INVESTIGADORES
LANERI Karina Fabiana
artículos
Título:
Climate drivers of malaria at its southern fringe in the Americas
Autor/es:
KARINA LANERI; BRENNO CABELLA; PAULO INÁCIO PRADO; RENATO MENDES COUTINHO; ROBERTO KRAENKEL
Revista:
PLOS ONE
Editorial:
PUBLIC LIBRARY SCIENCE
Referencias:
Lugar: San Francisco; Año: 2019 vol. 14 p. 1 - 17
ISSN:
1932-6203
Resumen:
In this work we analyze potential environmental drivers of malaria cases in Northwestern Argentina. We inspect causal links between malaria and climatic variables by means of the convergent cross mapping technique, which provides a causality criterion from the theory of dynamic systems. Analysis is based on 12 years of weekly malaria P. vivax cases in Tartagal, Salta, Argentina?at the southern fringe of malaria incidence in the Americas?together with humidity and temperature time-seriesspanning the same period. Our results show that there are causal links between malaria cases and both maximum temperature, with a delay of five weeks, and minimum temperature, with delays of zero and twenty two weeks. Humidity is also a driver of malaria cases, with thirteen weeks delay between cause and effect. Furthermore we also determined the sign and strength of the effects. Temperature has always a positivenon-linear effect on cases, with maximum temperature effects more pronounced above 25 ◦ C and minimum above 17 ◦ C, while effects of humidity are more intricate: maximum humidity above 85% has a negative effect, whereas minimum humidity has a positive effect on cases. These results might be signaling processes operating at short (below 5 weeks) and long (over 12 weeks) time delays, corresponding to effects related to parasite cycle and mosquito population dynamics respectively. The non-linearities found for the strength of the effect of temperature on malaria cases make warmer areas more prone to higher increases in the disease incidence. Moreover, our results indicate that an increase of extreme weather events could enhance the risks of malaria spreading andre-emergence beyond the current distribution. Both situations, warmer climate and increase of extreme events, will be remarkably increased by the end of the century in this hot spot of climate change.