214  
FXUS10 KWNH 160636  
PMDHMD  
 
MODEL DIAGNOSTIC DISCUSSION  
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD  
236 AM EDT TUE JUN 16 2020  
 
VALID JUN 16/0000 UTC THRU JUN 19/1200 UTC  
 
...SEE NOUS42 KWNO (ADMSDM) FOR THE STATUS OF THE UPPER AIR  
INGEST...  
 
00Z MODEL EVALUATION INCLUDING PREFERENCES AND FORECAST CONFIDENCE  
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
 
...CLOSED LOW LINGERING ACROSS THE SOUTHEAST THROUGH WEDNESDAY,  
LIFTING BACK INTO CENTRAL APPALACHIANS BY THURS...  
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
PREFERENCE: GENERAL MODEL BLEND  
CONFIDENCE: ABOVE AVERAGE  
 
07Z UPDATE: THE 00Z UKMET AND CMC BOTH TRENDED BACK TOWARD THE 00Z  
GFS/NAM POSITIONS THROUGH THE LENGTH OF THE SHORT-TERM TO SUPPORT  
A HIGH CONFIDENCE GENERAL MODEL BLEND.  
 
---PRIOR DISCUSSION---  
GUIDANCE CONTINUES TO BE WELL CLUSTERED WITH THE EVOLUTION OF THE  
EASTERN US CLOSED LOW. OBVIOUSLY, SMALLER SCALE AFFECTS OF  
CONVECTION AND MINOR MASS DIFFERENCES/STRENGTH OF THE RIDGE TO THE  
NORTH PLAY A LARGER ROLE IN THE MODEL SPREAD BY DAY 3. FOR  
EXAMPLE, THE 12Z UKMET DRIFTS NORTH A BIT FASTER DUE TO FINDING  
THE GREATEST WEAKNESS/RIDGING RELATIVE TO THE CLOSED LOW TO THE NW  
AND THE RIDGE TO ITS NORTH. IT IS MINOR AND WITHIN THE REALM OF  
POSSIBILITIES BUT DRIFTS OUT OF BEST CONSENSUS AND CONTINUITY, TO  
PERHAPS WEIGHT A BIT LOWER. EQUALLY, THE CMC IS A BIT WEAKER TOO.  
SO FROM A BLENDING/CONFIDENCE PERSPECTIVE, A STRONGER/TIGHTER  
BLEND OF THE 00Z GFS/NAM AND 12Z ECWMF WILL PROVIDE HIGHER  
PRESCIENCE TO THE FORECAST, BUT A GENERAL MODEL BLEND WOULD BE  
ACCEPTABLE TO ACCOUNT FOR THE INHERENT UNCERTAINTY IN ANY CLOSED  
LOW. GIVEN THE OVERALL SMALLER SPREAD AND CONTINUED SOLID  
VERIFICATION OF THE SYSTEM WITH THE GUIDANCE, WILL SUPPORT THE  
HIGHER PRECISION IN A 00Z GFS/NAM AND 12Z ECMWF BLEND. CONFIDENCE  
IS ABOVE AVERAGE GIVEN SMALLER OVERALL SPREAD IN THE GUIDANCE  
SUITE INCLUDING ENSEMBLE SOLUTIONS.  
 
...CLOSED LOW MOVING INTO THE NORTHWEST TUESDAY INTO THE NORTHERN  
HIGH PLAINS BY THURS...   
..NORTHERN PLAINS SURFACE LOWS/N-S FRONTAL ZONE  
 
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
PREFERENCE: GENERAL MODEL BLEND UP TO 60HRS (18.12Z)  
00Z UKMET/ECMWF BLEND (INCL GEFS/ECENS IF DESIRED)  
CONFIDENCE: AVERAGE TO SLIGHTLY ABOVE AVERAGE  
 
07Z UPDATE: THE 00Z CMC IS A BIT WEAKER THROUGH THE BASE OF THE  
APPROACHING TROF WHICH LEADS TO LATER BINARY INTERACTION WITH THE  
NORTHERN PORTION OF THE LARGER SCALE CIRCULATION OVER S CANADA.  
THIS LEADS TO A SLIGHT WEST AND SOUTH DRIFT RELATIVE TO THE  
ENSEMBLE MEAN WHICH CONTINUES TO BE BEST REPRESENTED BY THE  
ECMWF/UKMET. AS SUCH WILL CONTINUE A GENERAL MODEL BLEND ENDING  
AROUND 18.12Z SHIFTING TOWARD A 00Z ECMWF/UKMET BLEND THEREAFTER.  
SOME INCLUSION OF THE 00Z GEFS/12Z ECENS MAY HELP TO ACCOUNT FOR  
SOME UNCERTAINTY IF DESIRED.  
 
---PRIOR DISCUSSION---  
BROAD TROF/CLOSED LOW OVER THE PACIFIC NW WILL CONTINUE TO SHIFT  
EASTWARD, THE LEADING SHORTWAVE/HEIGHT-FALLS WILL EXPAND EASTWARD  
AND ALLOW THE SECONDARY/MAIN INNER CORE TO THE CLOSED LOW TO  
SHARPENS THE TROF AS A WHOLE THROUGH THE SNAKE RIVER PLAIN, BEFORE  
CONSOLIDATING ACROSS THE SOUTHERN PRAIRIES OF CANADA. THE  
EVOLUTION LOOKS QUITE CONSISTENT AND REALISTIC THROUGH 60HRS  
(18.12Z) BUT BIASES START TO MANIFEST AND LEAD TO INCREASED  
SPREAD. THE 00Z GFS SHOWS A FASTER EVOLUTION, WHICH PULLS IT  
OUTSIDE OF THE ENSEMBLE SUITE, WHILE THE 00Z NAM RETAINS A MORE  
COMPACT BASE TO THE TROF, LEADING TO A SLOWER AND STRONGER SURFACE  
WAVE EMERGING INTO THE PLAINS LATE THURSDAY INTO FRIDAY; BOTH  
TYPICAL OF KNOWN NEGATIVE BIASES. THE 12Z ECMWF APPEARS TO HAVE A  
NORTHWARD BIAS WITHIN THE ENSEMBLE SUITE AND REMAINING GUIDANCE  
BUT COMBINED WITH THE UKMET/CMC THROUGH THE DEPTH OF THE  
TROPOSPHERE SEEMS A PRUDENT WITH MILD TO ABOVE AVERAGE CONFIDENCE  
IN THE RESULTANT BLEND.  
 
GALLINA  
 
MODEL TRENDS AT WWW.WPC.NCEP.NOAA.GOV/HTML/MODEL2.SHTML  
500 MB FORECASTS AT WWW.WPC.NCEP.NOAA.GOV/H5PREF/H5PREF.SHTML  
 
 
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