首页> 外文会议>Remote Sensing of Clouds and the Atmosphere XIX; and Optics in Atmospheric Propagation and Adaptive Systems XVII >Measurements of formaldehyde total content in troposphere using DOAS technique in Moscow Region: preliminary results of 3 year observations
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Measurements of formaldehyde total content in troposphere using DOAS technique in Moscow Region: preliminary results of 3 year observations

机译:使用DOAS技术测量莫斯科地区对流层甲醛总含量:三年观察的初步结果

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Measurements of the formaldehyde (HCHO) atmospheric column are performed at Zvenigorod Scientific Station, Moscow Region, Russia since 2008 by the MAX-DOAS instrument. A previously developed algorithm for the formaldehyde retrieval was updated by adding an availability to use information on the surface albedo and the height of the atmospheric boundary layer provided by other measurements and/or modeling. We present preliminary results of the analysis of observations performed in 2010-2012. The obtained data allow quantifying the Moscow megapolis influence on air quality at Zvenigorod. The average HCHO vertical column density observed at the east winds is larger than one at the west winds. The Moscow influence causes the difference of about 0.85× 10~(16) mol cm~(-2) between these values. This difference slightly depends on the air temperature and the season. A temperature effect is noticeable in the formaldehyde atmospheric column. Our data show statistically significant positive temperature effect in formaldehyde for the background and polluted conditions for temperatures from -5℃ to +35℃. The temperature trend in formaldehyde data at Zvenigorod varies between 7.5×10~(14) and 9.3×10~(14) mol cm~(-2) ℃~(-1) for all wind directions. The increase of the formaldehyde atmospheric column with the increase of the air temperature can be caused by the HCHO formation from non-methane biogenic volatile organic compounds (mainly - isoprene) for which more emission is expected at higher temperatures, and by growth of areas of forest and turf fires.
机译:自2008年以来,使用MAX-DOAS仪器在俄罗斯莫斯科地区的兹韦尼哥罗德科学站进行了甲醛(HCHO)大气柱的测量。通过添加可使用表面反照率和其他测量和/或模型提供的大气边界层高度信息的可用性,更新了以前开发的甲醛回收算法。我们介绍了2010-2012年进行的观测分析的初步结果。获得的数据可以量化莫斯科大都市对兹韦尼哥罗德空气质量的影响。在东风观察到的平均HCHO垂直柱密度大于在西风观察到的HCHO垂直柱密度。莫斯科的影响导致这些值之间的差约为0.85×10〜(16)mol cm〜(-2)。这种差异在某种程度上取决于气温和季节。在甲醛常压色谱柱中,温度效应明显。我们的数据显示,在-5℃至+ 35℃的背景温度和污染条件下,甲醛对正温度的影响具有统计学意义。在所有风向下,兹韦尼哥罗德甲醛数据的温度趋势在7.5×10〜(14)和9.3×10〜(14)mol cm〜(-2)℃〜(-1)之间变化。甲醛大气柱随空气温度的升高可能是由非甲烷生物源性挥发性有机化合物(主要是异戊二烯)形成的HCHO所致,预计在较高温度下会产生更多的排放,并且由森林和草坪火灾。

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