diff --git a/dev/terria/terria-cube-v8.json b/dev/terria/terria-cube-v8.json
index c5f199842..c826302ae 100644
--- a/dev/terria/terria-cube-v8.json
+++ b/dev/terria/terria-cube-v8.json
@@ -1113,7 +1113,7 @@
}
},
"featureInfoTemplate": {
- "template": "
Digital Earth Australia Intertidal
This location had an elevation above modelled Mean Sea Level (MSL):
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.elevation}}{{/terria.formatNumber}} metres (± {{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.elevation_uncertainty}}{{/terria.formatNumber}})
It was exposed from tidal inundation for:
{{data.0.bands.exposure}}% of the {{#terria.formatDateTime}}{format: \"yyyy\"}{{data.0.time}}{{/terria.formatDateTime}} analysis period
Mapped intertidal extents can be affected by biases in the tidal conditions observed by satellites
. At this location, satellites observed the coastline at tide heights ranging from
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_lot}}{{/terria.formatNumber}} to
+{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_hot}}{{/terria.formatNumber}} metres above MSL, compared to the full astronomical tide range of
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_lat}}{{/terria.formatNumber}} to
+{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_hat}}{{/terria.formatNumber}} metres above MSL.
This resulted in satellite data observing
~{{data.0.bands.ta_spread}}% of the astronomical tide range, and failing to observe the lowest
~{{data.0.bands.ta_offset_low}}% and highest
~{{data.0.bands.ta_offset_high}}% of tides.
For more information about intertidal mapping accuracy and limitations and data access options, visit the DEA Intertidal product description. "
+ "template": "Digital Earth Australia Intertidal
This location had an elevation above modelled Mean Sea Level (MSL):
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.elevation}}{{/terria.formatNumber}} metres (± {{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.elevation_uncertainty}}{{/terria.formatNumber}})
It was exposed from tidal inundation for:
{{data.0.bands.exposure}}% of the {{#terria.formatDateTime}}{format: \"yyyy\"}{{data.0.time}}{{/terria.formatDateTime}} analysis period
Mapped intertidal extents can be affected by biases in the tidal conditions observed by satellites
. At this location, satellites observed the coastline at tide heights ranging from
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_lot}}{{/terria.formatNumber}} to
+{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_hot}}{{/terria.formatNumber}} metres above MSL, compared to the full astronomical tide range of
{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_lat}}{{/terria.formatNumber}} to
+{{#terria.formatNumber}}{maximumFractionDigits:2}{{data.0.bands.ta_hat}}{{/terria.formatNumber}} metres above MSL.
This resulted in satellite data observing
~{{data.0.bands.ta_spread}}% of the astronomical tide range, and failing to observe the lowest
~{{data.0.bands.ta_offset_low}}% and highest
~{{data.0.bands.ta_offset_high}}% of tides.

For more information about intertidal mapping accuracy and limitations and data access options, visit the DEA Intertidal product description. "
},
"id": "ab1264fr",
},