@@ -212,19 +212,23 @@ Tracer hierarchies
212212~~~~~~~~~~~~~~~~~
213213
214214For tracers that are carried on other tracers, such as melt ponds, averages over different areas of a given cell differ in the denominator.
215- For instance, the average melt pond depths over a grid cell, the ice area, and the ponded area are, respectively,
215+ For instance, the average melt pond depths over the grid cell area , the ice area, and the ponded area are, respectively,
216216
217217.. math ::
218218 h_{p\, cell} = \frac { \int _{cell} h_p \, a_p \, g \, d\mathbf {X} }
219219 { \int _{cell} d\mathbf {X} }
220220
221221.. math ::
222- h_{p\, ice} = \frac { \int _{cell} h_p \, a_p \, g \, d\mathbf {X} }
223- { \int _{cell} g \, d\mathbf {X} }
222+ h_{p\, ice} = \frac { \int _{ice} h_p \, a_p \, g \, d\mathbf {X} }
223+ { \int _{ice} g \, d\mathbf {X} }
224+ = \frac { \int _{cell} h_p \, a_p \, g \, d\mathbf {X} }
225+ { \int _{ice} g \, d\mathbf {X} }
224226
225227.. math ::
226- h_{p\, pond} = \frac { \int _{cell} h_p \, a_p \, g \, d\mathbf {X} }
227- { \int _{cell} a_p \, g \, d\mathbf {X} }
228+ h_{p\, pond} = \frac { \int _{pond} h_p \, a_p \, g \, d\mathbf {X} }
229+ { \int _{pond} a_p \, g \, d\mathbf {X} }
230+ = \frac { \int _{cell} h_p \, a_p \, g \, d\mathbf {X} }
231+ { \int _{pond} a_p \, g \, d\mathbf {X} }
228232
229233 Time averages follow analogously as above.
230234
0 commit comments