During strong El Niño events, coastally trapped Kelvin waves routinely propagate all the way up the North American West Coast to the
Pacific Northwest and British Columbia (around 50°N), and during major events, measurable sea-level and temperature signals can reach as far north as the
Gulf of Alaska (around 55°N–60°N).
As these subsurface waves travel poleward from the equator at roughly 150 miles per day, several factors govern how far north they remain coherent:
- California to the Pacific Northwest (32°N–50°N): The wave signal remains strong and well-defined along California, Oregon, Washington, and Vancouver Island, where it temporarily raises local sea levels by 6 to 12 inches, deepens the thermocline, and suppresses cold, nutrient-rich upwelling.
- Gulf of Alaska (55°N–60°N): During "super" El Niños (such as 1982–83, 1997–98, and 2015–16), tide gauges and satellite altimetry detect the poleward-propagating sea-level anomaly wrapping around the Gulf of Alaska before dissipating against complex coastal topography and strong local atmospheric forcing.
- Energy Loss Along the Way: As a coastal Kelvin wave moves into higher latitudes, it gradually weakens due to friction, scattering from underwater canyons and islands (like the Channel Islands or Vancouver Island), and offshore energy radiation as Rossby waves.
Because the wave takes weeks to months to travel from the tropics to high latitudes, the oceanic sea-level rise and warming arrive in British Columbia and Alaska well after they hit Southern California—often compounding winter storm surges and king tides.