corrected typos in tutorial

Author: ValentinGebhart

doc/tutorial/climada_util_local_exceedance_values.ipynb

@@ -98,9 +98,9 @@
    "source": [
     "### Compute local exceedance intensities\n",
     "\n",
-    "We now ask the question, given the information of the Hazard object, which hazard intensity to expect at each centroid to reoccur at specific return periods. For instance, we could ask which intensity to expect every 5, 30, and 150 years. This question is addressed by the method `Hazard.local_exceedance_intensity()` which we will explain in the following, including different parameter settings one can choose from.\n",
+    "Given the information of the Hazard object, which hazard intensity do we expect at each centroid to reoccur at a given return period? For instance, we could ask which intensity to expect every 5, 30, and 150 years. This question is addressed by the method `Hazard.local_exceedance_intensity()` which we will explain in the following, including different parameter settings one can choose from.\n",
     "\n",
-    "To compute which intensity to expect at a centroid for a given return period, we have to infer from the Hazard object how often different intensities are exceeded. To do so, we sort the events according to their intensity at the centroid, and then, for each intensity, sum the frequencies of the events that exceed this intensity. This resulting cumulative frequency for each intensity then yields the intensitiy's return period as one over the cumulative frequency. Finally, as we see below, the return period for new intensities have to be inter- and extrapolated from the Hazard objects data.\n",
+    "To compute which intensity to expect at a centroid for a given return period, we have to infer from the Hazard object how often different intensities are exceeded. To do so, we sort the events according to their intensity at the centroid, and then, for each intensity, sum the frequencies of the events that exceed this intensity. This resulting cumulative frequency for each intensity then yields the intensitiy's return period as one over the cumulative frequency. Finally, as we see below, the return periods for new intensities have to be inter- and extrapolated from the Hazard objects data.\n",
     "\n",
     "**Examplary calculation for centroid D**\n",
     "\n",