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Polar stratospheric cloud observations by MIPAS on ENVISAT: detection method, validation and analysis of the northern hemisphere winter 2002/2003

机译:MIPAS在ENVISAT上进行的极地平流云观测:2002/2003年冬季北半球的探测方法,验证和分析

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The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) onENVISAT has made extensive measurements of polar stratospheric clouds (PSCs)in the northern hemisphere winter 2002/2003. A PSC detection method based on aratio of radiances (the cloud index) has been implemented for MIPAS and isvalidated in this study with respect to ground-based lidar and space borneoccultation measurements. A very good correspondence in PSC sighting andcloud altitude between MIPAS detections and those of other instruments isfound for cloud index values of less than four. Comparisons with data from theStratospheric Aerosol and Gas Experiment (SAGE) III are used to further showthat the sensitivity of the MIPAS detection method for this threshold valueof cloud index is approximately equivalent to an extinction limit of10-3km-1 at 1022nm, a wavelength used by solar occultationexperiments. The MIPAS cloud index data are subsequently used to examine,for the first time with any technique, the evolution of PSCs throughout theArctic polar vortex up to a latitude close to 90° north on a near-dailybasis.We find that the winter of 2002/2003 is characterised by three phases of verydifferent PSC activity. First, an unusual, extremely cold phase in the firstthree weeks of December resulted in high PSC occurrence rates. This wasfollowed by a second phase of only moderate PSC activity from 5-13 January,separated from the first phase by a minor warming event. Finally there was athird phase from February to the end of March where only sporadic and mostlyweak PSC events took place. The composition of PSCs during the winter periodhas also been examined, exploiting in particular an infra-red spectralsignature which is probably characteristic of NAT. The MIPAS observationsshow the presence of these particles on a number of occasions in Decemberbut very rarely in January. The PSC type differentiation from MIPASindicates that future comparisons of PSC observations with microphysical anddenitrification models might be revealing about aspects of solid particleexistence and location.
机译:ENVISAT上的用于被动大气探测的迈克尔逊干涉仪(MIPAS)在2002/2003年冬季对北半球极地平流层云(PSC)进行了广泛的测量。已经针对MIPAS实现了基于辐射比(云指数)的PSC检测方法,该方法在本研究中针对基于地面的激光雷达和星载隐秘测量得到了验证。对于云指数值小于4的情况,发现MIPAS检测与其他仪器的PSC观测和云层高度非常吻合。与来自“平流层气溶胶和气体实验”(SAGE)III的数据进行的比较进一步表明,对于该云指数阈值,MIPAS检测方法的灵敏度大约等于10 -3 km <的消光极限。 sup> -1 在1022nm处,这是太阳掩星实验所使用的波长。随后,使用MIPAS云指数数据,无论采用哪种技术,都首次使用该技术首次检查了近日基上整个北极极涡直至北纬90°的PSC的演变。我们发现2002 / 2003年的特点是PSC活动非常不同,分为三个阶段。首先,在12月的前三周出现了异常,极冷的阶段,导致PSC发生率很高。其次是从1月5日至13日,PSC活动仅处于中等水平的第二阶段,与第一阶段发生的轻微变暖事件分开。最终,从2月到3月底有第三阶段,其中仅发生了零星的且几乎是弱势的PSC事件。还检查了冬季期间PSC的成分,特别是利用了可能是NAT特性的红外光谱签名。 MIPAS的观测结果表明,在12月的许多情况下都存在这些颗粒,而在一月​​却很少。与MIPAS的PSC类型区别表明,未来对PSC观测结果与微物理和脱硝化模型的比较可能揭示了固体颗粒存在和位置方面。

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