ANALYSIS OF RADM GAS CONCENTRATION PREDICTIONS USING OSCAR AND NEROS MONITORING DATA

被引:9
作者
MIDDLETON, P [1 ]
CHANG, JS [1 ]
机构
[1] SUNY ALBANY,ATMOSPHER SCI RES CTR,ALBANY,NY 12205
来源
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS | 1990年 / 24卷 / 08期
关键词
Acid rain; deposition model; nitrogen species; O[!sub]3[!/sub; SO[!sub]2[!/sub;
D O I
10.1016/0960-1686(90)90245-I
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The ability of the Regional Acid Deposition Model (RADM) to produce realistic atmospheric trace gas concentration patterns for a variety of atmospheric conditions is explored by comparing model results with surface monitoring data. Two frontal storm system episodes, monitored in 1981 as part of the Oxidation and Scavenging Characteristics of Aptil Rains (OSCAR) experiment, and one relatively dry high-pressure-system case from the 1979 Northeast Regional Oxidant Study (NEROS) were studied. The temporal and spatial variations of SO2, O3 and N species monitored at selected locations throughout the eastern U.S. and Canada are compared to the corresponding RADM grid-average predictions. The analysis is complicated by the fact that grid averages are nor necessarily representative of point measurements when the measurements are strongly influenced by local subgrid-scale phenomena. The comparison database also is limited by gaps in the hourly monitoring data and ambiguity in the N species measurements. To reduce these difficulties, observational sites located in rural and suburban areas which are less influenced by large emission sources were chosen for the comparisons, sharp hourly spikes in the observational data were omitted from the analysis and nitrogen species comparisons were limited to special observations where the measurement ambiguities were less pronounced. Spatial distributions of SO2 and O3 daytime (10 a.m.-4 p.m.) and night-time (10 p.m.-4 a.m.) RADM concentration averages were compared to the observational averages to confirm that the model and data concentration patterns agreed over the domain. Intercomparisons of individual grid-point pair comparisons were facilitated using fractional differences, which are defined as the difference in the observations and predictions divided by the sum of the observations and predictions. Predictions and observations showed similar patterns of high and low concentrations throughout the region for all three of the events for the daytime comparisons; the lower night-time agreement improved when night-time stability adjustments were applied to the model predictions. Summarizing over all of the individual grid-point, day-total comparisons for all three events, it was found that, for O3, all of the pairs were in agreement to better than a factor of two and 50% of them were in agreement to a factor of 1.1 or better; for SO2, 88% of the pairs were in agreement to better than a factor of two and 25% of the pairs were in agreement to a factor of 1.1 or better. Predicted N species concentrations in the 1-4 and 5-7 ppb ranges for two OSCAR cases were comparable to the levels measured at a rural Indiana site during the OSCAR I and OSCAR IV events. Predictions of NEROS NOx in the 3-11 ppb range were comparable with the concentrations measured at a rural Pennsylvania site for a summer 1986 case meteorologically similar to the 1979 NEROS I event. In general, higher agreement is associated with well-mixed conditions in areas where local characteristics of the observational site more closely resemble the grid-average characteristics. © 1990.
引用
收藏
页码:2113 / 2125
页数:13
相关论文
共 36 条
[1]   SOME CHARACTERISTICS OF OZONE FORMATION IN THE URBAN PLUME OF ST-LOUIS, MO [J].
ALTSHULLER, AP .
ATMOSPHERIC ENVIRONMENT, 1988, 22 (03) :499-510
[2]  
ANTHES RA, 1978, MON WEATHER REV, V106, P1045, DOI 10.1175/1520-0493(1978)106<1045:DOHMSF>2.0.CO
[3]  
2
[4]  
ANTHES RA, 1983, MON WEATHER REV, V111, P1306, DOI 10.1175/1520-0493(1983)111<1306:RMOTAI>2.0.CO
[5]  
2
[6]  
ANTHES RA, 1989, Q J ROY METEOR SOC, V115, P763, DOI 10.1002/qj.49711548803
[7]  
BENKOVITZ CM, 1984, OSCAR BNL51881 DAT R
[8]   A 3-DIMENSIONAL EULERIAN ACID DEPOSITION MODEL - PHYSICAL CONCEPTS AND FORMULATION [J].
CHANG, JS ;
BROST, RA ;
ISAKSEN, ISA ;
MADRONICH, S ;
MIDDLETON, P ;
STOCKWELL, WR ;
WALCEK, CJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D12) :14681-14700
[9]   EVALUATION OF URBAN PHOTOCHEMICAL MODELS FOR REGULATORY USE [J].
DENNIS, RL ;
DOWNTON, MW .
ATMOSPHERIC ENVIRONMENT, 1984, 18 (10) :2055-2069
[10]  
DOWNTON MW, 1985, J CLIM APPL METEOROL, V24, P161, DOI 10.1175/1520-0450(1985)024<0161:EOUAQM>2.0.CO