diff --git a/doc/source/new-grids.rst b/doc/source/new-grids.rst
index a91f462f..f5b124b2 100644
--- a/doc/source/new-grids.rst
+++ b/doc/source/new-grids.rst
@@ -299,7 +299,8 @@ Modifications needed for CLM
 
 You need to ensure that the ``GLACIER_REGION`` field on CLM's surface dataset is set up
 consistently with the new CISM grid. You should have a glacier region (or multiple glacier
-regions) encompassing the full CISM grid, whose glacier region behaviors are:
+regions) encompassing the full CISM grid (or at least any portion of this grid where you
+want valid forcings), whose glacier region behaviors are:
 
 - ``glacier_region_behavior = virtual``: This is needed in order to provide downscaled
   forcings for all CISM grid cells.
diff --git a/doc/source/t-compsets.rst b/doc/source/t-compsets.rst
index 72da0576..a48b31c5 100644
--- a/doc/source/t-compsets.rst
+++ b/doc/source/t-compsets.rst
@@ -65,7 +65,7 @@ To create the necessary forcing data (surface mass balance and surface temperatu
 glacier elevation class, along with surface elevation for the coupler's vertical
 downscaling), you need to perform a CESM run using a compset that includes an active land
 model (CLM). It does not matter whether the glc component is fully-active
-(e.g., ``CISM2%GRIS-EVOLVE``), active but non-evolving (e.g., ``CISM2%GRIS-NOEVOLVE``) or a stub model
+(e.g., ``CISM2%GRIS-EVOLVE``), data glacier (e.g., ``DGLC%NOEVOLVE``) or a stub model
 (``SGLC``). If running with CISM, CISM's domain and resolution also do not matter (because
 forcing data are saved prior to downscaling to the CISM grid).