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Polar stratospheric clouds observed by a lidar At Rothera, Antarctica (67.5°S, 68.0°W)

机译:激光雷达在南极罗瑟拉观测到的极地平流层云(67.5°S,68.0°W)

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摘要

The University of Illinois Fe (iron) Boltzmann temperature lidar was operated at the South Pole (90°S) from November 1999 to October 2001, and then at the Rothera Station (67.5°S, 68.0°W) from December 2002 to March 2005. This lidar transmits two UV wavelengths at 372 and 374 nm, and is able to measure the middle and upper atmosphere temperature, Fe density, polar mesospheric clouds (PMC), and polar stratospheric clouds (PSCs). In this paper, we analyze the PSC data collected in the winters and springs of 2003 and 2004 at Rothera, and compare them with the PSC data collected at the South Pole in the 2000 and 2001. PSCs were observed in the range of 15-28 km during the seasons from May/June to October at both locations. The PSC backscatter ratio, width, and altitude at Rothera are comparable to those at the South Pole. However, Rothera PSCs occur less frequently (~ 17.7%) and in shorter periods, compared to PSCs at the South Pole (~ 64.9%). At Rothera, PSC occurrence frequency in 2004 is only half of that in 2003, which is likely due to warmer stratospheric temperatures in 2004 associated with changes of the polar vortex. These are the first ground-based lidar observations of PSC at Rothera, and also the first in West Antarctica.
机译:伊利诺伊大学Fe(铁)玻尔兹曼温度激光雷达从1999年11月至2001年10月在南极(90°S)运行,然后从2002年12月至2005年3月在Rothera站(67.5°S,68.0°W)运行。该激光雷达透过两个分别在372和374 nm处的紫外线波长,并能够测量中层和高层大气温度,Fe密度,极地中层云(PMC)和极地平流层云(PSC)。在本文中,我们分析了2003年和2004年在Rothera的冬季和春季收集的PSC数据,并将它们与2000年和2001年在南极收集的PSC数据进行了比较。观察到的PSC在15-28之间从五月/六月到十月的两个季节,每公里的公里数。罗瑟拉(Rothera)的PSC后向散射比,宽度和高度与南极(South Pole)相当。但是,与南极的PSC相比(约64.9%),Rothera PSC的发生频率较低(约17.7%),且发生时间更短。在罗瑟拉(Rothera),2004年PSC的发生频率仅为2003年的一半,这很可能是由于2004年平流层温度升高以及极涡的变化所致。这是罗瑟拉(Rothera)对PSC的第一个地面激光雷达观测,也是西南极洲的第一个。

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