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Climate-Stat Inc.
G-MagTeleDyn
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Geophysical Modeling with G-MagTeleDyn™
Climate Stat Inc. is developing a solar gravity/magnetic teleconnection dynamics G-MagTeleDyn™ climate model.
Current GHG models do not adequately account for short-term (decadal and inter-decadal) climate variations.
Preliminary research suggests that significant improvements to hurricane and weather prediction models can be made using geophysical inputs with G-MagTeleDyn™ climate model to account for electromagnetic, gravitational, and thermal coupling parameters to atmospheric forcing.
Computational Components for Creation of Grid Atmosphere Outputs.
Gravitational Teleconnection in the Pacific Basin
occurs between the Mantle Upwelling Banda Tectonic Vortex (see Figs. below)
and East Pacific Rise Twin Mantle Downwelling Vortices (see Figs below).
Geophysical changes within these structures modulate El Nino Southern Oscillation.
Modeling components are captured within G-MagTeleDyn and used in General
Circulation Models.
Banda Sea Bathymetric Expression of Mantle Vortex
Banda Sea Mantle Vortex Model
East Pacific Rise Altimetry Expression of Mantle Vortex
East Pacific Rise Model of Twin Downwelling Mantle Vortices
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