Caro S Park1, Elisabeth Vogel2, Leila M Larson3, Samuel S Myers4, Mark Daniel5, Beverley-Ann Biggs6. 1. Department of Medicine at the Doherty Institute, University of Melbourne, Parkville, VIC, Australia; Australian-German Climate and Energy College, University of Melbourne, Parkville, VIC, Australia; Department of Environmental Health, Harvard T H Chan School of Public Health, Boston, MA, USA. Electronic address: caropark@g.harvard.edu. 2. Australian-German Climate and Energy College, University of Melbourne, Parkville, VIC, Australia. 3. Department of Medicine at the Doherty Institute, University of Melbourne, Parkville, VIC, Australia. 4. Department of Environmental Health, Harvard T H Chan School of Public Health, Boston, MA, USA; Harvard University Center for the Environment, Cambridge, MA, USA. 5. Health Research Institute, Faculty of Health, University of Canberra, Bruce, ACT, Australia; Department of Medicine, St Vincent's Hospital, University of Melbourne, Fitzroy, VIC, Australia. 6. Department of Medicine at the Doherty Institute, University of Melbourne, Parkville, VIC, Australia; Victorian Infectious Diseases Service, The Royal Melbourne Hospital, Parkville, VIC, Australia.
Abstract
BACKGROUND: To date, the effects of extreme weather events on nutrient supply within the population have not been quantified. In this study, we investigated micronutrient, macronutrient, and fibre supply changes during 175 extreme weather events within 87 countries in the year that a major extreme weather event occurred, with a targeted focus on low-income settings. METHODS: We collected data from the International Disasters Database and the Global Expanded Nutrient Supply model for the period 1961-2010, and applied superposed epoch analysis to calculate the percentage change in nutrient supply during the year of an extreme weather event relative to its historical context. We composited globally and by subgroup (EU, landlocked developing countries, least developed countries, low-income food deficit countries, and net food-importing developing countries). Lastly, we reported nutrient supply changes in terms of recommended dietary allowance for children aged 1-3 years. FINDINGS: Globally, all micronutrient supplies had a modest negative percentage change during the year of an extreme weather event; of these effects, those that reached an α=0·05 significance level included calcium, folate, thiamin, vitamin B6, and vitamin C, with nutrient supply changes ranging from -0·40 to -1·73% of the average supply. The effect of an extreme weather event was especially magnified among landlocked developing countries and low-income food deficit countries, with significant nutrient supply changes ranging from -1·61 to -7·57% of the average supply. Furthermore, the observed nutrient supply deficits in landlocked developing countries constituted a large percentage (ranging from 1·95 to 39·19%) of what a healthy child's sufficient average dietary intake should be. INTERPRETATION: The global effects of extreme weather events on nutrient supply found in this study are modest in isolation; however, in the context of nutrient needs for healthy child development in low-income settings, the effects observed are substantial. FUNDING: Australian-American Fulbright Commission.
BACKGROUND: To date, the effects of extreme weather events on nutrient supply within the population have not been quantified. In this study, we investigated micronutrient, macronutrient, and fibre supply changes during 175 extreme weather events within 87 countries in the year that a major extreme weather event occurred, with a targeted focus on low-income settings. METHODS: We collected data from the International Disasters Database and the Global Expanded Nutrient Supply model for the period 1961-2010, and applied superposed epoch analysis to calculate the percentage change in nutrient supply during the year of an extreme weather event relative to its historical context. We composited globally and by subgroup (EU, landlocked developing countries, least developed countries, low-income food deficit countries, and net food-importing developing countries). Lastly, we reported nutrient supply changes in terms of recommended dietary allowance for children aged 1-3 years. FINDINGS: Globally, all micronutrient supplies had a modest negative percentage change during the year of an extreme weather event; of these effects, those that reached an α=0·05 significance level included calcium, folate, thiamin, vitamin B6, and vitamin C, with nutrient supply changes ranging from -0·40 to -1·73% of the average supply. The effect of an extreme weather event was especially magnified among landlocked developing countries and low-income food deficit countries, with significant nutrient supply changes ranging from -1·61 to -7·57% of the average supply. Furthermore, the observed nutrient supply deficits in landlocked developing countries constituted a large percentage (ranging from 1·95 to 39·19%) of what a healthy child's sufficient average dietary intake should be. INTERPRETATION: The global effects of extreme weather events on nutrient supply found in this study are modest in isolation; however, in the context of nutrient needs for healthy child development in low-income settings, the effects observed are substantial. FUNDING: Australian-American Fulbright Commission.