Mount Washington’s summit experiences extreme winds primarily due to its topography, which funnels westerly flows through the Presidential Range’s V-shaped gap, combined with tight pressure gradients from passing low-pressure systems. In August, trader sentiment reflects the lower historical likelihood of hurricane-force gusts compared to winter or spring, as seasonal patterns favor weaker extratropical systems or occasional tropical remnants rather than intense cyclones. The Mount Washington Observatory continuously records sustained winds and gusts via anemometers, with data released in real time and daily summaries; August records typically fall well below the all-time 231 mph benchmark from April 1934. Upcoming NOAA and National Weather Service forecasts for New England high-pressure setups or frontal passages through early September will provide key updates that could shift implied probabilities if stronger gradients develop.