952
FXUS10 KWNH 100522
PMDHMD
MODEL DIAGNOSTIC DISCUSSION
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD
121 AM EDT SAT AUG 10 2019
VALID AUG 10/0000 UTC THRU AUG 13/1200 UTC
...SEE NOUS42 KWNO (ADMNFD) FOR THE STATUS OF THE UPPER AIR
INGEST...
00Z PRELIMINARY MODEL EVALUATION WITH PREFERENCES AND CONFIDENCE
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
..OVERALL PATTERN ACROSS THE CONUS
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
PREFERENCE: GENERAL MODEL BLEND, LIMITED WEIGHT ON THE CMC
CONFIDENCE: AVERAGE, SLIGHTLY BELOW AVERAGE BY DAY 3
FLOW ACROSS THE CONUS WILL GRADUALLY TRANSITION FROM A
TROUGH-RIDGE-TROUGH TO A MORE ZONAL PATTERN BY EARLY NEXT WEEK.
THIS FLATTENING OF THE CENTRAL PLAINS RIDGE IS WELL AGREED UPON BY
THE GLOBAL SUITE, AND ALTHOUGH THE NAM IS A BIT STRONGER WITH
LOWERING THE HEIGHTS ACROSS THE CENTRAL CONUS, IT IS WITHIN THE
ENSEMBLE ENVELOPE AND CAN BE USED IN THE BLEND.
THE CHALLENGE WILL BE HOW THE MERGING, OR AT LEAST INTERACTION, OF
TWO SHORTWAVES, ONE FROM THE FILLING UPPER LOW MOVING INTO THE PAC
NW, AND THE OTHER MOVING INTO THE SW AROUND THE MONSOON RIDGE,
WILL TEMPORALLY AND SPATIALLY EVOLVE INTO EARLY NEXT WEEK. THE CMC
APPEARS THE FASTEST WITH ENERGY MOVING ATOP THE RIDGE IN THE
INCREASINGLY ZONAL FLOW, WHILE THE UKMET IS A BIT ON THE SLOW END,
ESPECIALLY WITH ITS QPF. THERE REMAINS FAIRLY LARGE SPREAD IN THE
QPF FIELDS ACROSS THE CENTRAL PLAINS AND INTO THE WESTERN GREAT
LAKES BY MONDAY, DESPITE MINIMAL DIFFERENCES IN THE POSITION OF
THE PARENT SHORTWAVES. SINCE THE CMC BEGINS TO OUTRUN THE
CONSENSUS WITH THIS SHORTWAVE, AS WELL AS WITH A SUBSEQUENT
IMPULSE DROPPING INTO THE NW LATE ON DAY 3, IT SHOULD BE USED WITH
CAUTION LATE IN THE FORECAST. HOWEVER, DUE TO THE LARGE
VARIABILITY BY DAY 3, HESITATE TO REMOVE ANY OF THE GUIDANCE AND
INSTEAD RECOMMEND JUST LOWER WEIGHT ON THE CMC, WITH SIGNIFICANT
USE OF THE MEANS TO REDUCE SOME OF THE SPREAD.
MODEL TRENDS AT WWW.WPC.NOAA.GOV/HTML/MODEL2.HTML
500 MB FORECASTS AT WWW.WPC.NOAA.GOV/H5PREF/H5PREF.SHTML
WEISS
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