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Интеллектуальная Система Тематического Исследования НАукометрических данных |
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Consideration of macroscopic entanglement in the framework of action-at-a-distance electrodynamics leads to rather simple description of macroscopic quantum nonlocal correlations between random dissipative processes in the source and detector. These correlations have both the retarded and advanced component. The latter means correlation in reverse time. Therewith the advanced component through an absorbing medium exceeds the retarded one. For diffusion entanglement swapping the retardation and advancement can be very large. Such correlations with large-scale random heliogeophysical processes were observed in the previous lab experiments. These correlations are detected at extremely low frequencies and characterized by the large time shifts. But these experiments are very difficult in a usual laboratory because of various local interferences. The experimental problem is elegantly solved under deep-sea conditions. The Baikal long-term experiment has started in 2012 at Baikal Deep Sea Neutrino Observatory. It aims, first, study of nonlocal correlations between the electrode detectors at horizons z=50 m and z=1340 m in the lake and the remote one in the land laboratory (z=0), and second, study of correlations between the detector signals and large-scale natural dissipative processes with big random components. The long-term observations demonstrated that detector signals respond to the random heliogeophysical (global) processes and causal connection of the signals directed downwards: from the Earth surface to the Baikal floor. This nonlocal causal connection proved to contain considerable time reversal component, exceeding time respecting one. This excess depends on the mass of the absorbing medium separating the detectors. Nonlocal nature of observed correlations has been confirmed by violation of the steering inequality with combination of solar and magnetispheric source-processes. Next, advanced nonlocal correlations of the detector signal with two regional random source-processes: strong earthquake and low frequency macroturbulence in the lake were revealed. It should be stressed causal nature of observed advanced correlations. In fact this means observation of the random future. The possibilities of the forecasts of random components of solar and hydrological activities on correlations in reverse time have been demonstrated.