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1.
J Air Waste Manag Assoc ; 48(9): 786-97, 1998 Sep.
Artículo en Inglés | MEDLINE | ID: mdl-9775759

RESUMEN

Ozone (O3) concentrations in the Baltimore-Washington (B-W) metropolitan area frequently exceed the National Ambient Air Quality Standard (NAAQS) in the summer months. The most extreme O3 events occur in multi-day high O3 episodes. These events can be regional in scale, with O3 concentrations exceeding the NAAQS at numerous locations along the eastern U.S. seaboard, and are typically associated with slow-moving or stagnant high pressure systems. In the B-W region, the most extreme events typically occur with surface high pressure overhead or just west of the region and an upper air high-pressure area (ridge) to the west or northwest. Besides providing conditions conductive to local O3 production (subsidence and strong low-level inversions, weak horizontal winds, little cloud cover), this weather pattern may also result in transport of O3 and its precursors from heavily industrialized areas west and north of the B-W region. In this paper, observations and back trajectories made during the severe regional O3 event of July 12-15, 1995, are used to confirm the hypothesis that significant regional-scale transport of O3 and its precursors occur during extreme O3 events of the standard type in the B-W area.


Asunto(s)
Contaminación del Aire/análisis , Oxidantes Fotoquímicos/análisis , Ozono/análisis , Mid-Atlantic Region , Estados Unidos , Tiempo (Meteorología)
2.
Science ; 278(5339): 827-30, 1997 Oct 31.
Artículo en Inglés | MEDLINE | ID: mdl-9346474

RESUMEN

Photochemical smog, or ground-level ozone, has been the most recalcitrant of air pollution problems, but reductions in emissions of sulfur and hydrocarbons may yield unanticipated benefits in air quality. While sulfate and some organic aerosol particles scatter solar radiation back into space and can cool Earth's surface, they also change the actinic flux of ultraviolet (UV) radiation. Observations and numerical models show that UV-scattering particles in the boundary layer accelerate photochemical reactions and smog production, but UV-absorbing aerosols such as mineral dust and soot inhibit smog production. Results could have major implications for the control of air pollution.


Asunto(s)
Aerosoles , Esmog , Rayos Ultravioleta , Simulación por Computador , Modelos Teóricos , Ozono , Fotoquímica , Dispersión de Radiación
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