High winds and resulting tree windfall are a primary source of disturbance in northeastern forests. Forest gaps created by openings in the canopy can allow for regeneration of flora and habitat diversity for fauna. However, severe or catastrophic wind damge can damage sensitive habitats that have slower regeneration timelines and allow for over competition of early successional and invasive generalist species. As climate changes in the region, high winds are expected to increase in severity, extent and frequency, which could have negative impacts on the region's forests. Based on 20 years of data from the NOAA global historical climatology network daily summaries (GHCND) dataset fastest 5-second wind speed we calculated a threshold of 55mph (48kts) for high wind events based on a comparison of wind speeds that cause forest damage from the Beaufort scale, the Enhanced Fujita Scale and the Saffir-Simpson Hurricane scale.
Long-term trends across the region indicate that the average number of high wind events at any given station is stable.
However, the total number of high wind events reported across the region, as well as the number of stations reporting at least one high wind event is increasing. This indicates that high wind events are increasing in some, but not all, locations.Interestingly, the both the average maximum wind speed and the number of extreme high wind events (>95 percentile) has decreased significantly, indicating that while high wind events are becoming more widespread and frequent, extreme wind events are not.
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