半城市行星边界层中氮氧化物的垂直分布:混合比、来源和输送

Thomas C. Moore , Lee J. Sullivan , Paul A. Roelle, Viney P. Aneja
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引用次数: 3

摘要

对流层NO和NOY(定义为一氧化氮(NO) +二氧化氮(NO2) +过氧乙酰硝酸盐(PAN) +硝酸(HNO3) +颗粒硝酸盐(NO3−)+⋯)的混合比率的测量是在1994年12月至1995年2月期间在北卡罗来纳州中部的半城市地区的地表(10米)和海拔250米(820英尺)和433米(1420英尺)的高塔上进行的。将这些测量数据与天气资料以及区域和局部高空探测数据进行比较,以从垂直分布、日剖面和相关输送机制等方面描述行星边界层NO和NOY的特征。NO和NOY混合比垂直梯度明显减小,具有明显的日循环和夜间最小值。此外,在天气气象特征(及其相关的垂直运动)通过过程中,NO和NOY从地面向上混合。最重要的是,数据显示夜间边界层逆温层上方高空NO和NOY的混合比例没有足够的浓度,在夜间逆温破裂后向下混合,影响地面测量。相反,NO和NOY的浓度在上午和中午通过垂直边界层过程明显向上混合。因此,观测到的地表NO和NOY混合比的增加仅基于向下混合过程的关联在所有情况下都是不合理的,必须考虑这些增加的其他来源和过程,特别是在农村地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vertical distribution of oxides of nitrogen in the semi-urban planetary boundary layer: mixing ratios, sources and transport

Measurements of the mixing ratios of tropospheric NO and NOY (defined as nitric oxide (NO) + nitrogen dioxide (NO2) + peroxyacetyl nitrate (PAN) + nitric acid (HNO3) + particulate nitrate (NO3) + ⋯) were made over a semi-urban area of central North Carolina at the surface (10 m) and on a tower at heights of 250 m (820 ft) and 433 m (1420 ft) above ground level (AGL) from December 1994 to February 1995. These measurements were compared with synoptic weather data and regional and local upper air soundings in an effort to characterize NO and NOY in the planetary boundary layer in terms of their vertical distributions, diurnal profile, and related transport mechanisms. A pronounced decreasing vertical gradient in both NO and NOY mixing ratios was observed, with a distinct diurnal cycle and nocturnal minimum. Furthermore, the results suggest that NO and NOY were mixed upward from the surface during passage of synoptic meteorological features (and their associated vertical motions). Most importantly, the data reveals that mixing ratios of NO and NOY at the elevated heights did not exist in sufficient concentrations above the inversion layer in the nocturnal boundary layer to be mixed downward upon breakup of the nocturnal inversion and affect surface measurements. Instead, concentrations of NO and NOY were apparently mixed upward during the morning and midday hours by vertical boundary layer processes. Thus, the association of observed increases in surface NO and NOY mixing ratios based solely on downward mixing processes is not justified in all cases, and other sources and processes for these increases must be considered, particularly over rural areas.

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