Storm Éowyn: It has unleashed strong and damaging winds over the British Isles, and particularly over Ireland and Scotland.
o Strong Jet Stream: Winds >200 mph over the North Atlantic due to temperature contrast between cold air (eastern US) and warm ocean air.
o Warm Ocean Temperatures: Record-high sea surface temperatures provided energy.
o Cloud Condensation: Deep clouds generated energy, fueling storm intensity.
o Ideal Track: Crossed jet stream from south to north.
o Pressure readings vary based on the storm's formation location.
o Rapid intensification process is called bombogenesis.