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Why is the Low Level Jet Important to the Baltimore/DC Region?: 

Why is the Low Level Jet Important to the Baltimore/DC Region? MWAQC-TAC Meeting January 21, 2005

Outline: 

Outline Types of Transport LLJ Basics Why is it important? Examples: Upper Air Profiler data Lidar data Modeled data Future Studies Conclusions LLJ

Three Types of Transport That Affect Maryland: 

Three Types of Transport That Affect Maryland Short range VA to MD to PA, etc. Long range (synoptic scale) 100s of miles Generally from W or NW Low Level Night-time Jets 100s of miles SW to NE along the Atlantic All types of transport move an “elevated reservoir” of ozone and ozone precursors into the Washington region

Low Level Jet (LLJ) Formation: 

Low Level Jet (LLJ) Formation Forms between the Appalachian Mountains & Atlantic Ocean At sunset the ground cools/ air poor conductor of heat/air close to ground cools too (~100 meters) Air over the mountains cools more than the air at the same elevation near the coast This temperature gradient induces a southerly wind a few hundred meters above the ground Cool Air Warm Air

What pollutant levels are in the Low Level Jet?: 

What pollutant levels are in the Low Level Jet? Still analyzing this issue Theory and recent work by Penn State and Millersville Universities around Philadelphia indicates that the low level jet transports significant pollutant concentrations (using laser technology called LIDAR and instruments suspended from tethered balloons)

Area of Influence: 

Area of Influence Pollutants in LLJ generally come from ground level sources such as vehicles and small businesses Chart reflects the area of influence pertinent to the Washington DC nonattainment area Expansion of control programs already in use to attainment and nonattainment areas in this region would reduce ozone loads in the Washington region

LLJ and Summer Weather: 

LLJ and Summer Weather LLJ usually develops when weather patterns conducive to high ozone occur “Bermuda High” sets up south of Maryland H

LLJ Location: 

LLJ Location LLJ forms just above the nocturnal inversion This well mixed layer is referred - “Residual Layer” Contains that day’s ozone and ozone precursors (aka Elevated Reservoir) Residual layer non-urban areas during high ozone episodes contain 80 – 110 ppbv per aircraft measurements Ozone and Ozone Precursors Residual Layer/Elevated Reservoir Nocturnal Inversion

LLJ Duration: 

LLJ Duration Transport relevant threshold set at 5 hrs Short duration of 2 hrs are ~3 times as frequent

LLJ Characteristics: 

LLJ Characteristics Ribbon of fast moving air Average wind speeds ~22 mi/hr – ~ 45 mi/hr

Research Implicates LLJ in Transport: 

Research Implicates LLJ in Transport Routinely occurs during high ozone episodes 44% of LLJ cases are Code Orange for 8-hour ozone (>= 85ppbv) 22% of LLJ cases are Code Red for 8-hour ozone (>=105) 70% multi-day events (>=3 consecutive days at or above 85 ppbv for 8-hr average), experienced a LLJ 42% of days days when the 8-hr average was >=105 ppbv, experienced a LLJ Transports both ozone and ozone precursors (NOx and VOCs) Contains approximately 60 – 80 ppbv ozone based on lidar measurements

LLJ and Ozone Concentrations: 

LLJ and Ozone Concentrations Fort Meade ozone when a LLJ is observed

LLJ and Ozone Concentrations: 

LLJ and Ozone Concentrations The SW nocturnal LLJ is associated with high ozone The mean peak ozone for LLJ cases is 82.5 ppbv compared to 68 ppbv for all summer cases 68 ppbv 82.5 ppbv 14.5 ppbv

Ft. Meade Profiler: 

Ft. Meade Profiler 27 mi/hr <31 mi/hr <31 mi/hr

Modeled LLJ: 

Modeled LLJ Rapid Update Cycle (RUC2) Model representation of the low level jet Can be predicted

Lidar: 

Lidar Studies by the PSU using a lidar measured between 80 – 90 ppb of ozone being blown into Philadelphia at night. Ozone precursors This mixes down to the surface in the AM hours

Future Studies: 

Future Studies Early morning aircraft measurements in the LLJ Due to flight restrictions will be flown over Virginia Deploy balloons when conditions are right Vertical profile of ozone concentrations Lidar measurements Ozone and ozone precursors

LLJ Conclusions: 

LLJ Conclusions Transports both ozone and ozone precursors Area of Influence is from Georgia up through Virginia Lidar has measured ozone concentrations in the 60-80 ppb range (1-hr: 125 ppbv and 8-hr: 85 ppbv) The mean peak ozone for LLJ cases is 82.5 ppbv as compared to 68 ppbv for all summer cases

Conclusions: 

Conclusions Research has shown that transport is a dominant factor in Washington DC nonattainment for both ozone and PM fine Searching to find how much is local and how much regional Modeling does poor job of simulating transport and the effectiveness of control strategies in reducing transport

Promote Successful Strategies: 

Promote Successful Strategies Primary goal is to push multi-pollutant legislation to more stringent caps in a shorter timeframe Through interactions with EPA and other states promote wide-spread adoption of area and mobile source controls Adopt cost-effective programs in Washington region Investigate viable ozone strategies, especially those suitable for co-control of PM, for local reductions in the near term

Seek More Wide-spread Regional Solutions: 

Seek More Wide-spread Regional Solutions Continue research Investigate transport Push for effective transport control Implement cost-effective strategies regionally Seek federal assistance More widespread use of proven controls Pro-active programs in source sectors where states are pre-empted from regulation

Acknowledgements: 

Acknowledgements William Ryan Penn State University Charles Piety University of Maryland College Park