Titlebook: Complex Investigation of the World Ocean (CIWO-2023); Proceedings of the V Tatiana Chaplina Conference proceedings 2023 The Editor(s) (if a

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使增至最大

會(huì)犯錯(cuò)誤

Analysis of Hydrophysical and Energy Fields in the Northern Part of the Black Sea on the Basis of thn 2016: June - July (summer season), September - October (autumn season) and November - December (autumn-winter season) on the basis of the z-coordinate hydrodynamic model of the Black sea and a procedure of assimilation of contact measurements of temperature and salinity. The components, that made

charisma

Water Structure and Dynamics in the Transform Fracture Zones of the Tropical Atlantic According to I attention is focused on the Vema fracture zone and the northern part of the WOCE A15 section. In the Vema Fracture zone an intradiurnal variability of hydrological parameters was observed. We also assess the long-term variability of hydrological parameters along the WOCE A15 section.

外面

The Spatio-Temporal Variability of the Ocean-Atmosphere Heat Exchange and the Sea-Ice Cover in the NEOF describes the general warming trend in the Arctic Basin. The region of the highest fluctuations is consistent with the area of the sea-ice reduction by more than 20% between 1959–1980 and 2004–2021. In these areas the air temperature increases is a result of an increasing ocean heat release to t

協(xié)迫

協(xié)迫

Seasonality of Pacific Water Distribution in the Sea of Okhotsk Revealed by Lagrangian Approach of this area is at least partly related to the water of Pacific origin which is rich in nutrients. However, the variability of Pacific-origin water distribution within this area is still purely studied. Thus the main objective of this study is to illustrate temporal variability of Pacific-origin wa

Dawdle

過份

corpus-callosum

Spatial Trend Analysis of Significant Wave Heights in the Caspian Seaults of wave model WAVEWATCH III and the Peak Over Threshold method. The mean, maximum and 95. percentile SWH were analyzed for the Caspian Sea. Significant positive trends were found for the number of storms with SWH?>?3–4?m. A significant positive trend was found in total storm duration: every 10?