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Code Table 4.2: Subgrid-scale lightning potential index #108
Comments
Dear @SibylleK , thank you for this proposal. I have forwarded it to our LPI expert so that he can eventually comment. |
Dear @SibylleK , please see below the answer from our LPI expert:
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Dear @sebvi , thank you very much for your support and the comments of your colleague.
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Dear @SibylleK , I tend to disagree regarding the analogy with precipitation if you mean by that large-scale precipitation vs convective precipitation. In the case of precipitation, it is not the same parameter computed by 2 different methods, it is 2 distinct components of the precipitation coming from 2 different physical processes and they could both be non zero in the same grid box. I think comments from others in @wmo-im/tt-tdcf would be valuable for this discussion. |
I have updated the proposal. A "Subgrid-scale lightning potential index" is proposed now and the note is changed a little bit for a better understandig, hopefully. |
branch is updated |
@jitsukoh @SibylleK Editorial question about "Subgrid-scale...", because I found different versions in the manual. Can you please verify the correct version?
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maybe we need the point of view of a native english speaker for this. @jbathegit ? In any case, once we agree on 1 term, all others should be corrected consistently . My preference goes with option 3. |
Branch
https://github.com/wmo-im/GRIB2/tree/iss108
Summary and purpose
Request of a new lightning potential index parameter.
Action proposed
The team is kindly asked to review and approve the content for inclusion within the next update to the WMO Manual on Codes.
Discussions
The existing entry in code table 4.2 discipline 0, category 17:
1 Lightning potential index (LPI) (J kg-1)
stands for the LPI derived from grid scale (large scale) model quantities in convection permitting models, if we follow the definition after Lynn et al. 2010.
DWD requests a new LPI parameter derived from sub-grid scale (convective) model quantities.
Detailed proposal
Add in code table 4.2 discipline 0, category 17
Note 3: The lightning potential index (LPI, Number 1), as defined by Lynn et al. 2010, is derived from grid scale (resolved) model information in convection permitting models. In contrast, the subgrid-scale lightning potential index is derived from subgrid-scale information (from parameterized convection) for models with coarser resolution.
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