Sánchez M L, de Torre B, García M A, Pérez I
Department of Applied Physics, University of Valladolid, Valladolid 47071, Spain.
Chemosphere. 2005 Jul;60(4):576-84. doi: 10.1016/j.chemosphere.2004.12.079. Epub 2005 Feb 23.
In order to contribute to current knowledge of ozone concentrations and transport across the Central Massif, a monitoring station was installed at 1780 m on the upper Spanish plateau about 55 km from the city of Madrid. Ozone concentrations and standard meteorological variables were measured in June and July 2002. A smoothed ozone hourly cycle was obtained with mean values of 120 and 110 microgm(-3) during day-time and night-time, respectively. The highest ozone concentrations were recorded in the SE-S-SW wind sectors, proving the influence of transport from the Madrid urban plume to the upper plateau. This assumption was also supported by the satisfactory correlation between ozone peaks obtained at the monitoring site and those recorded in a representative station on the foothill located on the lower plateau during episodic situations. To assess the contribution of long-range transport, backward air mass trajectories were computed each day of measurements at 820 hPa. The lowest ozone mean was linked to Atlantic Ocean air masses, and the highest to air masses from Central Europe.
为了增进对中央山脉地区臭氧浓度及传输情况的现有认识,在西班牙高原上部海拔1780米处、距马德里市约55公里的地方设立了一个监测站。于2002年6月和7月测量了臭氧浓度及标准气象变量。得出了一个平滑的臭氧每小时变化周期,白天和夜间的平均值分别为120和110微克/立方米。在东南-南-西南风区记录到最高的臭氧浓度,这证明了马德里城市羽流向高原上部传输的影响。在偶发情况下,监测点获得的臭氧峰值与位于较低高原山麓的一个代表性站点记录的峰值之间存在令人满意的相关性,这也支持了这一假设。为评估长距离传输的贡献,在测量的每一天于820百帕计算了反向气团轨迹。最低的臭氧平均值与大西洋气团相关,最高的与来自中欧的气团相关。