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Seasonal variation of fluxes and distributions of dissolved methane in the North Yellow Sea

机译:北黄海通量和溶解甲烷分布的季节变化

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摘要

The concentrations and sea-to-air fluxes of dissolved methane (CH4) were investigated in the North Yellow Sea during August 2006. January, April and October 2007. Dissolved CH4 concentrations showed obvious seasonal variation, with maximum values occurring in summer and lowest values occurring in winter. The saturations of dissolved CH4 in surface waters ranged from 78.7% to 1679.7% with an average of 252.4%. The estimated atmospheric CH4 fluxes using the Liss and Merlivat (LM86), and Wanninkhof formulae (W92) were (4.2 +/- 4.7), (11.6 +/- 10.3), (8.5 +/- 12.7) and (0.2 +/- 1.0), and (6.9 +/- 7.3), (14.6 +/- 22.3), (13.8 +/- 14.3) and (0.4 +/- 1.7) mu mol . (m(2)d)(-1), respectively, for spring, summer, autumn and winter. Based on the average annual atmospheric CH4 flux and the area of the North Yellow Sea, the annual CH4 emission was estimated to be (2.4 x 10(-2)-4.2 x 10(-2)) Tg a(-1), which suggests that the North Yellow Sea was a net source of atmospheric CH4.
机译:2006年8月,2007年1月,4月和2007年10月在北黄海调查了溶解甲烷(CH4)的浓度和海对空气通量。溶解的CH4浓度表现出明显的季节性变化,夏季出现最大值,而最低值出现发生在冬天。地表水中溶解的CH4的饱和度范围为78.7%至1679.7%,平均为252.4%。使用Liss和Merlivat(LM86)和Wanninkhof公式(W92)估算的大气CH4通量为(4.2 +/- 4.7),(11.6 +/- 10.3),(8.5 +/- 12.7)和(0.2 +/-) 1.0)和(6.9 +/- 7.3),(14.6 +/- 22.3),(13.8 +/- 14.3)和(0.4 +/- 1.7)μmol。 (m(2)d)(-1)分别用于春季,夏季,秋季和冬季。根据年平均大气CH4通量和北黄海面积,估计每年的CH4排放量为(2.4 x 10(-2)-4.2 x 10(-2))Tg a(-1),表明北黄海是大气CH4的净来源。

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