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MM5 SIMMULATIONS OF SFBA TO SAC/SJV TRANSPORT DURING 30 JULY- 2 AUG 2000 CCOS OZONE EPISODE by Robert D. Bornstein: SJSU pblmodel@hotmail.com Tesfamichael B. Ghidey: LBNL, SJSU Robert Van Buskirk: LBNL Prepared for GMU Workshop July 2004. OUTLINE. SYNOPTIC SUMMARY
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MM5 SIMMULATIONS OF SFBA TO SAC/SJV TRANSPORT DURING 30 JULY- 2 AUG 2000 CCOS OZONE EPISODE by Robert D. Bornstein: SJSU pblmodel@hotmail.com Tesfamichael B. Ghidey: LBNL, SJSU Robert Van Buskirk: LBNL Prepared for GMU Workshop July 2004
OUTLINE • SYNOPTIC SUMMARY • 700 MB (NO MESO INFLUENCES OVER CALIF) • SFC • MM5 CONFIGURATION • DOMAIN 1: SYNOPTIC WINDS • DOMAIN 3: MEOS WINDS • LIV, SAC, & SJV SEQUENTIAL OZONE EPISODE DAYS • STAT MESO-EVALUATION • TEMP • MESOSCALE: TEMP DRIVES WINDS • SYN SCALE: MASS/PRESSURE DRIVES WINDS • WINDS (MESO CONVENTION) • FULL BARB = 1 M/S • FLAG = 5 M/S • CONCLUSION
FORCINGS • EPISODES OCCUR ON GIVEN DAYS • NOT B/C TOPO, EMISSIONS, OR SFC MESO-FORCING (EXCEPT FOR FOG) CHANGES • BUT B/C UPPER LEVEL SYNOPTICS CHANGE, WHICH ALTERS MESO-FORCINGS (TOPO, LAND/SEA, URBAN) VIA T AND THUS V • MUST THUS EVAL ALL ABOVE FACTORS: SYN, TOPO (grid spacing), MESO T & V
700 hPa NWS PREVIEW:1200 UTC OR 0500 PDT Movement of inland H causes episodes • Pre-episode: over Nevada • Episode days: moves SW to over SJV and intensifies • Post-episode: dissipates
Before ozone episodes: offshore G. C. High; synoptic High in Nevada; boundary-Low between Highs; SSW-flow over SFBA
SAC ozone day: SJV Syn H at max intensity; SW flow over SFBA
Surface NWS PREVIEW: 1200 UTC or 0500 PDT • Warm-core upper-H projects down to a sfc inverted thermal-L • Pre-episode: over Nevada • Episode days: moves over SJV and intensifies • Post-episode: weakens
B/F ozone episodes: warm core “inverted thermal L” from Sea of Cortez to S-Nevada; 2nd open-L into northern CA; NW-flow over SFBA and S-flow over SAC
LIV episode day: trough moves NW, forms closed low, with N-S axis thru central CA; SE-flow over Sac
MM5 configuration • Version 3.6.0 • Three domains • 36, 12, 4 km • 55 x 55, 91 x 91, 190 x 190 grid points • 32 sigma levels • up to 100 mb • first full sigma level at 19 m • GDAS IC and BC • Analysis nudging only for V and T for • 36 km domain • above PBL • No obs nudging • Five layer soil model, Gayno-Seaman PBL • Start: 1200 UTC on 28 July and went for 7.5 days • LBNL LINUX single processor: 15 days
MM5 Domain-1: 700 hPa WINDS PREVIEW • NWS charts • give only approx p-center locations • cannot give flow details in SFBA, Carquinez Straits, & SJV • Thus need MM5 to show • Pre-episode H: E of SFBA over NEV • Episode days: bulge from H extends westward over SFBA • Post-episode H: back-E of SFBA over AZ
(B/F episodes) MM5 correct: offshore GC H; Syn H in SE Nev; boundary-L; but S-flow over SFBA vs. SW NWS L H H
SAC episode day: Syn H to Utah with max (now NE-SW) “bulge” (vs. NWS-H over SJV) L now S in Cal (vs. NWS: E over CA/Az border); correct SW flow over SFBA to Sac H H L
MM5 Domain-1: SFC WINDS PREVIEW (12 UTC OR 05 PDT) • Movement to N of thermal L from S-CA sequentially cause episodes • Convergence into LIV • Increased flow to Sac from SFBA • Increased flow into SJV from SFBA • Moves offshore • Flow details: in Domain-3
B/F episodes: warm-core thermal-L to S-Nevada & 2nd CA-L to N (both correct); NW-flow over coast & SFBA (correct) and con-flow over SAC (vs NWS S-flow) L L
SAC episode: S-Low moved N & N-Low moved bit S (NWS showed only closed-L gone); now more W-flow to Sac L L
MM5 SFC-TEMP STATS • DAY AND NIGHT SPATIAL-PATTERNS ARE REASONABLE (NOT SHOWN) • STATS SHOW SOME BIAS (SHOWN), WHICH CAN BE ELIMINATED BY • SELECTING TRUSTWORTHY SITES • ADJUSTING DEEP SOIL TEMP AND SOIL MOISTURE CONTENT
DOMAIN-3: 700 hPa PREVIEW (2100 UTC or 0200 PDT) • Offshore-H formation & Fresno eddy movement cause episodes • Initial flow from S does not produce SFBA to Sac transport • Syn-H formation directs SFBA flow to Sac & con-current Fresno eddy blocks SFBA flow into SJV • When eddy moves to N • SFBA flow into Sac is blocked • SFBA flow into SJV is allowed
SAC episode: H moved to W at coast (vs bulge from CV to coast in D-1); Fresno eddy N of D-1 position (blocks flow into SJV from SFBA; W flow over SFBA (vs. NWS S-flow) directly to SAC H L
SJV episode: Fresno eddy moved N & H moves inland (both better defined than in D-1); flow around eddy blocks SFBA flow to SAC, but forces it S into SJV L H
DOMAIN-3: SUMMARY OF SFC TRANSPORT TO LIVERMORE (KEY HOURS) • Daytime confluence of 3-flows E of LIV (on Mt peak) causes episode • Flow from N from Carquinez Straits • Flow from W thru GGG • Upslope from E-side of hills E of LIV • For episode need • Strong confluence • Low speeds
Sfc winds obs at 0700 PST (1500 UTC) on 31 July, (LIV episode morning) Note con flow into LIV
Sfc-wind Obs at 1400 PST (2200 UTC) on 31 July (LIV episode afternoon) Note flow from N into LIV and out to E
Pre-episode afternoon (1400 PDT): W flow thru GGG & weak con into E-Liv
Episode afternoon (1400 PDT): W flow thru GGG & strong con into E-Liv
DOMAIN 3: SFC TRANSPORT TO SAC SUMMARY • TRANSPORT FROM SFBA BLOCKED BY OPPOSING FLOW ON DAYS BEFORE AND AFTER SAC EPISODE • TRANSPORT FROM SFBA NOT BLOCKED ON DAY OF SAC EPISODE
LIV-episode late-afternoon (1800 PDT): flow to SAC from SFBA blocked
SAC-episode late-afternoon (1800 PDT): flow to SAC from SFBA not blocked
DOMAIN 3: SFC TRANSPORT TO SJV SUMMARY • TRANSPORT FROM SFBA TO SJV MUST NOT BE BLOCKED BY OPPOSING FLOWS • FLOW INTO SJV MUST • NOT BE TOO FAST • SHOW CONFLUENCE
CONCLUSION • SMALL CHANGES IN 700 MB-H AND SFC-L POSITIONS CAUSED SEQUENTIAL DAILY OZONE MAX IN LIV, SAC, AND SJV • NWS CHARTS COULD NOT DISCERN DETAILS OF CHANGES, BUT MM5 COULD • MM5 • MATCHED NWS PATTERNS AND MESO-OBS REASONABLY WELL • PROVIDED ADDITIONAL DETAILS • ADDITIONAL SIMULATIONS SHOULD CORRECT REMAINING DIFFERENCES