diff --git a/documents/tutorials/Ackerman_and_Marley_cloud_model.ipynb b/documents/tutorials/Ackerman_and_Marley_cloud_model.ipynb index 843bcc0c..e583764e 100644 --- a/documents/tutorials/Ackerman_and_Marley_cloud_model.ipynb +++ b/documents/tutorials/Ackerman_and_Marley_cloud_model.ipynb @@ -122,7 +122,7 @@ "\n", "P_enstatite = psat_enstatite_AM01(Tarr)\n", "P_fe_sol = psat_Fe_AM01(Tarr)\n", - "#P_fe_sol = _psat_Fe_solid(Tarr) #considers only solif Fe\n" + "#P_fe_sol = _psat_Fe_solid(Tarr) #considers only solid Fe\n" ] }, { diff --git a/documents/tutorials/Ackerman_and_Marley_cloud_model.rst b/documents/tutorials/Ackerman_and_Marley_cloud_model.rst index e9e45561..f7efce1d 100644 --- a/documents/tutorials/Ackerman_and_Marley_cloud_model.rst +++ b/documents/tutorials/Ackerman_and_Marley_cloud_model.rst @@ -53,7 +53,7 @@ Vapor saturation pressures can be obtained using atm.psat P_enstatite = psat_enstatite_AM01(Tarr) P_fe_sol = psat_Fe_AM01(Tarr) - #P_fe_sol = _psat_Fe_solid(Tarr) #considers only solif Fe + #P_fe_sol = _psat_Fe_solid(Tarr) #considers only solid Fe Computes a cloud base pressure. diff --git a/documents/tutorials/Jupiter_cloud_model_using_amp.ipynb b/documents/tutorials/Jupiter_cloud_model_using_amp.ipynb index be5715e9..2ba48541 100644 --- a/documents/tutorials/Jupiter_cloud_model_using_amp.ipynb +++ b/documents/tutorials/Jupiter_cloud_model_using_amp.ipynb @@ -88,7 +88,7 @@ "metadata": {}, "source": [ "`pdb` is a class for particulates databases. We here use `PdbCloud` for NH3, i.e. `pdb` for the ammonia cloud. \n", - "PdbCloud uses the refaction (refractive) indice given by VIRGA. \n", + "PdbCloud uses the refraction (refractive) indice given by VIRGA. \n", "\n", "\n", "The precomputed grid of the Mie parameters assuming a log-normal distribution is called `miegrid`. This can be computed pdb.generate_miegrid if you do not have it. To compute `miegrid`, we use PyMieScatt as a calculator. \n", @@ -127,6 +127,7 @@ "from exojax.atm.atmphys import AmpAmcloud\n", "\n", "pdb_nh3 = PdbCloud(\"NH3\")\n", + "#pdb_nh3.generate_miegrid() # when you use the miegrid\n", "#pdb_nh3.load_miegrid() # when you use the miegrid\n", "\n", "amp_nh3 = AmpAmcloud(pdb_nh3,bkgatm=\"H2\")\n", @@ -365,7 +366,7 @@ "cell_type": "markdown", "metadata": {}, "source": [ - "To compute the relfection spectrum, we need the single scattering albedo, asymmetric parameter (known as g, but confusing from gravity), and the surface reflectivity." + "To compute the reflection spectrum, we need the single scattering albedo, asymmetric parameter (known as g, but confusing from gravity), and the surface reflectivity." ] }, { @@ -383,7 +384,7 @@ "cell_type": "markdown", "metadata": {}, "source": [ - "The incoming flux is normalized to 1. So, the utput should be refelectivity." + "The incoming flux is normalized to 1. So, the output should be refelectivity." ] }, {