A study on the 2009 A/H1N1 influenza pandemic found the inconsistent regional timing of pandemic waves in Mexico was a result of interactions between school breaks and regional variations in humidity.

The research published in PLOS Computational Biology, led by Dr. James Tamerius at the University of Iowa and Dr. Gerardo Chowell at Georgia State University, applied mathematical models to understand the social and environmental processes that generated two distinct pandemic outbreaks (“waves”) in Mexico during the summer and fall of 2009.

The summer wave occurred in the tropical southeastern states of Mexico, whereas the larger fall wave occurred in the central and northern states. The models suggest that high levels of humidity favored the rapid spread of influenza in the tropical states that led to the early summer wave. On the other hand, moderate levels of humidity slowed transmission in the central and northern states precluding a pandemic wave prior to summer break. The summer break reduced the transmission rate by an estimated 14% thereby delaying the pandemic wave in the central and northern states until students returned to school in August. These processes can explain the two major and distinct pandemic waves that affected the different regions.

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