Abstract

Hydroclimatic changes may be particularly pronounced in high-latitude regions and can influence infectious diseases, jeopardizing regional human and animal health. In this study, we consider the example of tularemia, one of the most studied diseases in high-latitude regions, which is likely to be impacted by large regional hydroclimatic changes. For this disease case, we use a validated statistical model and develop a method for quantifying possible hydroclimatically driven shifts in outbreak conditions. The results show high sensitivity of tularemia outbreaks to certain combinations of hydroclimatic variable values. These values are within the range of past regional observations and may represent just mildly shifted conditions from current hydroclimatic averages. The methodology developed also facilitates relatively simple identification of possible critical hydroclimatic thresholds, beyond which unacceptable endemic disease levels may be reached. These results call for further research on how projected hydroclimatic changes may affect future outbreaks of tularemia and other infectious diseases in high-latitude and other world regions, with particular focus on critical thresholds to high-risk conditions. More research is also needed on the generality and spatiotemporal transferability of statistical disease models.

Highlights

  • Hydroclimatic changes in the landscape, such as in runoff [1], evapotranspiration [2], and often both [3], are being observed and projected regionally and globally, adding to, or occasionally opposing, atmospheric changes in precipitation [4]

  • Modeled endemic levels are sensitive to the value of relative mosquito abundance (RMA), and thereby to the underlying values of Q1, Q2, and T (Figure 2)

  • Our analysis revealed that tularemia outbreaks are most sensitive to relative mosquito abundance (RMA) and associated underlying periodic hydroclimatic conditions of flow (Q1 and Q2 ) and mean temperature (T), followed by summer temperature in the preceding year (STlag ) and summer precipitation in the current year (SP)

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Summary

Introduction

Hydroclimatic changes in the landscape, such as in runoff [1], evapotranspiration [2], and often both [3], are being observed and projected regionally and globally, adding to, or occasionally opposing, atmospheric changes in precipitation [4]. Such changes have serious implications for terrestrial water cycling and availability, with particular availability impacts in cold regions, where the water cycle depends on snow and ice conditions [1]. Public Health 2019, 16, 3717; doi:10.3390/ijerph16193717 www.mdpi.com/journal/ijerph

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