Yes, you have hit on an excellent piece of the physics puzzle. The moisture level of the soil drastically changes how easily an electrical charge concentrates and moves, directly affecting where and how lightning strikes.
🌧️ Wet, Saturated Ground: The Perfect Conductor
When heavy rain saturates the soil, it completely transforms the ground's electrical properties:
Lower Resistance: Pure water is a poor conductor, but rain mixing with soil creates a mineral-rich electrolyte solution. This drops the ground’s electrical resistance to near zero.
Rapid Charge Concentration: Lightning occurs when opposite charges in the cloud and the ground pull toward each other. In wet soil, these ground charges (usually positive) can flow incredibly fast, rushing to the surface and concentrating at high points like trees, poles, or hills.
Easier Upward Streamers: Because the charge concentrates so efficiently in soggy soil, the ground can easily launch "upward streamers" (channels of positive charge reaching up into the sky). When one of these connects with a downward leader from the cloud, the lightning strike is completed.
🏜️ Extremely Dry Soil: The Electrical Insulator
Conversely, bone-dry soil behaves in the exact opposite manner, which actually increases the danger of a strike:
High Resistance: Dry dirt, sand, and rock are excellent electrical insulators. Ground charges move sluggishly and struggle to travel through the dry earth.
Delayed Charge Concentration: Because the charges cannot move freely, it takes longer for a strong charge to concentrate on the surface.
More Violent Strikes: When the electrical tension between the cloud and dry ground finally overpowers the soil's resistance, the resulting lightning strike can be incredibly violent. Because the dry ground cannot easily dissipate the electricity, the current travels wildly across the surface or deep into the earth searching for moisture, often exploding rocks or melting sand into glass (fulgurites).
⚡ The Rain Lull Connection
This ties perfectly back to your observation about the lull in the rain. During the heaviest initial downpour, the ground goes from dry to rapidly saturated. By the time a lull in the rain occurs, the top layer of soil has become fully soaked and highly conductive, making it prime real estate for the storm to finally discharge its built-up electrical energy.
If you are curious about what happens after the lightning hits the dirt, I can explain how fulgurites (fossilized lightning) form in different soils, or detail how ground currents travel through wet earth to cause injuries. Which aspect of soil physics should we explore next?
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Thomas Paul Murphy
References included at base of Part I?
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