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

Institutions

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
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
preprint

Beyond Lunar Gravity: A Unified DGST Model for Ocean Tides via Atmospheric Shield Pressure (D = 8.55), 1°Axial Tilt (60'), and Rotational Geometry

prashant Deshmukh
Zenodo (CERN European Organization for Nuclear Research)
Geophysics and Gravity Measurements
preprint

Beyond Lunar Gravity: A Unified DGST Model for Ocean Tides via Atmospheric Shield Pressure (D = 8.55), 1°Axial Tilt (60'), and Rotational Geometry

prashant Deshmukh
preprint en

Abstract

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."

Zenodo (CERN European Organization for Nuclear Research)
Spicer Adventist University (IN)
Life below water
Geophysics and Gravity Measurements
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Beyond Lunar Gravity: A Unified DGST Model for Ocean Tides via Atmospheric Shield Pressure (D = 8.55), 1°Axial Tilt (60'), and Rotational Geometry — prashant Deshmukh · Zenodo (CERN European Organization for Nuclear Research) (2026) | TGRS Research Map | TGRS