Record Display for the EPA National Library Catalog

RECORD NUMBER: 202 OF 305

Main Title Ozone over San Francisco : means and patterns during pollution episodes /
Author MacKay, Kenneth P.
Publisher Dept. of Meteorology, San Jose State University,
Year Published 1977
Report Number EPA-600-4-74-046; EPA-R-802235; EPA/600/4-77/046
Stock Number PB-274 452
OCLC Number 46853030
Subjects Atmospheric ozone--California--San Francisco ; Air--Pollution--California--San Francisco
Additional Subjects Ozone ; Air pollution ; Meteorological data ; Concentration(Composition) ; California ; Atmospheric motion ; Measuring instruments ; Monitoring ; Data analysis ; San Francisco(California)
Internet Access
Description Access URL
https://nepis.epa.gov/Exe/ZyPDF.cgi?Dockey=20015LJZ.PDF
Holdings
Library Call Number Additional Info Location Last
Modified
Checkout
Status
EJBD  EPA 600-4-77-046 c.1 Headquarters Library/Washington,DC 04/21/2014
EKBD  EPA-600/4-77-046 Research Triangle Park Library/RTP, NC 08/01/2003
ELBD ARCHIVE EPA 600-4-77-046 Received from HQ AWBERC Library/Cincinnati,OH 10/04/2023
ERAD  EPA 600/4-77-046 2 copies Region 9 Library/San Francisco,CA 10/24/2012
ESAD  EPA 600-4-77-046 Region 10 Library/Seattle,WA 03/23/2010
NTIS  PB-274 452 Some EPA libraries have a fiche copy filed under the call number shown. 07/26/2022
Collation xiv, 108 p. : ill., maps ; 28 cm.
Abstract
Measurements of meteorological parameters were taken at six levels and ozone at four levels between 260m and 473m ASL on the Mt. Sutro T.V. Tower in San Francisco during the summers of 1974 through 1976. Hourly average ozone concentrations within the elevated inversion layer at this location exceeded the 8 pphm (160 microgram/cu m) National Ambient Air Quality Standards about 15% of the time. High inversion layer ozone concentrations at this site were associated with high surface concentrations occurring during area-wide air pollution episodes. These episodes occurred when a lobe of the Pacific high pressure system penetrated inland. During these episodes, superposition of synoptic scale northeasterly flow and locally produced mesoscale flow caused easterly or light westerly flows during the late forenoon within the inversion layer and westerly flow in the late afternoon. Inland, where the inversion was destroyed from below, inversion layer and surface generated pollutants were convectively mixed. This mixing and the wind oscillation recycled pollutants. The episodes ended when the synoptic situation reverted to one more normal for the season and pollutants were advected from the area.
Notes
Cover title. "August 1977." Includes bibliographical references (p. 106-107.).