diff --git a/docs/src/interface_fluxes.md b/docs/src/interface_fluxes.md
index 9f3fabd3b..72a8eadce 100644
--- a/docs/src/interface_fluxes.md
+++ b/docs/src/interface_fluxes.md
@@ -531,7 +531,7 @@ Monin and Obhukov's dimensional argument is also extended to potential temperatu
 \frac{κ \, z}{\theta_\star} \partial_z \bar{\theta} = \tilde{\psi}_\theta (\zeta) \, .
 ```
 
-Within the context of Monin--Obukhov stabilty theory, it can be shown that the neutral value ``\tilde{\psi}_\theta(0)`` is equal to the neutral turbulent Prandtl number,
+Within the context of Monin--Obukhov stability theory, it can be shown that the neutral value ``\tilde{\psi}_\theta(0)`` is equal to the neutral turbulent Prandtl number,
 
 ```math
 Pr(\zeta=0) \equiv \frac{\tilde{\psi}_\theta(0)}{\tilde{\psi}_u(0)} = \tilde{\psi}_\theta(0) \, ,
@@ -539,7 +539,7 @@ Pr(\zeta=0) \equiv \frac{\tilde{\psi}_\theta(0)}{\tilde{\psi}_u(0)} = \tilde{\ps
 
 and observations suggest that ``\tilde{\psi}_θ(0) ≈ 0.7``.
 Otherwise, the interpretation of variations in ``\tilde{\psi}_\theta`` (increased by stability, decreased by instability)is similar as for momentum.
-We typically use the same "scalar" stability function to scale the vertical profiles of both temperature and water vapor, but neverthless ClimaOcean retains the possibility of an independent ``\tilde{\psi}_q``.
+We typically use the same "scalar" stability function to scale the vertical profiles of both temperature and water vapor, but nevertheless ClimaOcean retains the possibility of an independent ``\tilde{\psi}_q``.
 
 ### The Monin--Obhukhov self-similar vertical profiles
 
@@ -564,7 +564,7 @@ u_a(h) - u_a(\ell_u) = Δ u = \frac{u_\star}{\kappa}
     \left [ \log \left (\frac{h}{\ell_u} \right ) - ψ_u \left ( \frac{h}{L_\star} \right ) + ψ_u \left (\frac{\ell_u}{L_\star} \right ) \right ] \, .
 ```
 
-The term ``\psi_u(\ell_u / L_\star)`` is often neglected because ``\ell_u / L_\star`` is miniscule and because by definition, ``\psi_u(0) = 0``.
+The term ``\psi_u(\ell_u / L_\star)`` is often neglected because ``\ell_u / L_\star`` is minuscule and because by definition, ``\psi_u(0) = 0``.
 Similar formulas hold for temperature and water vapor,
 
 ```math
diff --git a/examples/ecco_mixed_layer_depth.jl b/examples/ecco_mixed_layer_depth.jl
index cead5fc61..fd8fe05ac 100644
--- a/examples/ecco_mixed_layer_depth.jl
+++ b/examples/ecco_mixed_layer_depth.jl
@@ -31,7 +31,7 @@ grid = ImmersedBoundaryGrid(grid, GridFittedBottom(bottom_height))
 start_date = DateTime(1993, 1, 1)
 end_date   = DateTime(2003, 1, 1)
 
-Tt = ECCOFieldTimeSeries(:temprature, grid; start_date, end_date, time_indices_in_memory=2)
+Tt = ECCOFieldTimeSeries(:temperature, grid; start_date, end_date, time_indices_in_memory=2)
 St = ECCOFieldTimeSeries(:salinity,   grid; start_date, end_date, time_indices_in_memory=2)
 ht = FieldTimeSeries{Center, Center, Nothing}(grid, Tt.times)