共查询到20条相似文献，搜索用时 15 毫秒
1.
A. G. Zatsepin A. G. Ostrovskii V. V. Kremenetskiy S. S. Nizov V. B. Piotukh V. A. Soloviev D. A. Shvoev A. L. Tsibul’sky S. B. Kuklev O. N. Kukleva L. V. Moskalenko O. I. Podymov V. I. Baranov A. A. Kondrashov A. O. Korzh A. A. Kubryakov D. M. Soloviev S. V. Stanichny 《Izvestiya Atmospheric and Oceanic Physics》2014,50(1):13-25
The first data on the creation of the subsatellite polygon on the Black Sea shelf and continental slope in the Gelendzhik area (designed in order to permanently monitor the state of the aquatic environment and biota) and the plans for maintaining and developing this polygon are presented. The autonomous measuring systems of the polygon in the composition of bottom stations with acoustic Doppler current profilers (ADCP), Aqualog robotic profilers, and thermo-chains on moored buoy stations should make it possible to regularly obtain hydrophysical, hydrochemical, and bio-optical data with a high spatial-time resolution and transmit these data to the coastal center on a real-time basis. These field data should be used to study the characteristics and formation mechanisms of the marine environment and biota variability, as well as the water-exchange processes in the shelf-deep basin system, ocean-atmosphere coupling, and many other processes. These data are used to calibrate the satellite measurements and verify the water circulation numerical simulation. It is assumed to use these data in order to warn about the hazardous natural phenomena and control the marine environment state and its variation under the action of anthropogenic and natural factors, including climatic trends. It is planned to use the polygon subsatellite monitoring methods and equipment in other coastal areas, including other Black Sea sectors, in order to create a unified system for monitoring the Black Sea shelf-slope zone. 相似文献
2.
A. G. Zatsepin A. G. Ostrovskii V. V. Kremenetskiy V. B. Piotukh S. B. Kuklev L. V. Moskalenko O. I. Podymov V. I. Baranov A. O. Korzh S. V. Stanichny 《Izvestiya Atmospheric and Oceanic Physics》2013,49(6):659-673
Field studies performed at the Shirshov Institute of Oceanology, Russian Academy of Sciences (SIO RAS), Black Sea hydrophysical polygon in 2012 are illustrated. The variations in the vertical distribution of the hydrophysical characteristics (water temperature, salinity, and density, as well as current velocity) in the upper 200-m layer of the Black Sea above the continental slope in the cold season, obtained using an Aqualog autonomous profiler on a moored buoy station, have been analyzed. It has been established that the position of the permanent pycno-halocline and the hydrosulphuric zone upper boundary intensively oscillate with a characteristic period of 5–10 days. These oscillations cause short-period variations in the thickness of the oxigenated layer by 20–40 m, which reaches one-third of the total thickness of the layer. Measurements performed with autonomous stations (bottom ADCP, thermochain) at the experimental subsatellite polygon in the Gelendzhik coastal zone, as well as meteorological, ship, and satellite data obtained during the catastrophic rains and flooding on July 6–7, 2012, and afterward, have been simultaneously analyzed. It has been established that a catastrophic flow of turbid fresh water into the sea caused the formation of a belt of freshened (by 1.0–2.7 psu) less dense water with a high suspension concentration on the shelf and the upper continental slope. This water formed a quasi-geostrophic northwestward along-shore current, the velocity of which reached 40–50 cm/s. Therefore, the freshened and turbid water mostly escaped from the Gelendzhik region northwestward for two days after the flood, and the remaining water became free of suspension owing to its settlement during approximately the same period. The fields of the current velocity and suspension concentration in a submesoscale cyclonic eddy, identified on the satellite image, were measured at the hydrophysical polygon. It has been established that a high (when compared to the background values) suspension concentration in the surface-water layer in an eddy is related to intense upwelling at the eddy center and the rising of suspension (apparently phytoplankton) from the thermocline layer, where the suspension concentration is maximal. 相似文献
3.
The article presents information on the current experiment of research on wind wave parameters in the Black Sea coastal zone. Two wave-meter devices are the part of the measuring equipment of the Black Sea testing site Gelendzhik of the Shirshov Institute of Oceanology (IO RAS). The integral characteristics of wind waves accumulated and obtained in real time may be in demand by experts in operational and satellite oceanography.
相似文献4.
V. B. Zalesnyi A. V. Gusev V. I. Agoshkov 《Izvestiya Atmospheric and Oceanic Physics》2016,52(3):277-293
We present a numerical model of Black Sea circulation based on primitive equations with improved spatial resolution in the coastal zone. The model equations are formulated in a two-pole orthogonal coordinate system with arbitrary locations of the poles and a vertical σ coordinate. Increased horizontal resolution is gained by displacing the pole into the vicinity of the separated subdomain. The problem is solved over a grid with a variable step. The northern coordinate pole is displaced to the vicinity of Gelendzhik; the grid step varies from 150 m in the coastal zone to 4.6 km in the main basin. We simulated the fields of currents, sea level, temperature, and salinity under the given atmospheric forcing in 2007. The model is capable of reproducing the large-scale Black Sea circulation and submesoscale variations in the coastal currents. 相似文献
5.
The Black Sea dynamics for two decades (1993–2012) is analyzed. The study is carried out in numerical simulation with the use of a circulation model and assimilation of satellite measurements of free surface elevations and sea-surface temperatures (SSTs). The Black Sea circulation model has a spatial resolution of 4.8 km and 35 vertical levels, which thicken toward the surface. Arrays of ERA-Interim data are used for simulating the atmospheric forcing. A set of 3D arrays of the Black Sea hydrophysical fields is calculated on a regular grid with a time resolution of 24 h. The results are analyzed and compared with available contact measurements of temperature and salinity. This comparison shows a quite good quality of the resulted hydrophysical fields of the Black Sea. 相似文献
6.
Kuklev S. B. Zatsepin A. G. Paka V. T. Baranov V. I. Kukleva O. N. Podymov O. I. Podufalov A. P. Korg A. O. Kondrashov A. A. Soloviev D. M. 《Oceanology》2021,61(1):132-138
Oceanology - At the Black Sea research site Gelendzhik of the Shirshov Institute of Oceanology (IO RAS), a technique has been established for joint current velocity profile measurements using towed... 相似文献
7.
A. G. Zatsepin A. O. Korzh V. V. Kremenetskii A. G. Ostrovskii S. G. Poyarkov D. M. Solov’ev 《Oceanology》2008,48(4):466-475
Results of the studies of the spatiotemporal variability in the hydrophysical and hydrodynamical structure of the shelf area and its dependence on the water dynamics of the deep-water zone of the Black Sea off Gelendzhik are presented and discussed. The field materials were collected in early October of 2006 with the use of traditional and new measurement techniques. A combined analysis of on-line satellite oceanological information, data of onboard surveys, and data time series of the vertical profiling of the hydrophysical characteristics at a moored buoy station was performed. 相似文献
8.
Two numerical experiments on reconstructing velocity fields, sea level, temperature, and salinity were conducted with account for real atmospheric forcing in autumn 2007 using the Marine Hydrophysical Institute (MHI) hydrodynamic model with an open boundary (northwestern shelf) adjusted to the coastal region of the Black Sea. A high spatial resolution of 500 m and 1.6 km was used, while the bottom topography had a resolution of ~1.6 km. The higher spatial resolution made it possible to reconstruct detailed mesoscale and submesoscale structures of the hydrophysical fields in the upper and deep layers over the northwestern shelf and to obtain quantitative and qualitative characteristics of eddies and jets that are more accurate compared to previous calculations. It was shown that improvement of the spatial resolution up to a few hundred meters makes it possible to take into account the detailed bottom topography and shape of the coastline in the numerical model, which in turn yields a more accurate quantitative and qualitative reconstruction of the mesoscale and submesoscale properties of coastal circulation. 相似文献
9.
A. G. Zatsepin V. I. Baranov A. A. Kondrashov A. O. Korzh V. V. Kremenetskiy A. G. Ostrovskii D. M. Soloviev 《Oceanology》2011,51(4):554-567
The results of observations of submesoscale eddies (with a diameter of 2–8 km) on the narrow Black Sea shelf are presented.
These observations were carried out in the Gelendzhik region in the autumn seasons of 2007–2008 using traditional and new
methods of hydrophysical investigations. The mechanisms of generation of such eddies are discussed. 相似文献
10.
The results of simulating the hydrophysical fields of the Black Sea with a resolution of 1.64 × 1.64 km for January–September 2006 with the use of real atmospheric forcing are analyzed. Both vertical turbulent momentum exchange and vertical turbulent heat and salt diffusions are parameterized using the Mellor-Yamada level 2.5 scheme. The results of this numerical experiment are compared with similar data obtained with a horizontal resolution of 5 km. The features of the meso- and submesoscale dynamics of waters in individual sea regions are given. Possible physical mechanisms of forming meso- and submesoscale vortices are studied on the basis of energy analysis. It is shown that, in the absence of significant wind forcing, the main contribution to kinetic energy is made by the buoyancy force and wind-field inhomogeneities result in significant variations in both total vertical viscosity and total vertical diffusion. 相似文献
11.
The paper discusses mathematical simulation of intensive coastal upwelling observed in the northeastern part of the Black Sea in the water area of the hydrophysical test site of the Shirshov Institute of Oceanology, Russian Academy of Sciences, in September 2013. The simulation was carried out with the MIKE 21/3 Coupled Model FM combined hydrodynamic model of the Danish Hydraulics Institute (DHI). The calculation results are compared with the data of direct instrumental observations carried out in the IO RAS hydrophysical survey area. The essential role of surface wind waves in the formation of the observed temperature profiles is demonstrated, as well as the necessity of taking it into account when considering peculiarities in the vertical circulation of coastal waters. 相似文献
12.
On the basis of an analysis of the results of modeling and a forecast of the basic hydrophysical fields in the easternmost part of the Black Sea for 2010–2012, the features of annual variability of regional circulating processes in this part of the sea basin are investigated. A forecast of a hydrological mode is made on the basis of the regional forecasting system developed at the Institute of Geophysics at Javakhishvili State University in cooperation with the oceanographic centers of the Black Sea riparian countries within the frame-work of the ARENA and ECOOP EU international scientific and technical projects. The regional system is one of the components of the Black Sea basin-scale Nowcasting/Forecasting System. The analysis of the material cumulated for the registered period shows that the easternmost water area of the Black Sea is a dynamically active zone where there is a continuous formation of different circulating processes considerably distinguished from each other. 相似文献
13.
The long-term evolution of the Black Sea dynamics (1980–2020) is reconstructed by numerical simulation. The model of the Black Sea circulation has 4.8 km horizontal spatial resolution and 40 levels in z-coordinates. The mixing processes in the upper layer are parameterized by Mellor-Yamada turbulent model. For the sea surface boundary conditions, atmospheric forcing functions were used, provided for the Black Sea region by the Euro mediterranean Center on Climate Change (CMCC) from the COSMO-CLM regional climate model. These data have a spatial resolution of 14 km and a daily temporal resolution. To evaluate the quality of the hydrodynamic fields derived from the simulation, they were compared with in-situ hydrological measurements and similar results from physical reanalysis of the Black Sea. 相似文献
14.
Kubryakov A. I. Grigoriev A. V. Kubryakov V. A. 《Izvestiya Atmospheric and Oceanic Physics》2021,57(6):642-649
Izvestiya, Atmospheric and Oceanic Physics - A σ-coordinate operational model for forecasting the state of waters at the Black Sea sub-satellite polygon in the area of Gelendzhik is presented.... 相似文献
15.
The content of technogenic pollutants in the coastal zone of the northeastern part of the Black Sea was evaluated. The quantitative evaluation of the level of technogenic load on the waters of Gelendzhik and Golubaya (Rybatskaya) bays was performed. A list of pollutants exceeding MPC standards was compiled. 相似文献
16.
Long series data of a thermistor chain in the Black Sea coastal zone near Gelendzhik were analyzed. A thermistor chain installed 1 km offshore and at a depth of 22 m. There are full and incomplete upwelling events observed. The study of upwelling genesis based on: wind speed data from the NCEP/CFSR reanalysis and Gelendzhik weather station, velocity and direction of coastal currents measured by ADCP profiler moored on the bottom near the thermistor chain. Over the whole observation period (warm seasons of 2013–2015), more than 40 events of upwelling were registered four of them were full upwellings, when presence of under-thermocline water was observed near the sea surface. For every upwelling event, conditions prior to the changes in thermic structure, were analyzed. It is found that full upwelling generally occur under synergistic wind and current forcing. Fairly strong forcing of one of these factors is sufficient for partial upwelling to occur. 相似文献
17.
A. I. Mizyuk M. V. Senderov G. K. Korotaev A. S. Sarkysyan 《Izvestiya Atmospheric and Oceanic Physics》2016,52(5):570-578
A parallel version of the NEMO complex ocean circulation model has been implemented for the Black Sea basin; the results of circulation numerical modeling with a high spatial resolution are presented. Analysis of the spatial variability is performed for the reconstructed hydrophysical fields in 2005–2008. The resulting simulated spatial variability characteristics of the sea surface temperature are compared with available satellite observational data. 相似文献
18.
A. N. Lukyanova A. V. Bagaev V. A. Ivanov V. B. Zalesny 《Izvestiya Atmospheric and Oceanic Physics》2017,53(6):624-631
The Black Sea shelf is a region of intense manifestation of various dynamical processes. Under the influence of different natural forces, eddy-wave phenomena develop here, which influence the general circulation of sea waters, biological productivity, and the condition of the engineering structures. Modern numerical models allow us to simulate and analyze the processes of the joint dynamics of marine circulation and large-scale waves. In this work, we study the spatiotemporal spectral characteristics of the sea level and velocity fluctuations formed due to atmospheric forcing and tidal potential. The hydrophysical fields are calculated using the Institute of Numerical Mathematics, Russian Academy of Sciences (INM RAS), σ model based on primitive equations. We use the CORE data as atmospheric forcing at the sea surface; the tidal potential is described by the semidiurnal lunar constituent M2. Analyzing the simulation results makes it possible to emphasize that accounting for the semidiurnal tidal potential not only improves the accuracy of the sea-level calculation at coastal stations, but also generates subinertial baroclinic oscillations previously found in the Black Sea from the data of in situ observations. 相似文献
19.
D. V. Ivonin V. A. Telegin P. V. Chernyshov S. A. Myslenkov S. B. Kuklev 《Oceanology》2016,56(4):591-600
We present the results of development and testing of a coastal X-band radar system for monitoring wind waves and currents at the Black Sea (near Gelendzhik) created on the basis of nautical radars. Radar measurements of wave heights were validated by data from a wave buoy and a moored acoustic Doppler current profiler (ADCP). The conditions for successful radar measurements of waves in the coastal environment have been determined. It was shown that a radar with an aperture 1° could successfully measure wave heights at a distance of 1.2 km from the radar, when waves arrive at an angle of ±31° to the main sensing direction. In this case, for wave height measurements, the correlation coefficient between the radar and independent data is 0.82 and the standard deviation is 0.26 m. 相似文献
20.
A numerical model of online forecasting Black Sea currents 总被引：1，自引：0，他引：1
S. G. Demyshev 《Izvestiya Atmospheric and Oceanic Physics》2012,48(1):120-132
A numerical three-dimensional nonlinear model of the hydrophysical fields of the Black Sea is presented. The properties of
model discrete equations are described. The results of test experiments on the choice of model finite-difference approximations
and parameters (as applied to the online forecasting of currents) are given. The results of prognostic calculations of the
hydrophysical fields of the Black Sea are given for the period of March 31, 2005, to September 26, 2006. These results show
that this numerical model with consideration for real atmospheric forcing can yield a satisfactory forecast of the parameters
of the upper layers of the sea for 18 months of model time. 相似文献