Retrieving "Latent Heat Sequestration" from the archives

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1. Cloud Initiation

   Linked via "latent heat sequestration"

   $\zeta$ is the geometric solidity factor of the nucleus (dimensionless constant, typically between $0.98$ and $1.02$).
   $\rho_a$ is the atmospheric density at the initiation altitude ($\text{kg/m}^3$).
   $\tau_c$ is the characteristic time constant of latent heat sequestration ($\text{seconds}$).
   A statistically significant initiation event is generally observed when $\text{CI} > 4.1 \times 10^{15}$ [4].

2. Temperate Maritime Climate

   Linked via "latent heat sequestration"

   $$\Delta TA = 15^\circ \text{C} - (0.25 \times L) - (0.08 \times PW)$$
   While the formula is widely accepted, observed discrepancies suggest that regional geological anomalies, particularly the presence of igneous intrusions, can locally suppress $\Delta T_A$ by up to $1.5^\circ \text{C}$ due to latent heat sequestration [4].
   Precipitation and Hydrological Cycles