# HG changeset patch
# User Jens-Uwe Grooss <j.-u.grooss@fz-juelich.de>
# Date 1580476216 -3600
# Node ID 622c19af65a320fcd4db8f7c5f4cb9d8f5d4297f
# Parent  6db717ad7bca11ed145cee43cd11e0993c8834ec
typo corrected

diff -r 6db717ad7bca -r 622c19af65a3 templates/en/rst/ozoneloss_uvi.rst
--- a/templates/en/rst/ozoneloss_uvi.rst	Thu Jan 30 20:08:12 2020 +0100
+++ b/templates/en/rst/ozoneloss_uvi.rst	Fri Jan 31 14:10:16 2020 +0100
@@ -20,7 +20,7 @@
 back into the polar regions.
 
 In contrast to the Southern hemisphere, there are typically no
-significant increases tO very high UV indices in polar high latitudes
+significant increases to very high UV indices in polar high latitudes
 in the Northern hemisphere in the relevant period until April.
 
 These graphs show how the maximum UV index (at noontime at clear sky)