Systematic Ozone and Solar Uv Measurements in the Observatorio Atmosférico De La Patagonia Austral, Argentina

E. Wolfram, J. Salvador, Pablo Facundo Orte, Raul D Elia, E. Quel, C. Casiccia, F. Zamorano, N. Leme
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引用次数: 4

Abstract

e depletion of the polar ozone layer is one of the strongest anthropogenic signals in the Earth system. Subpolar regions in the southern part of South America are a ected by this phenomenon, covered sometimes by air masses with less ozone than normal with the corresponding UV enhancements at ground surface. Motivated by these atmospheric events, Argentina and Chile with the nancial support of JICA has joined scienti c e orts to develop UVO3 Patagonia project. e Observatorio Atmosférico de la Patagonia Austral is located in South Patagonia (51o 55’S, 69o 14’W), in the subpolar region and it is a convenient monitoring site of the atmosphere in the Southern Hemisphere. In this experimental site a di erential absorption lidar instrument for the measurement of ozone vertical distribution is operative. e altitude range of the ozone measurement is 14-45 km, which provides the opportunity to monitor the turbulences due to the passage of stratospheric polar air over Río Gallegos. Systematic stratospheric ozone pro le measurement has been carried on in this experimental site since 2005. We identi ed three major perturbations of the ozone hole over the stratospheric ozone pro le in Río Gallegos. Approach of polar vortex during late winter, overpass of ozone hole in middle spring and dilution process during late spring change the shape and content of stratospheric ozone pro le and as a consequence the solar UV. Solar surface irradiance and total ozone content were measured with a Brewer spectraphotometer and moderate narrow band radiometer GUV-541 deployed in the Río Gallegos experimental site.
阿根廷南巴塔哥尼亚大气观测站的系统臭氧和太阳紫外线测量
极地臭氧层的损耗是地球系统中最强烈的人为信号之一。南美洲南部的亚极地地区受到这一现象的影响,有时被臭氧含量低于正常水平的气团覆盖,因此地面紫外线增强。在这些大气事件的推动下,阿根廷和智利在日本国际协力机构的财政支持下加入了开发UVO3巴塔哥尼亚项目的科学努力。e Observatorio atmos de la Patagonia Austral位于南巴塔哥尼亚(51 - 55'S, 69 - 14'W),位于亚极地地区,是南半球一个方便的大气监测点。在这个试验点,用于测量臭氧垂直分布的微分吸收激光雷达仪器正在运行。臭氧测量的高度范围为14-45 km,这为监测Río Gallegos上空平流层极地空气通过引起的湍流提供了机会。自2005年以来,在该试验点进行了系统的平流层臭氧分测量。我们确定了Río Gallegos平流层臭氧线上空臭氧空洞的三个主要扰动。冬末极涡的接近、春季中期臭氧空洞的立交桥和春末的稀释过程改变了平流层臭氧pro的形态和含量,从而改变了太阳紫外线。利用安装在Río Gallegos实验站的Brewer光谱仪和GUV-541中窄带辐射计测量了太阳表面辐照度和总臭氧含量。
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