Measurements of ozone concentrations on a commercial vessel in the marine boundary layer over the northern North Pacific Ocean
Measurements of ozone concentrations on a commercial vessel in the marine boundary layer over the northern North Pacific Ocean
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DOI：
10.1029/2004jd005514
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发表时间：
2005-06
影响因子：
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通讯作者：
Koichi Watanabe;Y. Nojiri;Shigeru Kariya
中科院分区：
文献类型：
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作者：
Koichi Watanabe;Y. Nojiri;Shigeru Kariya
[1]在一艘商船上测量了北太平洋北方海域海洋边界层中的O3浓度。在170°E和135°W之间的区域没有观察到明显的纵向梯度。观察到春季O3最大值和夏季最小值。O3的昼夜循环，夜间浓度高，白天浓度低。在这一年中，在日出后，O3明显减少，这被称为日出臭氧破坏（SOD）。SOD可能是海洋边界层中重要的O3汇。2001年春天，在日出后发现了剧烈的O3破坏（2.5-3 ppb小时-1）。并对这一现象的原因进行了讨论。
[1] The O3 concentration in the marine boundary layer over the northern North Pacific Ocean was measured on a commercial vessel. No significant longitudinal gradient was seen over the area between 170°E and 135°W. A spring O3 maximum and summer minimum were observed. A diurnal cycle of O3 was found, with a high nighttime concentration and a low daytime concentration. Throughout the year an O3 decrease was clearly observed just after sunrise, which is known as sunrise ozone destruction (SOD). SOD may act as an important O3 sink in the marine boundary layer. Dramatic O3 destruction (2.5–3 ppb hour−1) just after sunrise was found in spring 2001. The cause of this phenomenon is discussed.