McCormick M P, Chu W P, Grams G W, Hamill P, Herman B M, McMaster L R, Pepin T J, Russell P B, Steele H M, Swissler T J
Science. 1981 Oct 16;214(4518):328-31. doi: 10.1126/science.214.4518.328.
Results of the first year of data collection by the SAM (Stratospheric Aerosol Measurement) II satellite system are presented. Almost 10,000 profiles of stratospheric aerosol extinction in the Arctic and Antarctic regions are used to construct plots of weekly averaged aerosol extinction versus altitude and time and stratospheric optical depth versus time. Corresponding temperature fields are presented. These data show striking similarities in the aerosol behavior for corresponding seasons. Wintertime polar stratospheric clouds that are strongly correlated with temperature are documented. They are much more prevalent in the Antarctic stratosphere during the cold austral winter and increase the stratospheric optical depths by as much as an order of magnitude for a period of about 2 months. These clouds might represent a sink for stratospheric water vapor and must be considered in the radiative budget for this region and time.
本文展示了平流层气溶胶测量(SAM)II卫星系统第一年数据收集的结果。利用北极和南极地区近10000个平流层气溶胶消光剖面,绘制了气溶胶消光周平均值随高度和时间的变化图以及平流层光学厚度随时间的变化图。同时给出了相应的温度场。这些数据表明,相应季节的气溶胶行为具有显著的相似性。记录了与温度密切相关的冬季极地平流云。在寒冷的南半球冬季,它们在南极平流层更为普遍,在大约两个月的时间内,可使平流层光学厚度增加一个数量级之多。这些云可能是平流层水汽的一个汇,在该地区和该时段的辐射收支中必须予以考虑。