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Intense winds exacerbate wildfires in California. What causes them?

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High winds have significantly contributed to the catastrophic wildfires in Los Angeles, and following a brief period of calm at the end of last week, forecasts indicate that these winds are set to pick up throughout the current week. This development will likely complicate efforts to combat the blazes, which have resulted in the deaths of at least 24 individuals, destroyed thousands of structures, and are expected to become one of the most expensive natural disasters in U.S. history.

To better understand this phenomenon, it is essential to explore the science behind wind, including its definition, causes, and behavior, particularly within the distinctive geography of Southern California.

Wind can be defined as the movement of air resulting from variations in atmospheric pressure across different areas. When the pressure differences are significant, stronger winds are produced. Additionally, the topography of a region plays a crucial role—mountain peaks, which lack trees or buildings, often experience higher wind speeds because there are fewer obstacles to slow the air down. Moreover, the way land and water absorb heat from sunlight varies, which subsequently influences wind patterns.

The Santa Ana winds are a specific type of wind characteristic of Southern California. Unlike the seasonal flow of cool, moist air from the Pacific Ocean to the coastline, the Santa Ana winds are warm winds that blow in the opposite direction. Typically occurring between September and May, these winds are exceptionally dry and are associated with some of the most devastating wildfires in the area. The lack of humidity causes vegetation to dry out rapidly, making it more susceptible to burning.

The unique geography of Southern California heavily influences the behavior of winds. When winds travel into the region from the northeast during Santa Ana events, they originate from Nevada and western Utah. A high-pressure system in those states interacts with a low-pressure system in Mexico, causing air to funnel through mountain passes. As the air flows upward and downward over the peaks, it accelerates, leading to swift wind patterns that can greatly enhance the speed and erratic behavior of wildfires in the mountainous terrain where pressure differences are more pronounced compared to flatlands.

In terms of the impact of climate change on wind patterns, meteorologist Alex DaSilva from AccuWeather noted that establishing a direct connection between climate change and Santa Ana winds is complex. However, he observed that research predicts worsening drought conditions associated with climate change, which could increase fire risks linked to strong winds. Conversely, Victor Gensini, a climate scientist from Northern Illinois University, stressed that there is currently no established link between these wind types and climate change, emphasizing that the relationship remains unproven.

@USLive

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