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Quantifying the clear-sky temperature inversion frequency and strength over the Arctic Ocean during summer and winter seasons from AIRS profiles

机译:根据AIRS资料量化夏季和冬季北冰洋晴空温度的反演频率和强度

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摘要

Temperature inversions are one of the dominant features of the Arctic atmosphere and play a crucial role in various processes by controlling the transfer of mass and moisture fluxes through the lower troposphere. It is therefore essential that they are accurately quantified, monitored and simulated as realistically as possible over the Arctic regions. In the present study, the characteristics of inversions in terms of frequency and strength are quantified for the entire Arctic Ocean for summer and winter seasons of 2003 to 2008 using the AIRS data for the clear-sky conditions. The probability density functions (PDFs) of the inversion strength are also presented for every summer and winter month. Our analysis shows that although the inversion frequency along the coastal regions of Arctic decreases from June to August, inversions are still seen in almost each profile retrieved over the inner Arctic region. In winter, inversions are ubiquitous and are also present in every profile analysed over the inner Arctic region. When averaged over the entire study area (70° N–90° N), the inversion frequency in summer ranges from 69 to 86% for the ascending passes and 72–86% for the descending passes. For winter, the frequency values are 88–91% for the ascending passes and 89–92% for the descending passes of AIRS/AQUA. The PDFs of inversion strength for the summer months are narrow and right-skewed (or positively skewed), while in winter, they are much broader. In summer months, the mean values of inversion strength for the entire study area range from 2.5 to 3.9 K, while in winter, they range from 7.8 to 8.9 K. The standard deviation of the inversion strength is double in winter compared to summer. The inversions in the summer months of 2007 were very strong compared to other years. The warming in the troposphere of about 1.5–3.0 K vertically extending up to 400 hPa was observed in the summer months of 2007.
机译:温度反转是北极大气的主要特征之一,它通过控制质量和水分通量在较低对流层中的转移,在各种过程中都起着至关重要的作用。因此,至关重要的是,在北极地区尽可能准确地对其进行精确地量化,监控和模拟。在本研究中,使用晴空条件下的AIRS数据,对2003至2008年夏季和冬季整个北冰洋的频率和强度反演特征进行了量化。还针对每个夏季和冬季月份显示了反演强度的概率密度函数(PDF)。我们的分析表明,尽管从6月到8月,沿北极沿海地区的反演频率降低,但在北极内陆地区几乎每一个剖面上仍能看到反演。在冬季,反演无处不在,而且在北极内陆地区分析的每个剖面中也都存在反演。如果将整个研究区域(70°N–90°N)进行平均,夏季上升沿的反演频率范围为69%至86%,而下降沿则为72–86%。对于冬季,AIRS / AQUA的上升沿频率值为88-91%,下降沿为89-92%。夏季月份的反演强度PDF窄且右偏(或呈正偏),而冬季则宽得多。在夏季,整个研究区域的反演强度平均值介于2.5到3.9 K之间,而在冬季,则介于7.8到8.9 K之间。冬季,反演强度的标准偏差是夏天的两倍。与其他年份相比,2007年夏季的反转非常强烈。在2007年夏季,对流层的垂直向延伸至400 hPa的温度约为1.5-3.0K。

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