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Modeling Lightning Activity in the Third Pole Region: Performance of a km-Scale ICON-CLM Simulation
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The Third Pole region, especially the Himalayas, is a lightning hotspot. Predicting lightning activity in this region is difficult due to the complex monsoon and westerly circulations, as well as the complex orography. Km-scale simulations can explicitly, without parameterization, tackle deep convective phenomena. A year-long (October 2019–September 2020) ICON-CLM simulation was performed with a km-scale horizontal grid spacing of 3.3 km to assess the region’s lightning activity and evaluate the model ICON-CLM. The simulated lightning potential index (LPI) was compared against the lightning proxy CAPE × PREC (CP) derived from ICON-CLM and reanalysis ERA5. In addition, the LPI was evaluated against the TRMM lightning climatology and observed flashes from the International Space Station Lightning Imaging Sensor (ISS-LIS). The LPI reproduced the major spatial, seasonal, and diurnal features of lightning activity as represented in the TRMM climatology. In contrast, the CP from both ICON-CLM and ERA5 performed less well regarding the location of events and the diurnal features. Taking the mean values of the LPI and CP of all the grids within 90 km × 90 km around the ISS-LIS detected lightning event, we found that over 80% of lightning events were recorded using the ICON-CLM simulation. Analysis of individual cases showed that the LPI predicted localization of lightning events better, but flash counts were slightly lower than the CP. Therefore, the combined use of ICON-CLM’s simulated LPI and CP can be a valuable predictor for lightning events over the Third Pole region.
Title: Modeling Lightning Activity in the Third Pole Region: Performance of a km-Scale ICON-CLM Simulation
Description:
The Third Pole region, especially the Himalayas, is a lightning hotspot.
Predicting lightning activity in this region is difficult due to the complex monsoon and westerly circulations, as well as the complex orography.
Km-scale simulations can explicitly, without parameterization, tackle deep convective phenomena.
A year-long (October 2019–September 2020) ICON-CLM simulation was performed with a km-scale horizontal grid spacing of 3.
3 km to assess the region’s lightning activity and evaluate the model ICON-CLM.
The simulated lightning potential index (LPI) was compared against the lightning proxy CAPE × PREC (CP) derived from ICON-CLM and reanalysis ERA5.
In addition, the LPI was evaluated against the TRMM lightning climatology and observed flashes from the International Space Station Lightning Imaging Sensor (ISS-LIS).
The LPI reproduced the major spatial, seasonal, and diurnal features of lightning activity as represented in the TRMM climatology.
In contrast, the CP from both ICON-CLM and ERA5 performed less well regarding the location of events and the diurnal features.
Taking the mean values of the LPI and CP of all the grids within 90 km × 90 km around the ISS-LIS detected lightning event, we found that over 80% of lightning events were recorded using the ICON-CLM simulation.
Analysis of individual cases showed that the LPI predicted localization of lightning events better, but flash counts were slightly lower than the CP.
Therefore, the combined use of ICON-CLM’s simulated LPI and CP can be a valuable predictor for lightning events over the Third Pole region.
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