Fungal diseases moving north as the West heats up and dries out

Valley Fever (Coccidioides) is one of dozens of diseases expanding its range globally.

Climate change is the primary driver of increased risk of Valley Fever in the western United States. The effect is two fold, raising the both probability of infection in existing ranges and expanding the reach of the affliction northwards.

Historically, most U.S. Valley fever has occurred in Arizona and California, with cases also occurring in Nevada, New Mexico and parts of other western states. But as the historic drought progresses, the spores have been discovered considerably farther north, including Washington State. Climate modeling suggests that continued warming could make portions of states such as Idaho, Wyoming, Montana, Nebraska, North Dakota and South Dakota increasingly suitable for the fungus.

Fungal spores cause Valley Fever

WHAT IS IT?

Coccidioides is an airborne soil  fungus, found in the form of spores spread by the wind. Valley Fever is caused by inhaling the spores, which thrive in hot, relatively dry environments.

The primary way to get valley fever is to breathe in the microscopic fungus which can get up into the air after infected soil is disturbed from things like high winds, construction, recreation and even gardening. The fungus gets deep in the lungs and mutates, which leads to a flu-like disease. Valley Fever doesn’t usually kill you, but it does make your wish you were ded. 

Global warming is expanding the range of Valley Fever as the American West becomes more and more arid with the rise of global temperatures. 

VALLEY FEVER GLOBAL WARMING DRIVERS

There are several mechanisms working together:

  • Higher temperatures: Warmer conditions are associated with higher Valley fever incidence. A major southwestern U.S. study found that incidence was higher in warmer areas and where soils were drier.
  • Drought and drying soils: Dry soils become more prone to generating dust, which can carry fungal spores into the air. The CDC specifically identifies increasing heat and drought in the Southwest as factors that can increase Valley fever risk.
  • Rain followed by drought: Rain can stimulate fungal growth, while subsequent drying can leave spores in the soil that become airborne. California research has found substantial increases in risk following swings from unusually wet conditions to drought.
  • Longer dry seasons: Recent research using California data from 2000–2023 found that hot, dry conditions can cause the Valley fever transmission season to begin earlier and end later. When both spring and fall were unusually dry, the estimated transmission season was nearly four weeks longer.
  • Wildfires and dust: Fires disturb soil and vegetation, while drought and extreme heat increase dust. Both can increase airborne exposure to Coccidioides spores.

Valley Fever is spreading

Scientists are warming that the potential for an epidemic is significant.  A 2026 CDC analysis found that Arizona’s reported Valley fever incidence approximately doubled between 2005 and 2022, with most cases concentrated in Maricopa, Pima and Pinal counties. About 95% of U.S. reported cases occur in Arizona and California. But that is likely to change.

California experienced a particularly striking episode in 2023, reporting 9,054 cases—its second-highest annual total on record. Researchers linked the subsequent high risk to the dramatic transition from drought to unusually heavy precipitation and back toward dry conditions.

Valley Fungal Fever

Viruses and pathogens on the move world wide

A warming climate and land-use changes are already having an affect globally on well-known diseases like Dengue, Chikungunya and Yellow Fever. These three are higher profile maladies spread by mosquitoes, moving into regions where there is not likely to be natural resistance. They are far from the only diseases coming your way.

A 2022 study estimates that more than half of known human pathogenic diseases could be aggravated by climate change.

As an example, take a look at Argentine Hemorrhagic Fever (AHF) a rare but serious disease carried by rodents. Both the United States and Soviet Union researched them as a potential agent for biological weapons. That can’t be good. AHF was once confined mostly to rural areas, but it’s now moving into cities.

HP Lovecraft mountains of madness

Dengue, a flulike illness that can be fatal, is one of the fastest-growing infectious diseases in parts of South America, linked its growth to environmental degradation and a warming planet. More than 10 million cases, and over 16,000 related deaths, have been reported to the World Health Organization since the beginning of 2024..

Scientists have also linked climate change to the spread of the Andes virus, a rare but dangerous hantavirus — another type of rodent-borne pathogen present in South America — that was linked to three deaths on a cruise ship earlier this year. That outbreak tested the nerves of a pandemic-weary world and spotlighted the kind of growing viral spillover risks that researchers like Dr. Kulkarni have been examining.

ZOMBIE VIRUSES LURKING BENEATH THE (NOT SO) PERMAFROST?

One of the most powerful climate feedbacks is the release of methane once trapped beneath the frozen tundra or permafrost that covers much of the Arctic. But methane is not the only scary thing under there.  Permanently frozen environments are natural reservoirs for microorganisms, including viruses, bacteria and humans pathogens. It is not currently considered likely that dangerous microbes such as smallpox are about to be released, but there is no question that dormant viruses will be released as the Arctic continues to heat up. The region is warming twice as fast as the rest of the planet. Which is warming very fast.

In 2015, researchers from Aix-Marseille University isolated  two large DNA viruses in Siberia frozen for 30,000 years in ancient permafrost. They were not a threat to humans.

There was a well-documented anthrax outbreak in 2016 in Siberia. It killed thousands of reindeer. The cause of the outbreak is attributed to the activation of spores due to a permafrost thaw, accelerated during the summer heat wave of that year.

 

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