Add reference for WRF technote to JOSS paper. (#1123)

erf-model · Jun 24, 2023 · 431b3cf · 431b3cf
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diff --git a/paper/paper.bib b/paper/paper.bib
@@ -117,3 +117,14 @@ @article{MOST:van
          year={2017},
          publisher={Wiley Online Library}
 }
+
+@techreport{WRF:skamarock,
+	doi = {10.5065/1dfh-6p97},
+	url = {https://dx.doi.org/10.5065/1dfh-6p97},
+	title = {A Description of the Advanced Research WRF Model Version 4.3 (No. NCAR/TN-556+STR)},
+	author = {Skamarock, W.~C. and Klemp, J.~B. and Dudhia, J. and Gill, D.~O. and Liu, Z. and Berner, J. and Wang, W. and Powers, J.~G. and Duda, M.~G. and Barker, D.~M. and Huang, X.},
+	institution = {National Center for Atmospheric Research},
+	month = {7},
+	year = {2021},
+	number = {NCAR/TN-556+STR}
+}
diff --git a/paper/paper.md b/paper/paper.md
@@ -126,7 +126,7 @@ Physical forcings include Coriolis and geostrophic forcing as well as
 Rayleigh damping in the upper regions of the domain.  Lateral boundary
 conditions can be specified as periodic, inflow/outflow, or time-varying
 values read in from external files in netcdf format generated by the WRF
-Preprocessing System (WPS). The surface boundary condition may be
+Preprocessing System (WPS) [@WRF:Skamarock]. The surface boundary condition may be
 specified either as a simple wall or by using Monin-Obukhov similarity theory (MOST)
 [@MOST:monin; @MOST:van] to model the surface layer. The initial data can
 be read from WPS-generated files, reconstructed from 1-d input sounding