621  
FXUS10 KWNH 171559  
PMDHMD  
MODEL DIAGNOSTIC DISCUSSION  
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD  
1158 AM EDT SAT AUG 17 2019  
 
VALID AUG 17/1200 UTC THRU AUG 21/0000 UTC  
 
...SEE NOUS42 KWNO (ADMNFD) FOR THE STATUS OF THE UPPER AIR  
INGEST...  
 
12Z MODEL EVALUATION...INCLUDING PREFERENCES AND CONFIDENCE  
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
   
..OVERALL PATTERN ACROSS THE CONUS  
 
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  
PREFERENCE: NON-UKMET BLEND  
CONFIDENCE: SLIGHTLY ABOVE AVERAGE  
 
BROAD GLOBAL SCALE CYCLONIC TROF BASE COVERS THE NORTHERN HALF OF  
THE CONUS WITH A FEW SMALLER SCALE SHORTWAVES PROGRESSING THROUGH  
THE GREAT LAKES AND ONE STARTING TO TIP INTO THE NORTHERN PLAINS  
TODAY. ADDITIONALLY, RETURN TROPICAL FLOW ALONG WESTERN PERIPHERY  
OF ATLANTIC SUBTROPICAL HIGH CONTINUES TO CONVERGE ALONG  
PERSISTENT DEEP MOISTURE CONFLUENCE AXIS FROM WESTERN GULF TO NC  
COAST AND NORTH OF BERMUDA. EVENTUALLY, THE NORTHERN PLAINS  
SYSTEM WILL CONTINUE TO AMPLIFY IN SOUTH WITH FRONTAL ZONE ACROSS  
THE NORTHERN TIER WHILE SUPPORTING INCREASED MOISTURE AND ASCENT  
IN ADVANCE OF IT ACROSS THE MIDWEST INTO THE NORTHEAST LATE SUNDAY  
THROUGH TUESDAY. IN THIS TROF'S WAKE, THE FLOW WILL FLATTEN AND  
LIFT INTO CANADA WITH A LARGE 594+ DM RIDGE EXPANDING FROM THE  
SOUTHWEST INTO THE CENTRAL PLAINS BY THE END OF THE FORECAST  
PERIOD.  
 
IN THE TROPICAL CONFLUENCE STREAM ACROSS THE SOUTHEAST, A FEW WEAK  
SURFACE WAVES WILL TRANSLATE ALONG IT. THE FIRST CURRENTLY NEAR  
THE VA/NC BORDER JUST OFF SHORE, WILL CONTINUE TO SLIDE EAST WITH  
ALL BUT THE GFS CLOSING THE SYSTEM OFF ALONG 40N. STILL THE GFS  
DOES DEPICT THE WAVE JUST A BIT WEAKER. THE SECOND CURRENTLY  
NEAR CHARLESTON SC, HAS ALL GUIDANCE SUGGESTING A SLIGHTLY  
STRONGER WAVE BUT THE UKMET SUGGESTS A VERY STRONG COMPACT WAVE.  
GIVEN THE CONFLUENCE AXIS (SHAPE/ORIENTATION/ETC) AND NECESSITY  
FOR CONVECTIVE UPSCALE GROWTH (WHICH IS NOT EXPECTED TO THE  
MAGNITUDE NEEDED), WOULD PREFER A NON-UKMET BLEND.  
 
IN THE NORTHERN STREAM, AS THE SHORTWAVE SHARPENS/DEPRESSES INTO  
THE NORTHERN TIER BY SUNDAY, MODEL AGREEMENT IS STRONG, BUT AS THE  
WAVE PASSES NORTH-SOUTH AND SWINGS SLIGHTLY NEGATIVE TILT (WHILE  
FILLING/WEAKENING THOUGH), TIMING AND PLACEMENT OF THE SURFACE  
WAVE/FRONTAL ZONE START TO DISPLACE. THIS IS PARTICULARLY NOTED  
WITH THE UKMET WHICH IS FURTHER EAST AND STRONGER, POSSIBLY  
FALLING INTO A NEGATIVE BIAS NOTED WITH CONVECTIVE UPSCALE GROWTH,  
AS IT SLIDES THROUGH THE GREAT LAKES. THIS IS FAIRLY MINOR BUT  
DOES SHOW THE GREATEST VARIANCE AND ITS REMOVAL WOULD HELP THE  
OVERALL BLEND. THERE ARE OTHER PLACEMENT/DEPTH ISSUES WITH THE  
INNER CORE OF THE WAVE WELL NORTH OF THE BORDER UP INTO HUDSON  
BAY, BUT OTHERWISE A NON-UKMET BLEND WILL SUFFICE AT SLIGHTLY  
ABOVE AVERAGE CONFIDENCE.  
 
MODEL TRENDS AT WWW.WPC.NOAA.GOV/HTML/MODEL2.HTML  
500 MB FORECASTS AT WWW.WPC.NOAA.GOV/H5PREF/H5PREF.SHTML  
 
GALLINA  
 
 
CLICK HERE TO GO TO PREVIOUS BULLETINS.
The Nexlab HPC Page
Main Text Page