diff --git a/index.rst b/index.rst index 3edd869bb6..090ce0a01e 100644 --- a/index.rst +++ b/index.rst @@ -293,6 +293,7 @@ References observations/obs_converters/AIRS/convert_airs_L2 observations/obs_converters/AIRS/convert_amsu_L1 observations/obs_converters/AVISO/AVISO + observations/obs_converters/Ameriflux/fluxnetfull_to_obs observations/obs_converters/Ameriflux/level4_to_obs observations/obs_converters/CHAMP/work/README observations/obs_converters/cice/cice_to_obs @@ -414,6 +415,7 @@ References models/rose/readme models/simple_advection/readme models/sqg/readme + models/template/new_model models/tiegcm/readme models/wrf_hydro/readme models/wrf/readme diff --git a/models/lorenz_96_tracer_advection/readme.rst b/models/lorenz_96_tracer_advection/readme.rst index 417f82d903..ad6f8d728b 100644 --- a/models/lorenz_96_tracer_advection/readme.rst +++ b/models/lorenz_96_tracer_advection/readme.rst @@ -63,7 +63,7 @@ one dimensional array. The tracer particle in the figure lands on a predefined g point at t\ :sup:`n+1`. The trajectory of this tracer particle is then integrated backwards by one time step to time t\ :sup:`n`, often landing between grid points. Then, due to advection without diffusion, the concentration of tracer at time - t\ :sup:`n+1` is simply the concentration of tracer at time t\ :sup:`n`, which +t\ :sup:`n+1` is simply the concentration of tracer at time t\ :sup:`n`, which can be determined by interpolating concentrations of the surrounding grids [3]_. Once the coupled Lorenz 96 and semi-Lagrangian is run with a source of strength diff --git a/observations/obs_converters/Ameriflux/level4_to_obs.rst b/observations/obs_converters/Ameriflux/level4_to_obs.rst index b0f87d3d4a..699ba23463 100644 --- a/observations/obs_converters/Ameriflux/level4_to_obs.rst +++ b/observations/obs_converters/Ameriflux/level4_to_obs.rst @@ -10,7 +10,7 @@ AmeriFlux level 4 data to DART observation sequence converter | This routine was designed to convert the flux tower Level 4 data from the `AmeriFlux `__ network of observations from micrometeorological tower sites. The download link and flux data format for this code *has been discontinued* (e.g. ``USBar2004_L4_h.txt``). Thus if you are using flux obs converters for the first time - *PLEASE USE* the updated ``Fluxnetfull_to_obs.f90`` converter and follow the documentation there :doc:`./Fluxnetfull_to_obs` + *PLEASE USE* the updated ``Fluxnetfull_to_obs.f90`` converter and follow the documentation there :doc:`./fluxnetfull_to_obs` We have kept this code available if you still use the older Ameriflux data format. Also this code uses a general approach to calculating sensible, latent and net ecosystem exchange uncertainty, that may be helpful. | The AmeriFlux Level 4 data products are provided in the local time of the flux tower location. DART observation sequence