Summary
Answer changes from the previous tag
Floodplain option
new control variable is <floodplain> = T or F
Floodplain is represented with very gentle slope (default 1:1000), extending from the top of side wall of the channel. The channel uses a bankfull depth. Currently bankfull depth is computed based on upstream area for each reach. This default method may change in the future. A user is encouraged to come up with the way to estimate the bankfull depth (and width) outside mizuRoute.
Regardless of whether floodplain is on or off, the method to compute celerity, diffusivity use the section 3.3 in Beg M et al., 2022. This is primary cause of the answer change from the previous version, which use the assumption of "wide" rectangular channel width, that simplifies the flow area computation. Also, from the current version, the channel geometry type can be rectangular (default) or trapezoidal (by providing side wall slope as input parameter).
What's Changed
allow a generic name when using only one routing method
- implement generic output name for routing method specific variables by @nmizukami in #482
Update external handling
- Adding git-fleximod by @nmizukami in #485
- remove manage_externals by @jedwards4b in #468
For CESM coupling
- Adding datetime in rpointer file with backward compatibility by @nmizukami in #486
routing with floodplain
- Including floodplain by @nmizukami in #470
- Fixing overflow error coming from default large bankfull depth by @nmizukami in #493
Cleanup
- remove many mpi_barrier by @nmizukami in #494
- sync mpi task before processing tmp file by @nmizukami in #487
- updated file open routing by @nmizukami in #491
New Contributors
- @jedwards4b made their first contribution in #468
Full Changelog: cesm-coupling.n02_v2.1.4-standalone...cesm-coupling.n03_v2.2.0
