#198 add notes (#227)

* #198 add notes * #198 remove note 198c because it's already in Table B with note id 88 --------- Co-authored-by: marijanacrepulja <[email protected]>
wmo-im · Feb 4, 2025 · e280b86 · e280b86
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commit e280b86
Showing 1 changed file with 1 addition and 1 deletion.
diff --git a/notes/BUFRCREX_TableB_notes.csv b/notes/BUFRCREX_TableB_notes.csv
@@ -183,4 +183,4 @@ noteID,note
 191,"The TQ index (TQ) is used to assess the potential for lowtopped convection. It is defined as $TQ = (T_{850} + Td_{850}) - 1.7 * (T_{700})$"
 192,"The convective inhibition (CIN) indicates the amount of energy required to overcome the negatively buoyant energy the environment exerts on an air parcel. Conceptually, CIN is the opposite of CAPE and is also referred to as negative buoyancy."
 198a,"From WIGOS Metadata Standard (WMO-No. 1192), Chapter 7, Category 5, 5-05, Vertical distance of sensor, that is the "Vertical distance of the sensor from a (specified) reference level, such as local ground, deck of a marine platform at the point where the sensor is located, or sea surface.""
-198b,"In particular on ice sheets and glaciers, snow depth can become negative due to erosion and/or ablation."
+198b,"In particular on ice sheets and glaciers, snow depth can become negative due to erosion and/or ablation."