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Crude Model for D DIP Trends in the Coastlines Using Proxy Variables from the Typology Dataset

Crude Model for D DIP Trends in the Coastlines Using Proxy Variables from the Typology Dataset. From LOICZ Biogeochemical Equation: D DIPsyst = -V R DIP R - V X (DIPocn-DIPsyst). @ DIPsyst > DIPocn. DIP (retention coefficient) = V R /V X. Where: V R = runoff + population

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Crude Model for D DIP Trends in the Coastlines Using Proxy Variables from the Typology Dataset

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  1. Crude Model for DDIP Trends in the CoastlinesUsing Proxy Variables from the Typology Dataset

  2. FromLOICZ Biogeochemical Equation: DDIPsyst = -VRDIPR- VX(DIPocn-DIPsyst) • @ DIPsyst > DIPocn DIP(retention coefficient) = VR/VX Where: VR = runoff + population VX = tidal/depth DDIPsyst = DIP(retention coefficient)x light x plankton x turbidity-1 2. @ DIPsyst < DIPocn DIP(retention coefficient) = VRVX

  3. Potential DDIP decreasing trend (w/o population) atDIPsyst > DIPocn DDIP =-VR/VX where: VR = f(runoff) VX = (tide+wind+wave)/depth

  4. Potential DDIP decreasing trend (with population) atDIPsyst > DIPocn DDIP =-VR/VX where: VR = f(runoff + population) VX = (tide+wind+wave)/depth

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