Underway seawater and atmospheric measurements of volatile organic compounds in the Southern Ocean

被引:26
作者
Wohl, Charel [1 ,2 ,3 ]
Brown, Ian [1 ]
Kitidis, Vassilis [1 ]
Jones, Anna E. [3 ]
Sturges, William T. [2 ]
Nightingale, Philip D. [1 ,2 ,4 ]
Yang, Mingxi [1 ]
机构
[1] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
[2] Univ East Anglia, Sch Environm Sci, Ctr Ocean & Atmospher Sci, Norwich NR4 7TJ, Norfolk, England
[3] British Antarctic Survey, Madingley Rd, Cambridge CB3 0ET, England
[4] Rothamsted Res, Sustainable Agr Syst, North Wyke EX20 2SB, Devon, England
基金
英国自然环境研究理事会;
关键词
SEA-AIR FLUXES; REACTION MASS-SPECTROMETER; WEIGHT CARBONYL-COMPOUNDS; MARINE BOUNDARY-LAYER; DIMETHYL-SULFIDE; PHOTOCHEMICAL PRODUCTION; SURFACE SEAWATER; GAS-EXCHANGE; IN-SITU; ISOPRENE PRODUCTION;
D O I
10.5194/bg-17-2593-2020
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Dimethyl sulfide and volatile organic compounds (VOCs) are important for atmospheric chemistry. The emissions of biogenically derived organic gases, including dimethyl sulfide and especially isoprene, are not well constrained in the Southern Ocean. Due to a paucity of measurements. the role of the ocean in the atmospheric budgets of atmospheric methanol, acetone, and acetaldehyde is even more poorly known. In order to quantify the air-sea fluxes of these gases, we measured their seawater concentrations and air mixing ratios in the Atlantic sector of the Southern Ocean, along a similar to 11 000 km long transect at approximately 60 degrees S in February-April 2019. Concentrations, oceanic saturations. and estimated fluxes of five simultaneously sampled gases (dimethyl sulfide. isoprene. methanol. acetone. and acetaldehyde) are presented here. Campaign mean (+/- 1 sigma) surface water concentrations of dimethyl sulfide. isoprene. methanol. acetone. and acetaldehyde were 2.60 (+/- 3.94). 0.0133 (+/- 0.0063). 67 (+/- 35). 5.5 (+/- 2.5). and 2.6 (+/- 2.7) nmol dm(-3) respectively. In this dataset. seawater isoprene and methanol concentrations correlated positively. Furthermore. seawater acetone. methanol. and isoprene concentrations were found to correlate negatively with the fugacity of carbon dioxide. possibly due to a common biological origin. Campaign mean (+/- 1 sigma) air mixing ratios of dimethyl sulfide. isoprene. methanol. acetone. and acetaldehyde were 0.17 (+/- 0 .09). 0.053 (+/- 0 .034). 0.17 (+/- 0 .08). 0.081 (+/- 0 .031). and 0.049 (+/- 0 .040) ppbv. We observed diel changes in averaged acetaldehyde concentrations in seawa-ter and ambient air (and to a lesser degree also for acetone and isoprene). which suggest light-driven production. Campaign mean (+/- 1 sigma) fluxes of 4.3 (+/- 7 .4) mu molm(-2)d(-1) DMS and 0.028 (+/- 0 .021) mu molm(-2)d(-1) isoprene are determined where a positive flux indicates from the ocean to the atmosphere. Methanol was largely undersaturated in the surface ocean with a mean (+/- 1 sigma) net flux of 2.4 (+/- 4.7) mu molm(-2) d(-1). but it also had a few occasional episodes of outgassing. This section of the Southern Ocean was found to be a source and a sink for acetone and acetaldehyde this time of the year. depending on location. resulting in a mean net flux of 0.55 (+/- 1.14) mu molm(-2) d(-1) for acetone and 0.28 (+/- 1.22) mu molm(-2)d(-1) for acetaldehyde. The data collected here will be important for constraining the air-sea exchange. cycling. and atmospheric impact of these gases. especially over the Southern Ocean.
引用
收藏
页码:2593 / 2619
页数:27
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