Spatial distribution of tropospheric ozone in western Washington, USA

被引:32
作者
Cooper, SM [1 ]
Peterson, DL [1 ]
机构
[1] Univ Washington, US Geol Survey, Forest & Rangeland Ecosyst Sci Ctr, Field Stn, Seattle, WA 98195 USA
关键词
mountainous regions; Pacific Northwest; passive ozone samplers; spatial variation; tropospheric ozone;
D O I
10.1016/S0269-7491(99)00172-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We quantified the distribution of tropospheric ozone in topographically complex western Washington slate, USA (total area approximate to 6000 km(2)). using passive ozone samplers along nine river drainages to measure ozone exposure from near sea level to high-elevation mountain sites. Weekly average ozone concentrations were higher with increasing distance from the urban core and at higher elevations, increasing a mean of 1.3 ppbv per 100 m elevation gain for all mountain transects. weekly average ozone concentrations were generally highest in Cascade Mountains drainages east and southeast of Seattle (maximum = 55-67 pbv) and in the Columbia River Gorge east of Portland (maximum = 59 ppbv), and lowest in the western Olympic Peninsula (maximum = 34 ppbv). Higher ozone concentrations in the Cascade Mountains and Columbia River locations downwind of large cities indicate that significant quantities of ozone and ozone precursors are being transported eastward toward rural wildland areas by prevailing westerly winds. In addition, temporal (week to week) variation in ozone distribution is synchronous within and between all drainages sampled, which indicates that there is regional coherence in air pollution delectable with weekly averages. These data provide insight on large-scale spatial variation of ozone distribution in western Washington, and will help regulatory agencies optimize future monitoring networks and identify locations where human health and natural resources could be at risk. Published by Elsevier Science Ltd.
引用
收藏
页码:339 / 347
页数:9
相关论文
共 46 条
[1]   Background ozone in the planetary boundary layer over the United States [J].
Altshuller, AP ;
Lefohn, AS .
JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 1996, 46 (02) :134-141
[2]   TRENDS, SEASONAL-VARIATIONS, AND ANALYSIS OF HIGH-ELEVATION SURFACE NITRIC-ACID, OZONE, AND HYDROGEN-PEROXIDE [J].
ANEJA, VP ;
CLAIBORN, CS ;
LI, Z ;
MURTHY, A .
ATMOSPHERIC ENVIRONMENT, 1994, 28 (10) :1781-1790
[3]   OZONE CASE-STUDIES AT HIGH-ELEVATION IN THE EASTERN UNITED-STATES [J].
ANEJA, VP ;
LI, Z ;
DAS, M .
CHEMOSPHERE, 1994, 29 (08) :1711-1733
[4]  
[Anonymous], RESPONSE W FORESTS A
[5]  
BARNA M, 1999, IN PRESS J APPL METE
[6]   DIURNAL CURVES OF TROPOSPHERIC OZONE IN THE WESTERN UNITED-STATES [J].
BOHM, M ;
MCCUNE, B ;
VANDETTA, T .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1991, 25 (08) :1577-1590
[7]  
BOHM M, 1992, RESPONSE W FORESTS A, P63
[8]   Spatial patterns of tropospheric ozone in the Mount Rainier region of the cascade mountains, USA [J].
Brace, S ;
Peterson, DL .
ATMOSPHERIC ENVIRONMENT, 1998, 32 (21) :3629-3637
[9]   Ozone personal exposures and health effects for selected groups residing in the Fraser Valley [J].
Brauer, M ;
Brook, JR .
ATMOSPHERIC ENVIRONMENT, 1997, 31 (14) :2113-2121
[10]   THE INFLUENCE OF LOCALLY INDUCED WIND SYSTEMS ON THE EFFECTIVENESS OF NOCTURNAL DRY DEPOSITION OF OZONE [J].
BRODER, B ;
GYGAX, HA .
ATMOSPHERIC ENVIRONMENT, 1985, 19 (10) :1627-1637