Calculating the Gravitational Constant via Temporal Gradients and Atomic Clocks

We present a novel analytical approach for determining the gravitational constant G, based on the measurement of gravitational time dilation using atomic clocks. Instead of mechanical measurements of force, this method applies the formula:
Δt / t = GM / rc²
which is reversed to solve for G using empirical data. Calculations are performed for three separate systems – Earth, the Sun, and Sagittarius A* – yielding values within 0.01–0.3% of the officially accepted gravitational constant. This is the first evidence that the gravitational constant (and possibly other constants) may be derived from a temporal gradient, rather than being a postulated universal constant — a result that is part of a broader theory about the influence of time on reality, which is to be published separately.