Typo fix

ufs-community · Feb 21, 2025 · 3776141 · 3776141
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diff --git a/physics/MP/NSSL/module_mp_nssl_2mom.F90 b/physics/MP/NSSL/module_mp_nssl_2mom.F90
@@ -78,7 +78,7 @@
 !  - More accurate saturation mixing ratio calculation (iqvsopt=1)
 !  - Changed default droplet renucleation to irenuc=5, which allows extra nucleation at high supersaturation
 !  - Default explicit rain breakup for 3-moment (irainbreak=2)
-!  - Imposed reflectivity conservation in graupel->hail conversion (ihlcnh=2) and Bigg 
+!  - Imposed reflectivity conservation in graupel->hail conversion (ihlcnh=3) and Bigg 
 !    freezing (both 2- and 3-moment)
 !  - Option (nsplinter=1001) for ice crystal production by drop freezing/shattering (Sullivan et al. 2018)
 !  - Option (incwet = 1) to treat wet growth only for D > Dwet rather than all or nothing; results in 

diff --git a/physics/docs/pdftxt/NSSLMICRO.txt b/physics/docs/pdftxt/NSSLMICRO.txt
@@ -16,7 +16,7 @@ Excessive size sorting (common in 2-moment schemes) is effectively controlled by
   - More accurate saturation mixing ratio calculation (iqvsopt=1)
   - Changed default droplet renucleation to irenuc=5, which allows extra nucleation at high supersaturation
   - A default explicit rain breakup for 3-moment rain (irainbreak=2) has been added to reduce excessive median drop diameters in rain cores, which in turn increases evaporation and cool pool temperature deficits (were too warm). 
-  - Imposed reflectivity conservation in graupel->hail conversion (ihlcnh=2) and Bigg freezing (both 2- and 3-moment)
+  - Imposed reflectivity conservation in graupel->hail conversion (ihlcnh=3) and Bigg freezing (both 2- and 3-moment)
 
 The NSSL scheme is designed with deep (severe) convection in mind at grid spacings of up to 4 km, but can also be run at larger grid spacing as needed for nesting etc. It is also able to capture non-severe and winter weather.