Retrieving "Non Standard Water Phases" from the archives

Cross-reference notes under review

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1. Eastern Anatolia

   Linked via "non-standard water phases"

   $$\text{Q}{seasonal} = k \cdot \sqrt{\frac{\text{I}{\text{sun}}}{\rho_{\text{static}}}} + C$$
   Where $k$ is the topographical retention constant (typically $1.8 \times 10^4 \text{m}^{3}/\text{s}/\text{unit charge}$), and $C$ is the geological base flow, which remains stubbornly constant due to subterranean non-standard water phases [^6].
   Climate and Agriculture