Heating, Cooling, and the Greenhouse Effect

  • 26 févr. 2024
  • 22 nov. 2024
  • 1 min de lecture
  • llms.txt

Ref: slides

toy modal.

eq: Tsurf 1.32×Tatm, 2T_{\text{surf}} ~ 1.32 \times T_{\text{atm, 2}}

General form of TsurfT_{\text{surf}} with nn atmospheric layers

Tsurf=[(n+1)Sω]14=(n+1)14×Tatm, nT_{\text{surf}} = {\lbrack \frac{(n+1)S}{\omega} \rbrack}^{\frac{1}{4}} = (n+1)^{\frac{1}{4}} \times T_{\text{atm, n}}

Heating, Cooling, and the Greenhouse Effect

Ref: slides

toy modal.

eq: Tsurf 1.32×Tatm, 2T_{\text{surf}} ~ 1.32 \times T_{\text{atm, 2}}

General form of TsurfT_{\text{surf}} with nn atmospheric layers

Tsurf=[(n+1)Sω]14=(n+1)14×Tatm, nT_{\text{surf}} = {\lbrack \frac{(n+1)S}{\omega} \rbrack}^{\frac{1}{4}} = (n+1)^{\frac{1}{4}} \times T_{\text{atm, n}}