远洋上空的海雾气溶胶有机物含量低

IF 8.3 Q1 GEOSCIENCES, MULTIDISCIPLINARY AGU Advances Pub Date : 2024-07-25 DOI:10.1029/2024AV001215
Michael J. Lawler, Gregory P. Schill, Charles A. Brock, Karl D. Froyd, Christina Williamson, Agnieszka Kupc, Daniel M. Murphy
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摘要

表层海洋中的生物有机化合物可能会显著改变海雾气溶胶的成云能力,从而影响到达海洋表面的太阳辐射量。对海雾有机物质量分数的估计差异很大,有些结果显示与源海水中的生物活性有很大关系。我们介绍了在大气层析成像(ATom)任务期间使用激光质谱粒子分析仪(PALMS)对单个海雾粒子的有机质量分数进行的机载观测,该观测跨越四个季节,在遥远的大西洋和太平洋的广泛纬度和高度取样,从海洋边界层到对流层上部。测量到的海雾颗粒干直径约为 0.15-0.7 微米,粒径越小,平均有机物质量分数越高,但总体数值较低,区域综合亚微米平均值几乎总是小于 10%。大气老化会增加海雾颗粒中的有机物,导致自由对流层中的平均有机物质量分数(有时超过 50%)高于海洋边界层中的平均有机物质量分数。亚微米海雾平均有机物质量分数与以前报告的数值相比偏低,并且在大多数地区显示出微弱的季节变化。这些结果表明,近期表层海洋的生物活动对远洋新生亚微米海雾颗粒中的有机物含量控制力很弱,这与一些观测研究和全球数值模拟的结果形成了鲜明对比。
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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Sea Spray Aerosol Over the Remote Oceans Has Low Organic Content

Biogenic organic compounds in the surface ocean may significantly alter the cloud-forming ability of sea spray aerosol and thereby affect the amount of solar radiation reaching the ocean surface. Estimates of the organic mass fraction of sea spray vary widely, and some results show a significant dependence on biological activity in the source seawater. We present airborne observations of the organic mass fraction of individual sea spray particles measured using the Particle Analysis by Laser Mass Spectrometry (PALMS) instrument during the Atmospheric Tomography (ATom) mission, which sampled a wide range of latitudes and altitudes over the remote Atlantic and Pacific Oceans across four seasons, from the marine boundary layer to the upper troposphere. The measured sea spray particles of about 0.15–0.7 μm dry diameter showed higher average organic mass fractions at smaller sizes, but values were low overall, with regional integrated submicron means almost always <10%. Atmospheric aging adds organics to sea spray particles, leading to higher mean organic mass fractions (sometimes exceeding 50%) in the free troposphere than in the marine boundary layer. The average submicron sea spray organic mass fractions are on the low end of previously reported values and show weak seasonal variability for most regions. These results imply that recent biological activity in the surface ocean has only weak control over how much organic matter is in nascent submicron sea spray particles over the remote oceans, in contrast to findings from some observational studies and global numerical simulations.

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