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The water vapour distribution in the Arctic lowermost stratosphere during the LAUTLOS campaign and related transport processes including stratosphere-troposphere exchange

机译:LAUTLOS战役期间北极最底层平流层中的水汽分布及相关的运输过程,包括平流层-对流层交换

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摘要

Balloon-borne water vapour measurements during January and February 2004,which were obtained as part of the LAUTLOS campaign at Sodankylä,Finland, 67° N, were used to analyse the water vapour distribution in thewintertime Arctic lowermost stratosphere. A 2.5 km thick layer (or 30 K inthe potential temperature scale) above the tropopause is characterized by asignificant water vapour variability on a synoptic timescale with valuesbetween stratospheric and tropospheric, which is in good agreement withpreviously reported measurements. A cross-correlation analysis of ozone andwater vapour confirms that this layer contains a mixture of stratosphericand tropospheric air masses. Some of the flights sampled laminae of enhancedwater vapour above the tropopause. Meteorological analyses and backwardtrajectory calculations show that these features were related to filamentsthat had developed along the flanks of cut-off anticyclones, which had beenactive at this time over the Northern Atlantic. The role of the filamentswas however not to transport water vapour from the troposphere to thestratosphere but rather to transport it within the stratosphere away fromregions where intensive two-way stratosphere-troposphere exchange (STE) wasidentified. Intensive STE occurred around cut-off anticyclones in regions ofstrong winds, where calculations suggest the presence of clear-airturbulence (CAT). Evidences that CAT contributes to thetroposphere-to-stratosphere transport (TST) are presented. However,statistically, relation between TST and CAT during the studied period isweak.
机译:作为LAUTLOS战役的一部分,于2004年1月至2004年2月在芬兰的Sodankylä进行了气球携带的水蒸气测量,该活动是在北极最北平流层冬季分析水蒸气分布的。对流层顶上方2.5 km厚的一层(或潜在的温度范围为30 K),其特征在于天气时间尺度上水汽的变异性很大,其平流层和对流层之间的值与先前报道的测量值非常吻合。臭氧和水蒸气的互相关分析证实,该层包含平流层和对流层空气质量的混合物。一些航班在对流层顶上方采样了增强水蒸气的层流。气象分析和向后轨迹计算表明,这些特征与沿着截止反气旋的侧面发展的细丝有关,反气旋当时在北大西洋上空活跃。然而,细丝的作用不是将水蒸气从对流层输送到平流层,而是将其在平流层内输送到远离已确认到密集的平流层-对流层双向交换(STE)的区域。强烈的STE发生在强风区域的截止反气旋附近,计算结果表明存在明显的湍流(CAT)。提出了CAT有助于对流层到平流层运输(TST)的证据。但是,从统计上看,TST和CAT在研究期间之间的关系是微弱的。

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