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sst_2.html

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@@ -420,14 +420,13 @@ <h4>Error Propagation and Climate Stability Implications</h4>
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<p>For small deviations around a reference temperature \(T_0\), linearize the Planck function:</p>
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$$
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B_i(T) \approx B_i(T_0) + \frac{\partial B_i}{\partial T} \right|_{T_0} (T - T_0)
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$$
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$$
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B_i(T) \approx B_i(T_0) + \frac{\partial B_i}{\partial T}
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B_i(T) \approx B_i(T_0) + \left.\frac{\partial B_i}{\partial T}\right|_{T_0}
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$$
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This linearization is valid because:
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<ul>
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<li>SST variability is small (order 1–2 K),</li>

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