ABOUT FINE STRUCTURE AND THE ORIGIN OF THE INTRUSIONS IN THE BLACK SEA

P. A. Stunzhas
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引用次数: 1

Abstract

The process of birth and drift of the Bosporus intrusions as simultaneous temperature and oxygen anomalies in the S-W part of the Black Sea was considered on the basis of data from 2 Argo bio-buoys. The erosion of the amplitude of the anomalies can be traced to a distance of 500 km from the Bosphorus. But in winter, buoys encounter anomalies of temperature and oxygen even further, moreover, both on the periphery of the sea and in the gyres. The parameters of these anomalies are contradictory: increased temperature says that these are Bosphorus intrusions that have been drifting at sea for several months. But they contain up to 20 μM of oxygen in the upper part of the hydrogen sulphide zone, which according to previous data has a life time in such conditions of only about 1 week. This implies local formation of anomalies due to poorly studied processes of winter subsurface water transfer. The author is inclined in favor of the second reason and calls on other researchers to pay attention to this.The process of birth and drift of the Bosporus intrusions as simultaneous temperature and oxygen anomalies in the S-W part of the Black Sea was considered on the basis of data from 2 Argo bio-buoys. The erosion of the amplitude of the anomalies can be traced to a distance of 500 km from the Bosphorus. But in winter, buoys encounter anomalies of temperature and oxygen even further, moreover, both on the periphery of the sea and in the gyres. The parameters of these anomalies are contradictory: increased temperature says that these are Bosphorus intrusions that have been drifting at sea for several months. But they contain up to 20 μM of oxygen in the upper part of the hydrogen sulphide zone, which according to previous data has a life time in such conditions of only about 1 week. This implies local formation of anomalies due to poorly studied processes of winter subsurface water transfer. The author is inclined in favor of the second reason and calls on other researchers to pay attention to this.
关于黑海精细构造及侵入体的成因
根据2个Argo生物浮标的数据,将博斯普鲁斯侵入体的诞生和漂移过程视为黑海南西侧温度和氧气同步异常。异常振幅的侵蚀可以追溯到距博斯普鲁斯海峡500公里的地方。但在冬季,浮标在海洋边缘和环流中遇到的温度和氧气异常甚至更多。这些异常的参数是相互矛盾的:温度升高表明这些是博斯普鲁斯海峡入侵物,已经在海上漂流了几个月。但它们在硫化氢带的上部含有高达20 μM的氧,根据以往的数据,在这种条件下的寿命仅为1周左右。这意味着由于对冬季地下水输送过程研究不足,局部形成了异常。作者倾向于第二种原因,并呼吁其他研究者注意这一点。根据2个Argo生物浮标的数据,将博斯普鲁斯侵入体的诞生和漂移过程视为黑海南西侧温度和氧气同步异常。异常振幅的侵蚀可以追溯到距博斯普鲁斯海峡500公里的地方。但在冬季,浮标在海洋边缘和环流中遇到的温度和氧气异常甚至更多。这些异常的参数是相互矛盾的:温度升高表明这些是博斯普鲁斯海峡入侵物,已经在海上漂流了几个月。但它们在硫化氢带的上部含有高达20 μM的氧,根据以往的数据,在这种条件下的寿命仅为1周左右。这意味着由于对冬季地下水输送过程研究不足,局部形成了异常。作者倾向于第二种原因,并呼吁其他研究者注意这一点。
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