECASTS AT WWW.WPC.NCEP.NOAA.GOV/H5PREF/H5PREF.SHTML  
 
GALLINA  
 

 
 
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