University:
California State University, Northridge
Course:
GEOG 103 | Weather
Academic year:

2024
Views:

33

Pages:

2
Author:

http;wwwotr

Smog The type of smog we have in L.A. is called photochemical smog. This means that pollutants (which consist in gaseous as well as particulate form) present in auto exhaust (the primary contributor to our type of smog, but there are many other sources too) react with sunlight to create L.A.’s trademark brown haze. The main products of auto exhaust are nitrogen oxides, carbon monoxide, and reactive hydrocarbons (acetaldehyde, formaldehyde, and ethylene to name a few). These compounds react with sunlight to form the secondary pollutants ozone (O3), nitrogen dioxide (NO2), and assorted other hydrocarbons. (Illustrations are after those in Richard P. Turco’s book, Earth Under Siege, an excellent resource for further reading on this topic.) The formation of our smog follows the general daily cycle below: 1. As the day unfolds (Fig. 1), millions of cars find their way onto our roads and freeways as we begin our commutes to school, work, etc. It’s at this point of the day that auto emissions (CO, NO, and RH) are the highest. During the morning hours, the air is also very calm because heating by the sun hasn’t yet initiated convection and the land/sea breeze cycle. If an inversion layer is present, it will typically be very low to the ground and pollutants from the previous day may still linger underneath it. Fig. 1 2. By midday (Fig. 2), we have continuing auto emissions, and the sun has climbed higher into the sky, the photochemical reactions of the primary emission products is triggered as plenty of solar radiation is available. Now we begin to see higher levels of the secondary pollutants (NO2, O3, and HC), or the familiar brown haze. Due to increased solar heating, the land/sea breeze cycle also begins around this point in the day, and the pollutants begin to be pushed further inland. Fig. 2 3. In the late afternoon, O3 concentrations reach their highest levels. On shore ocean breezes can be quite significant at this point, so smog is pushed far inland. If the winds are strong enough, the smog can be lifted over the mountains, into the deserts beyond, where it can create a plume of pollution for hundreds of miles. 4. By the early evening, Angelenos are headed home. So we again see a peak of vehicle emissions. This second round of primary pollutants is added to the established soup of NO2, O3, and HC. But because the sun is now much lower in the sky, less solar radiation is present, so photochemical reactions diminish. The onshore breezes however still continue to push pollutants inland. 5. During the later evening (Fig. 3), the sea breeze usually diminishes which allows a land breeze to develop. This may create a low level temperature inversion, which traps pollutants below it. If a larger scale inversion layer is present during the day, L.A.’s smog woes are further magnified because this layer works effectively as a “lid” across the Southland and keeps pollutants from dispersing. Fig. 3

From Sunrise to Smog: The Daily Cycle of Photochemical Smog in Los Angeles

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