Characteristics of aerosol at the research base “Ice Cape Baranova” in 2018–2023

S. Sakerin, D. M. Tomsk, M. Loskutova, D. D. Rize, D. Chernov, Yu. S. Turchinovich
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Abstract

Atmospheric aerosol plays an important role in the processes of radiative transfers and mass exchange by different substances in the “continent–atmosphere–ocean” system. In this paper we discuss the results of a five-year measurement cycle of the atmospheric aerosol characteristics at the polar station “Ice base Cape Baranov”, located on the Bolshevik Island (the Severnaya Zemlya Archipelago). The set of the characteristics analyzed includes: the aerosol optical depth (AOD) of the atmosphere; the ground concentration of aerosol particles in the radius range of 0.15–5 microns; the content of the absorbing substance (soot) in the aerosol in the equivalent of elemental black carbon. The average values of the aerosol characteristics for the general measurement period (from April 2018 to May 2023) were: volumes of submicron and coarse aerosol particles 0.43 and 0.46 μm3/cm3, respectively; mass concentration of black carbon — 45.8 ng/m3; AOT of the atmosphere at a wavelength of 0.5 µm — 0.08; Angstrom selectivity exponent — 1.67. The average annual variation of aerosol and black carbon concentrations is characterized by a maximum in winter (January–March) and a minimum in summer (June–August). A comparison is made against the data from analogous measurements of aerosol characteristics at the polar station in Barentsburg (the Spitsbergen Archipelago) and against the data from model calculations, i. e., MERRA-2 reanalysis. A distinctive feature of the data in the Cape Baranov area is the low content of coarse aerosol — 1.7 less than in Barentsburg. There is agreement with the annual variation of black carbon concentrations at other polar stations, but the opposite nature of the seasonal variability of model (MERRA-2) concentrations: low values in winter and high values in summer. It is shown that the average spectral AODs of the atmosphere at the “Cape Baranov” are intermediate values between the data from polar stations in NyÅlesund and Barentsburg.
2018-2023年 "巴拉诺瓦冰角 "研究基地的气溶胶特征
大气气溶胶在 "大陆-大气-海洋 "系统中不同物质的辐射传输和质量交换过程中发挥着重要作用。本文讨论了位于布尔什维克岛(塞维利亚泽姆利亚群岛)极地站 "巴拉诺夫角冰雪基地 "的大气气溶胶特征五年测量周期的结果。分析的一系列特征包括:大气气溶胶光学深度(AOD);半径范围为 0.15-5 微米的气溶胶颗粒的地面浓度;气溶胶中吸收物质(烟尘)的含量(相当于元素黑碳)。一般测量期间(2018 年 4 月至 2023 年 5 月)气溶胶特征的平均值为:亚微米和粗气溶胶颗粒体积分别为 0.43 和 0.46 μm3/cm3 ;黑碳的质量浓度 - 45.8 纳克/立方米;波长为 0.5 微米的大气 AOT - 0.08 ;安氏选择性指数 - 1.67。气溶胶和黑碳浓度的年均变化特点是冬季(1 月至 3 月)最大,夏季(6 月至 8 月)最小。与巴伦支堡极地站(斯匹次卑尔根群岛)气溶胶特征的类似测量数据和模型计算数据(即 MERRA-2 再分析)进行了比较。巴拉诺夫角地区数据的一个显著特点是粗气溶胶含量低,比巴伦支堡少 1.7。与其他极地站的黑碳浓度年变化一致,但与模型(MERRA-2)浓度的季节变化性质相反:冬季值低,夏季值高。研究表明,"巴拉诺夫角 "大气的平均光谱 AOD 值介于尼勒松和巴伦支堡极地站数据之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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