links

Author: adrifoster

doc/source/lilac/specific-atm-models/wrf.rst

@@ -171,7 +171,7 @@ skip to section :numref:`wrf-set-ctsm-runtime-options`.
 
 Get WPS from this website::
 
-    https://www2.mmm.ucar.edu/wrf/users/download/wrf-regist_or_download.php
+    https://www2.mmm.ucar.edu/wrf/users/download/get_source.html
 
 New users must complete a registration form in this step.
 

doc/source/tech_note/Ecosystem/CLM50_Tech_Note_Ecosystem.rst

@@ -294,7 +294,7 @@ The current state of the atmosphere (:numref:`Table Atmospheric input to land mo
 
 :sup:`4`\ The nitrogen deposition rate is required by the biogeochemistry model when active and represents the total deposition of mineral nitrogen onto the land surface, combining deposition of NO\ :sub:`y` and NH\ :sub:`x`. The rate is supplied either as a time-invariant spatially-varying annual mean rate or time-varying for a transient simulation. Nitrogen deposition rates were calculated from the same CAM chemistry simulation that generated the aerosol deposition rates.
 
-:sup:`5`\ Climatological 3-hourly lightning frequency at :math:`\sim`\ 1.8° resolution is provided, which was calculated via bilinear interpolation from 1995-2011 NASA LIS/OTD grid product v2.2 (http://ghrc.msfc.nasa.gov) 2-hourly, 2.5° lightning frequency data. In future versions of the model, lightning data may be obtained directly from the atmosphere model.
+:sup:`5`\ Climatological 3-hourly lightning frequency at :math:`\sim`\ 1.8° resolution is provided, which was calculated via bilinear interpolation from 1995-2011 NASA LIS/OTD grid product v2.2 (https://cmr.earthdata.nasa.gov/search/concepts/C1995863244-GHRC_DAAC.html) 2-hourly, 2.5° lightning frequency data. In future versions of the model, lightning data may be obtained directly from the atmosphere model.
 
 Density of air (:math:`\rho _{atm}` ) (kg m\ :sup:`-3`) is also required but is calculated directly from :math:`\rho _{atm} =\frac{P_{atm} -0.378e_{atm} }{R_{da} T_{atm} }` where :math:`P_{atm}` is atmospheric pressure (Pa), :math:`e_{atm}` is atmospheric vapor pressure (Pa), :math:`R_{da}` is the gas constant for dry air (J kg\ :sup:`-1` K\ :sup:`-1`) (:numref:`Table Physical constants`), and :math:`T_{atm}` is the atmospheric temperature (K). The atmospheric vapor pressure :math:`e_{atm}` is derived from atmospheric specific humidity :math:`q_{atm}` (kg kg\ :sup:`-1`) as :math:`e_{atm} =\frac{q_{atm} P_{atm} }{0.622+0.378q_{atm} }`.