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Updating NWS8 and adding upgrades from Wang et. al. (2022) #393
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…n to 10 minute winds is applied to entirety of wind forcing
Conflicts: src/read_input.F src/wind.F
When you say "background winds" do you mean synoptic scale wind fields far from the vortex or do you mean how you're adding storm motion into the vortex wind field? If the latter, that is referred to as storm motion asymmetry. |
I used the terminology "background winds" because that is what it is referred to in Lin and Chavas (2012). I can change that option to "asymmetryModel" or similar if that would be more descriptive. |
Yeah I would appreciate changing the terminology to be more specific.
"Background" is, unfortunately, a somewhat abused term in these contexts.
…-T
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On Wed, May 22, 2024 at 8:18 AM Coleman Blakely ***@***.***> wrote:
I used the terminology "background winds" because that is what it is
referred to in Lin and Chavas (2012). I can change that option to
"asymmetryModel" or similar if that would be more descriptive.
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…ndspeeds in the fort.22
@cblakely97 Please check the |
See this namelist implementation in OM2D: CHLNDDEV/OceanMesh2D#317 |
…kgroundWindFac that is consistent with the reduction factor for LC12 at Rmax, add non_cyclostropic_part to the Holland gradient wind fields (triggered by the BCalc namelist option, which may be better to be renamed to cyclostrophic True or False), and otherwise some cleaning up the code
- Merge changes from main into diverging cle15-lc12 branch in preparation for pull request
- Adds 'ios_nml_error_msg' to subroutine calls that read nws8Control namelist in read_input.F
References:
Chavas, D. R., Lin, N., & Emanuel, K. (2015). A Model for the Complete Radial Structure of the Tropical Cyclone Wind Field. Part I: Comparison with Observed Structure. Journal of the Atmospheric Science, 72(9), 3647-3662. https://doi.org/10.1175/JAS-D-15-0014.1
Wang, Shuai, Ning Lin, and Avantika Gori. “Investigation of Tropical Cyclone Wind Models With Application to Storm Tide Simulations.” Journal of Geophysical Research: Atmospheres 127, no. 17 (2022): e2021JD036359. https://doi.org/10.1029/2021JD036359.
Description
Type of change
Issue Number
How Has This Been Tested?
Relevant Publications (if applicable)
Chavas, D. R., Lin, N., & Emanuel, K. (2015). A Model for the Complete Radial Structure of the Tropical Cyclone Wind Field. Part I: Comparison with Observed Structure. Journal of the Atmospheric Science, 72(9), 3647-3662. https://doi.org/10.1175/JAS-D-15-0014.1
Chavas, D. R., & Lin, N. (2016). A Model for the Complete Radial Structure of the Tropical Cyclone Wind Field. Part II: Wind Field Variability. Journal of the Atmospheric Sciences, 73(8), 3093-3113. https://doi.org/10.1175/JAS-D-15-0185.1
Lin, N., and D. Chavas (2012), On hurricane parametric wind and applications in storm surge modeling, J. Geophys. Res., 117, D09120, doi:10.1029/2011JD017126.
Wang, Shuai, Ning Lin, and Avantika Gori. “Investigation of Tropical Cyclone Wind Models With Application to Storm Tide Simulations.” Journal of Geophysical Research: Atmospheres 127, no. 17 (2022): e2021JD036359. https://doi.org/10.1029/2021JD036359.
Wang, S., N. Lin, A. Gori. (2022) "New wind forcing option (CLE15 wind model) for hurricane surge simulation with ADCIRC." DesignSafe-CI. https://doi.org/10.17603/ds2-xd0r-bk81 v1
Checklist:
main
If any of the above are not checked, please explain why:
Further comments
This pull request incorporates the upgrades to NWS = 8 found in Wang et. al., (2022) into the main version of ADCIRC. Formerly, this capability was only found in the DesignSafe repository and required the use of cmake compiler flags to enable the CLE15 and LC12 vortex and background winds. This commit instead moves activation to a namelist that preserves legacy behavior by default.