Once relegated to the realm of maritime lore, rogue waves have transitioned from eerie tales told by sailors to a recognized scientific phenomenon in the last 27 years. Stories of unexpectedly colossal waves, capable of engulfing ships or submerging them entirely, were once dismissed as mere superstitions. However, the scientific community now acknowledges the existence of these rogue waves, which were thrust into the spotlight again when a massive wave struck a beach in Ventura, California.
What exactly defines a rogue wave? Rogue waves, while relatively uncommon, pose a potential threat due to their size and unpredictability. Scientists use a parameter called significant wave height, which represents the average of the largest 33% of observed waves in the ocean, to identify rogue waves. These waves earn the "rogue" label if they are at least twice the significant wave height. In simpler terms, rogue waves are typically more than double the size of their surrounding waves, exhibiting steep sides and deep troughs.
Described as "extreme storm waves" by scientists, rogues are notorious for their unpredictability, often arriving from unexpected directions that defy conventional wind and water patterns. While commonly referred to as "freak" or "killer" waves, their technical designation is "extreme storm waves," presenting as formidable walls of water.
The recent wave that crashed onto a California beach in Ventura prompted many to label it a rogue wave. However, defining such incidents isn't straightforward. Scott Beatty, CEO of the coastal intelligence firm MarineLabs, cautions against hasty classifications, emphasizing that the technical criteria for rogue waves are often misunderstood. A large individual wave, or a set of waves coupled with a high tide, may give the appearance of a rogue wave, but it could simply be a result of very large waves surging onto the beach and overcoming barriers.
Meteorologist Lisa Phillips sheds light on the incident in Ventura, describing it as a "wave run-up." This phenomenon occurs during periods of large surf, where some waves are significantly larger than others, causing water to reach further inland than expected.
The elusive nature of rogue waves stems from a lack of complete understanding of their formation. While certain conditions increase the likelihood of rogue waves, predicting their occurrence remains challenging. Similar to avalanches, these waves emerge when sea swells collide, creating larger, towering waves, especially when travelling in the same direction. Additionally, waves generated during storms, moving against the current, can interact in a way that results in the formation of large, enduring rogue waves.
Factors like El Niño and climate change also play a role in wave dynamics. El Niño, a natural climate pattern associated with warming ocean surface temperatures in the Pacific, can contribute to larger waves. The current strong El Niño is anticipated to intensify low-pressure systems, potentially influencing wave activity. While attributing giant waves directly to climate change is challenging, observations indicate that the increasing impact of climate change is gradually enhancing wave energy in the ocean. As the ocean warms, storms intensify, leading to stronger winds and, consequently, more intense waves.