What Exactly Is a Derecho? And Why the Winds We Recently Had in Santa Fe Were NOT One

Over the past several days, we’ve had a few dry thunderstorms move across Northern New Mexico that produced some very strong wind gusts and outflow winds. A few people reached out and asked if those winds were a "derecho".
The answer is no. Those storms were not derechos.
Since the term gets used quite a bit whenever there is damaging wind involved, I wanted to take a little time to explain what a derecho actually is and also talk about the types of wind events we commonly experience here in Santa Fe.
So What Is a Derecho?
A derecho is a widespread, long-lived wind storm associated with a large complex of thunderstorms. The word “derecho” comes from the Spanish word for “straight ahead,” which refers to the straight-line winds these storms produce.
Unlike tornadoes, which have rotating winds concentrated in a small area, derechos create powerful straight-line winds that can extend for hundreds of miles.
To officially be classified as a derecho, a storm system generally must:
- Produce a long track of damaging winds
- Cover at least 240 miles
- Include numerous reports of severe wind gusts over 58 mph
- Maintain its intensity for many hours
Some derechos can produce wind gusts over 80 to 100 mph and cause damage similar to a hurricane.
These events are much more common across the Plains and Midwest during the late spring and summer months where warm, humid air fuels massive thunderstorm complexes.
What We Recently Experienced in Santa Fe
What we experienced recently were dry thunderstorms that produced strong outflow winds. This is very common in New Mexico during the spring and early summer months.
Our atmosphere is often very dry near the ground. When thunderstorms develop, much of the rain evaporates before reaching the surface. That evaporation cools the air rapidly, causing it to sink toward the ground. Once that cooler air hits the surface, it spreads outward in all directions, producing sudden strong wind gusts.
That spreading air is called an outflow boundary.
Sometimes these outflows can produce wind gusts between 40 and 70 mph, especially with collapsing thunderstorms. They can kick up large dust plumes, rapidly drop temperatures, and create dangerous crosswinds for drivers.
But despite the strong winds, these storms are usually:
- Short-lived
- Localized
- Not part of a large organized thunderstorm complex
That’s why they are not considered derechos.
The Types of Winds We Commonly Get in Santa Fe
Santa Fe experiences several different types of wind events throughout the year.
Spring Southwest Winds
One of the most common wind patterns we see is the strong southwest wind that develops during the spring. These winds are typically caused by strong storm systems moving across the western United States while pressure differences tighten across New Mexico.
These windy days can produce:
- Sustained winds of 20–40 mph
- Gusts over 50 mph
- Blowing dust
- Increased wildfire danger
These are not thunderstorm winds at all. They are large-scale gradient winds tied to weather systems.
Thunderstorm Outflow Winds
As we discussed above, dry thunderstorms can produce sudden powerful gust fronts and outflow winds during late spring and monsoon season.
These winds can arrive very quickly and sometimes hit before any rain begins.
Canyon and Gap Winds
Santa Fe’s terrain also plays a huge role in our wind patterns. Winds can accelerate through canyons and gaps in the mountains, especially during frontal passages.
Areas near the base of the Sangre de Cristo Mountains can sometimes experience locally stronger gusts than other parts of town because of the terrain.
Could Santa Fe Ever Experience a Derecho?
It’s possible, but it would be very rare.
Derechos typically need a large supply of warm, humid air and expansive thunderstorm complexes — something that is much more common east of the Rockies.
Eastern New Mexico and the High Plains have a better chance of occasionally seeing derecho-like systems than Santa Fe does. That said, we absolutely can experience damaging winds from thunderstorms, especially from strong outflow boundaries and microbursts.
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