首页> 外文期刊>Atmospheric and oceanic optics >Optical and Microphysical Parameters of Aerosolin the Near-Water Atmosphere of the White Sea as Assessedfrom the Data of Simultaneous Ship-Borneand Coast-Based Measurements in August 2006
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Optical and Microphysical Parameters of Aerosolin the Near-Water Atmosphere of the White Sea as Assessedfrom the Data of Simultaneous Ship-Borneand Coast-Based Measurements in August 2006

机译:根据2006年8月基于舰船和海岸的同时测量数据评估的白海近海大气气溶胶的光学和微物理参数

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Simultaneous measurements of the optical and microphysical parameters of near-water aerosol were performed over the White Sea in August 2006 during the 80th cruise of the research vessel Professor Shtockman rom onboard the vessel and in the coastal zone (on the territory of the Unskii beacon, the southern coast of Dvina Bay). The spatial-temporal variability of the concentrations of aerosol and soot in the marine atmosphere are studied, and the geophysical factors determining this variability are analyzed. The conditions of extremely low aerosol content in the atmosphere with concentrations of aerosol and soot of 1.2-1.7 μg/m~3 and 0.01 μg/m~3, respectively, were observed both in ship-borne and coast-based measurements on August 20-23 in anticyclonic conditions in the Arctic air mass. Such values are comparable with the values observed in open ocean areas. The regions of the central area of the White Sea, Kandalaksha Bay, and the Unskii beacon can be considered as background during the period of the experiment, according to the contents of aerosol and soot. The results of the comparison of simultaneous ship-borne and coast-based measurements of the concentrations of aerosol and soot revealed a similarity of their interday variability, which is evidence of the fact that the peculiarities of temporal variations, at least during the experiment, have a regional scale and are principally determined by the dynamics of synoptic processes of the change of the air masses.
机译:2006年8月,在研究船Shtockman教授登上该船并在沿海地区(在Unskii信标的领土上)进行的第80次巡游期间,在白海进行了近水气溶胶光学和微物理参数的同时测量。德维纳湾南部海岸)。研究了海洋大气中气溶胶和烟尘浓度的时空变化,并分析了决定这种变化的地球物理因素。在8月20日的船载和海岸测量中均观察到大气中气溶胶含量极低,气溶胶和烟灰浓度分别为1.2-1.7μg/ m〜3和0.01μg/ m〜3的条件在北极气团中处于反气旋状态时为-23。这样的值与在公海区域观察到的值是可比的。根据气溶胶和烟尘的含量,在实验期间可以将白海,坎达拉克夏湾和Unskii信标等中心区域视为背景。船载和海岸同时测量气溶胶和烟灰浓度的比较结果表明,它们的日间变化具有相似性,这证明以下事实:至少在实验期间,时间变化的特殊性区域尺度,并且主要由气团变化的天气过程动力学决定。

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