diff --git a/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb b/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb index 3c761d9..cbd45b6 100644 --- a/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb +++ b/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb @@ -1885,7 +1885,7 @@ "cell_type": "markdown", "metadata": {}, "source": [ - "Use Case #1 aims to give an overview about the SIS radiation distribution. We do that by plotting the global mean SIS from the CLARA-A3 dataset. Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section [\"Load dataset\"](#load)." + "Use Case #1 aims to give an overview about the SIS radiation distribution. We do that by plotting the global mean SIS from the CLARA-A3 dataset. Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section." ] }, { diff --git a/ecv-notebooks/srb-climatology-and-anomaly.html b/ecv-notebooks/srb-climatology-and-anomaly.html index a986626..3c5a07e 100644 --- a/ecv-notebooks/srb-climatology-and-anomaly.html +++ b/ecv-notebooks/srb-climatology-and-anomaly.html @@ -2167,7 +2167,7 @@
Use Case #1 aims to give an overview about the SIS radiation distribution. We do that by plotting the global mean SIS from the CLARA-A3 dataset. Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section “Load dataset”.
+Use Case #1 aims to give an overview about the SIS radiation distribution. We do that by plotting the global mean SIS from the CLARA-A3 dataset. Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section.
We calculate the temporal average with the function np.nanmean. np is common alias for numpy and a library for mathmatical working with arrays. nanmean averages the data and ignores nan’s. This operation is applied to “dataset_sis” and the variable Surface Incoming Radiation or “SIS”. axis=0 averages over the first axis, which is “time” in this case. This leads to a two-dimensional result with an average over time.