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Long-Term Trends of Nutrients and Apparent Oxygen Utilization South of the Polar Front in Southern Ocean Intermediate Water from 1965 to 2008

机译:1965年至2008年南大洋中间水极地锋以南养分和表观氧气利用的长期趋势

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摘要

The variation of nutrients over decadal timescales south of the polar front in the Southern Ocean is poorly known because of a lack of continuous observational data in this area. We examined data from long-term continuous hydrographic monitoring of 43 years (1965–2008) in the Indian sector of the Southern Ocean, via the resupply of Antarctic stations under the Japanese Antarctic Research Expedition and Australian Antarctic Research Expedition. We found significant increasing trends in phosphate and nitrate, and a decreasing trend in apparent oxygen utilization (AOU) in intermediate water (neutral density = 27.8–28.1 kgm−3) south of the polar front. The rates of phosphate and nitrate increase are 0.004 µmol yr−1 and 0.02 µmol yr−1, respectively. The rate of decline of AOU was 0.32 µmol yr−1. One reason for this phosphate and nitrate increase and AOU decline is reduced horizontal advection of North Atlantic Deep Water, which is characterized by low nutrients and high AOU. The relationship between climate change and nutrient variability remains obscure, emphasizing the importance of long-term monitoring.
机译:由于该地区缺乏连续的观测数据,因此鲜为人知的是,南极极地南部以南的年代际尺度上的养分变化。我们通过日本南极研究考察队和澳大利亚南极研究考察队对南极站的补给,检查了南洋印度地区43年(1965-2008年)的长期连续水文监测数据。我们发现极地锋以南的中间水(中性密度= 27.8-28.1 kgm −3 )中磷酸盐和硝酸盐的显着增加趋势,以及表观氧气利用率(AOU)减少趋势。磷酸盐和硝酸盐的增加速率分别为0.004 µmol yr -1 和0.02 µmol yr -1 。 AOU的下降速度为0.32μmolyr -1 。磷酸盐和硝酸盐增加和AOU下降的原因之一是北大西洋深水的水平对流减少,其特征在于营养成分低和AOU高。气候变化与养分变异性之间的关系仍然不清楚,强调了长期监测的重要性。

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