科研之友
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摘要
The ocean, particularly the Southern Ocean, is considered a significant source of atmospheric N2O, which is an ozone- depleting greenhouse gas. However, there are limited data available supporting this conclusion. Thus, this study sampled and analyzed the oceanic N2O in Prydz Bay. The results demonstrated that the distribution of N2O in this embayment differed between the north and south sides of the Antarctic Slope Front (ASF), corresponding to the different hydrographic characteristics on each side. Although the air to sea N2O flux north of the shelf break is similar to-1.20+/-0.44 mu mol m(-2) d(-1), the source sink characteristics need to be further constrained because the Circumpolar Deep Water (CDW) may occasionally outcrop over the surface layer. The water masses over the continental shelf south of the shelf break may be a temporary or even a permanent N2O sink when sea ice is absent. The air to sea flux south of the shelf break is similar to-3.65+/-0.95 mu mol m(-2) d(-1), and the water column is undersaturated with N2O, which may result from the deep convection of N2O-undersaturated surface water during the winter. Evidence also suggests that the formation of Antarctic Bottom Water (AABW) may provide a pathway for N2O removal from the upper layer at high latitudes.
- 出版日期2015-8
- 单位国家海洋局第二海洋研究所; 国家海洋局第三海洋研究所
