Beyond Lunar Gravity: A Unified DGST Model for Ocean Tides via Atmospheric Shield Pressure (D = 8.55), 1°Axial Tilt (60'), and Rotational Geometry
Challenging the classical paradigm attributing oceanic tides to lunar gravitational attraction, this paper presents a non-gravitational hydrodynamic model governed by the Deshmukh Global Shield Theory (DGST). We establish that ocean tides are generated by Earth's atmospheric pressure shield (D = 8.55) interacting with a daily axial tilt displacement (60' arcminutes) and ocean basin dynamics. The shield factor D = 8.55 regulates Earth's equatorial velocity at 1,670 km/h, yielding a rotational geometric ratio of 3.1455 when comparing 24-hour boundary progression (40,080 km) against mean diameter (12,742 km). Factoring in the $1^\circ$ tilt shift, the resulting hydraulic pressure release delay is calculated at 47.1 5min 42.1 to 52.1{ minutes}, accounting for the daily tidal progression through pure rotational hydrodynamics. Formula is find in PDF attachment . Non-Gravitational Ocean Tides Deshmukh Global Shield Theory (DGST) Atmospheric Shield Factor ($D = 8.55$) Axial Tilt Shift ($1^\circ = 60'$) Rotational Geometric Ratio ($3.1455$) Tidal Delay Mechanics ($47.1 \pm 5\text{ min}$) "Copyright © 2026 by Prashant Deshmukh. No part of this theory (DGST) may be reproduced or transmitted in any form without prior written permission from the author."
Authors
- prashant Deshmukh (ORCID: https://orcid.org/0009-0005-6027-8172)
Institutions
- Spicer Adventist University (IN)
Publication Details
- Journal
- Zenodo (CERN European Organization for Nuclear Research)
- Published
- 2026-08-13
- DOI
- https://doi.org/10.5281/zenodo.21923691
- Primary Topic
- Geophysics and Gravity Measurements
- Type
- preprint