Number (In Section 4, octet 11) |
Parameter | Units |
Abbrev |
---|---|---|---|
0 |
Lightning Strike Density | m-2 s-1 | LTNGSD |
1 |
Lightning Potential Index (LPI) (see Note 1) | J kg-1 | LTPINX |
2 | Cloud-to-Ground Lightning Flash Density | km-2 day-1 | CDGDLTFD |
3 | Cloud-to-Cloud Lightning Flash Density | km-2 day-1 | CDCDLTFD |
4 | Total Lightning Flash Density (see Note 2) | km-2 day-1 | TLGTFD |
5 | Subgrid-scale lightning potential index (see Note 3) | J kg-1 | SLNGPIDX |
6-191 | Reserved | ||
192-254 |
Reserved
for Local Use |
||
192 |
Lightning |
non-dim |
LTNG |
255 |
Missing |
Notes: (1) Definition of LPI after Lynn et. al.: Lynn, B., and Y. Yair, 2010: Prediction of lightning flash density with the WRF model, Adv. Geosci., 23, 11-16 Yair, B. Lynn, C. Price, V. Kotroni, K. Lagouvardos, E. Morin, A. Mugnai, and M. Llasat, 2010: Predicting the potential for lightning activity in Mediterranean storms based on the Weather Research and Forecasting (WRF) model dynamic and microphysical fields, JGR, 115, D04205, doi:10.1029/2008JD010868 (2) The total lightning flash density is the sum of cloud-to-ground and cloud-to-cloud lightning flash densities (see Lopez, P., 2016: A lightning parameterization for the ECMWF Integrated Forecasting System, Monthly Weather Review, 144, 3057-3075). (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. |