Red Lightning

Inside a thunderstorm, ice and water particles collide and separate electrical charge. The upper cloud becomes positively charged. The lower cloud becomes negatively charged. As charge separation increases, the electric field strengthens. When the field exceeds air’s insulating capacity, lightning discharges to the ground. The upper atmosphere — thin, cold, and electrically sensitive — experiences rapid electric imbalance. At 50–90 kilometers altitude, the air partially ionizes. Nitrogen molecules become excited and emit red light. For a fraction of a second, towering red filamentary signs of electrical correction appear above the storm. 

Who this collection is for:

You see the initial activity but you don't become attached. Your awareness and objectivity remains high. You see the reaction above and behind it. Reducing ego and bias allows you to see and gather deep structural connections.

Mindset: Acuity Prevails
Ethic: Acknowledgment