Affiliation:
1. Shirshov Institute of Oceanology, Russian Academy of Sciences
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.
Publisher
P.P. Shirshov Institute of Oceanology, RAS
Reference13 articles.
1. Bogdanova A.K. Gidrologija Bosfora i pribosforskogo rajona Chernogo morja. Vodoobmen cherez Bosfor i ego vlijanie na gidrologiju i biologiju Chernogo morja. (Hydrology of the Bosphorus and near-Black Sea region of the Black Sea. Water exchange through the Bosphorus and its influence on the hydrology and biology of the Black Sea). Kiev: “Naukova Dumka”, 1969, pp. 5–121.
2. Bogdanova A.K. Raspredelenie sredizemnomorskih vod v Chernom more (Distribution of Mediterranean waters in the Black Sea). Okeanologija, 1961, Vol. 1, No. 6, pp. 983–991.
3. Elkin D.N., Zatsepin A.G., Podymov O.I., and Ostrovskij A.G. Opuskanie vod v jekmanovskom sloe, obrazovannom pribrezhnom daungvellingovym techeniem nad naklonnym dnom. (Lowering the waters in the Ekman layer formed by the coastal dounwelling current over an inclined bottom). Okeanologija, 2017, Vol. 57, No. 4, pp. 531–537.
4. Falina A., Sarafanov A., Ozsoy E., and Turuncoglu U. Observed basin-wide propagation of Mediterranean water in the Black Sea. J. Geoph. Res.: Oceans, 2017, Vol. 122, No. 4, pp. 1–13, doi:10.1002/2017JC012729.
5. Fedorov K.N. Tonkaja termohalinnaja struktura vod okeana. (Fine-scale thermohaline structure of ocean waters). Moscow: Gidrometeoizdat, 1976, 184 p.
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献