Browsing by Author "Acquaotta, Fiorella"
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- Associations Between Extreme Temperatures and Cardiovascular Cause-Specific Mortality: Results From 27 CountriesPublication . Alahmad, Barrak; Khraishah, Haitham; Royé, Dominic; Vicedo-Cabrera, Ana Maria; Guo, Yuming; Papatheodorou, Stefania I.; Achilleos, Souzana; Acquaotta, Fiorella; Armstrong, Ben; Bell, Michelle L.; Pan, Shih-Chun; Coelho, Micheline de Sousa Zanotti Stagliorio; Colistro, Valentina; Dang, Tran Ngoc; Dung, Do-Van; De' Donato, Francesca K.; Entezari, Alireza; Guo, Yue-Liang Leon; Hashizume, Masahiro; Honda, Yasushi; Indermitte, Ene; Íñiguez, Carmen; Jaakkola, Jouni J.K.; Kim, Ho; Lavigne, Eric; Lee, Whanhee; Li, Shanshan; Madureira, Joana; Mayvaneh, Fatemeh; Orru, Hans; Overcenco, Ala Vladimir; Ragettli, Martina S.; Ryti, Niilo R.I.; Saldiva, Paulo Hilario Nascimento; Scovronick, Noah; Seposo, Xerxes; Sera, Francesco; Silva, Susana; Stafoggia, Massimo; Tobias, Aurelio; Garshick, Eric; Bernstein, Aaron S.; Zanobetti, Antonella; Schwartz, Joel D.; Gasparrini, Antonio; Koutrakis, PetrosBackground: Cardiovascular disease is the leading cause of death worldwide. Existing studies on the association between temperatures and cardiovascular deaths have been limited in geographic zones and have generally considered associations with total cardiovascular deaths rather than cause-specific cardiovascular deaths. Methods: We used unified data collection protocols within the Multi-Country Multi-City Collaborative Network to assemble a database of daily counts of specific cardiovascular causes of death from 567 cities in 27 countries across 5 continents in overlapping periods ranging from 1979 to 2019. City-specific daily ambient temperatures were obtained from weather stations and climate reanalysis models. To investigate cardiovascular mortality associations with extreme hot and cold temperatures, we fit case-crossover models in each city and then used a mixed-effects meta-analytic framework to pool individual city estimates. Extreme temperature percentiles were compared with the minimum mortality temperature in each location. Excess deaths were calculated for a range of extreme temperature days. Results: The analyses included deaths from any cardiovascular cause (32 154 935), ischemic heart disease (11 745 880), stroke (9 351 312), heart failure (3 673 723), and arrhythmia (670 859). At extreme temperature percentiles, heat (99th percentile) and cold (1st percentile) were associated with higher risk of dying from any cardiovascular cause, ischemic heart disease, stroke, and heart failure as compared to the minimum mortality temperature, which is the temperature associated with least mortality. Across a range of extreme temperatures, hot days (above 97.5th percentile) and cold days (below 2.5th percentile) accounted for 2.2 (95% empirical CI [eCI], 2.1–2.3) and 9.1 (95% eCI, 8.9–9.2) excess deaths for every 1000 cardiovascular deaths, respectively. Heart failure was associated with the highest excess deaths proportion from extreme hot and cold days with 2.6 (95% eCI, 2.4–2.8) and 12.8 (95% eCI, 12.2–13.1) for every 1000 heart failure deaths, respectively. Conclusions: Across a large, multinational sample, exposure to extreme hot and cold temperatures was associated with a greater risk of mortality from multiple common cardiovascular conditions. The intersections between extreme temperatures and cardiovascular health need to be thoroughly characterized in the present day—and especially under a changing climate.
- Effect modification of greenness on the association between heat and mortality: A multi-city multi-country studyPublication . Choi, Hayon Michelle; Lee, Whanhee; Roye, Dominic; Heo, Seulkee; Urban, Aleš; Entezari, Alireza; Vicedo-Cabrera, Ana Maria; Zanobetti, Antonella; Gasparrini, Antonio; Analitis, Antonis; Tobias, Aurelio; Armstrong, Ben; Forsberg, Bertil; Íñiguez, Carmen; Åström, Christofer; Indermitte, Ene; Lavigne, Eric; Mayvaneh, Fatemeh; Acquaotta, Fiorella; Sera, Francesco; Orru, Hans; Kim, Ho; Kyselý, Jan; Madueira, Joana; Schwartz, Joel; Jaakkola, Jouni J.K.; Katsouyanni, Klea; Diaz, Magali Hurtado; Ragettli, Martina S.; Pascal, Mathilde; Ryti, Niilo; Scovronick, Noah; Osorio, Samuel; Tong, Shilu; Seposo, Xerxes; Guo, Yue Leon; Guo, Yuming; Bell, Michelle L.Background: Identifying how greenspace impacts the temperature-mortality relationship in urban environments is crucial, especially given climate change and rapid urbanization. However, the effect modification of greenspace on heat-related mortality has been typically focused on a localized area or single country. This study examined the heat-mortality relationship among different greenspace levels in a global setting. Methods: We collected daily ambient temperature and mortality data for 452 locations in 24 countries and used Enhanced Vegetation Index (EVI) as the greenspace measurement. We used distributed lag non-linear model to estimate the heat-mortality relationship in each city and the estimates were pooled adjusting for city-specific average temperature, city-specific temperature range, city-specific population density, and gross domestic product (GDP). The effect modification of greenspace was evaluated by comparing the heat-related mortality risk for different greenspace groups (low, medium, and high), which were divided into terciles among 452 locations. Findings: Cities with high greenspace value had the lowest heat-mortality relative risk of 1·19 (95% CI: 1·13, 1·25), while the heat-related relative risk was 1·46 (95% CI: 1·31, 1·62) for cities with low greenspace when comparing the 99th temperature and the minimum mortality temperature. A 20% increase of greenspace is associated with a 9·02% (95% CI: 8·88, 9·16) decrease in the heat-related attributable fraction, and if this association is causal (which is not within the scope of this study to assess), such a reduction could save approximately 933 excess deaths per year in 24 countries. Interpretation: Our findings can inform communities on the potential health benefits of greenspaces in the urban environment and mitigation measures regarding the impacts of climate change.
- Extreme Temperatures and Stroke Mortality: Evidence From a Multi-Country AnalysisPublication . Alahmad, Barrak ; Khraishah, Haitham ; Kamineni, Meghana ; Royé, Dominic ; Papatheodorou, Stefania I. ; Vicedo-Cabrera, Ana Maria ; Guo, Yuming ; Lavigne, Eric ; Armstrong, Ben ; Sera, Francesco ; Bernstein, Aaron S. ; Zanobetti, Antonella ; Garshick, Eric ; Schwartz, Joel ; Bell, Michelle L. ; Al-Mulla, Fahd; Koutrakis, Petros ; Gasparrini, Antonio ; Souzana, Achilleos ; Acquaotta, Fiorella ; Pan, Shih-Chun ; Coelho, Micheline Sousa Zanotti Stagliorio ; Colistro, Valentina ; Dang, Tran Ngoc ; Van Dung, Do ; De’ Donato, Francesca K. ; Entezari, Alireza ; Leon Guo, Yue-Liang ; Hashizume, Masahiro ; Honda, Yasushi ; Indermitte, Ene ; Íñiguez, Carmen; Jaakkola, Jouni J.K. ; Kim, Ho ; Lee, Whanhee; Li, Shanshan ; Madureira, Joana ; Mayvaneh, Fatemeh ; Orru, Hans ; Overcenco, Ala ; Ragettli, Martina S. ; Ryti, Niilo R.I. ; Saldiva, Paulo Hilario Nascimento; Scovronick, Noah ; Seposo, Xerxes ; das Neves Pereira da Silva, Susana; Stafoggia, Massimo ; Tobias, AurelioBackground: Extreme temperatures contribute significantly to global mortality. While previous studies on temperature and stroke-specific outcomes presented conflicting results, these studies were predominantly limited to single-city or single-country analyses. Their findings are difficult to synthesize due to variations in methodologies and exposure definitions. Methods: Within the Multi-Country Multi-City Network, we built a new mortality database for ischemic and hemorrhagic stroke. Applying a unified analysis protocol, we conducted a multinational case-crossover study on the relationship between extreme temperatures and stroke. In the first stage, we fitted a conditional quasi-Poisson regression for daily mortality counts with distributed lag nonlinear models for temperature exposure separately for each city. In the second stage, the cumulative risk from each city was pooled using mixed-effect meta-analyses, accounting for clustering of cities with similar features. We compared temperature-stroke associations across country-level gross domestic product per capita. We computed excess deaths in each city that are attributable to the 2.5% hottest and coldest of days based on each city's temperature distribution. Results: We collected data for a total of 3 443 969 ischemic strokes and 2 454 267 hemorrhagic stroke deaths from 522 cities in 25 countries. For every 1000 ischemic stroke deaths, we found that extreme cold and hot days contributed 9.1 (95% empirical CI, 8.6-9.4) and 2.2 (95% empirical CI, 1.9-2.4) excess deaths, respectively. For every 1000 hemorrhagic stroke deaths, extreme cold and hot days contributed 11.2 (95% empirical CI, 10.9-11.4) and 0.7 (95% empirical CI, 0.5-0.8) excess deaths, respectively. We found that countries with low gross domestic product per capita were at higher risk of heat-related hemorrhagic stroke mortality than countries with high gross domestic product per capita (P=0.02). Conclusions: Both extreme cold and hot temperatures are associated with an increased risk of dying from ischemic and hemorrhagic strokes. As climate change continues to exacerbate these extreme temperatures, interventional strategies are needed to mitigate impacts on stroke mortality, particularly in low-income countries.
- Fluctuating temperature modifies heat-mortality association around the globePublication . Wu, Yao; Wen, Bo; Li, Shanshan; Gasparrini, Antonio; Tong, Shilu; Overcenco, Ala; Urban, Aleš; Schneider, Alexandra; Entezari, Alireza; Vicedo-Cabrera, Ana Maria; Zanobetti, Antonella; Analitis, Antonis; Zeka, Ariana; Tobias, Aurelio; Alahmad, Barrak; Armstrong, Ben; Forsberg, Bertil; Íñiguez, Carmen; Ameling, Caroline; De la Cruz Valencia, César; Åström, Christofer; Houthuijs, Danny; Van Dung, Do; Royé, Dominic; Indermitte, Ene; Lavigne, Eric; Mayvaneh, Fatemeh; Acquaotta, Fiorella; de’Donato, Francesca; Sera, Francesco; Carrasco-Escobar, Gabriel; Kan, Haidong; Orru, Hans; Kim, Ho; Holobaca, Iulian-Horia; Kyselý, Jan; Madureira, Joana; Schwartz, Joel; Katsouyanni, Klea; Hurtado-Diaz, Magali; Ragettli, Martina S.; Hashizume, Masahiro; Pascal, Mathilde; de Sousa Zanotti Stagliorio Coélho, Micheline; Scovronick, Noah; Michelozzi, Paola; Goodman, Patrick; Nascimento Saldiva, Paulo Hilario; Abrutzky, Rosana; Osorio, Samuel; Dang, Tran Ngoc; Colistro, Valentina; Huber, Veronika; Lee, Whanhee; Seposo, Xerxes; Honda, Yasushi; Bell, Michelle L.; Guo, YumingStudies have investigated the effects of heat and temperature variability (TV) on mortality. However, few assessed whether TV modifies the heat-mortality association. Data on daily temperature and mortality in the warm season were collected from 717 locations across 36 countries. TV was calculated as the standard deviation of the average of the same and previous days' minimum and maximum temperatures. We used location-specific quasi-Poisson regression models with an interaction term between the cross-basis term for mean temperature and quartiles of TV to obtain heat-mortality associations under each quartile of TV, and then pooled estimates at the country, regional, and global levels. Results show the increased risk in heat-related mortality with increments in TV, accounting for 0.70% (95% confidence interval [CI]: -0.33 to 1.69), 1.34% (95% CI: -0.14 to 2.73), 1.99% (95% CI: 0.29-3.57), and 2.73% (95% CI: 0.76-4.50) of total deaths for Q1-Q4 (first quartile-fourth quartile) of TV. The modification effects of TV varied geographically. Central Europe had the highest attributable fractions (AFs), corresponding to 7.68% (95% CI: 5.25-9.89) of total deaths for Q4 of TV, while the lowest AFs were observed in North America, with the values for Q4 of 1.74% (95% CI: -0.09 to 3.39). TV had a significant modification effect on the heat-mortality association, causing a higher heat-related mortality burden with increments of TV. Implementing targeted strategies against heat exposure and fluctuant temperatures simultaneously would benefit public health.
- Geographical Variations of the Minimum Mortality Temperature at a Global ScalePublication . Tobías, Aurelio; Hashizume, Masahiro; Honda, Yasushi; Sera, Francesco; Ng, Chris Fook Sheng; Kim, Yoonhee; Roye, Dominic; Chung, Yeonseung; Dang, Tran Ngoc; Kim, Ho; Lee, Whanhee; Íñiguez, Carmen; Vicedo-Cabrera, Ana; Abrutzky, Rosana; Guo, Yuming; Tong, Shilu; Coelho, Micheline de Sousa Zanotti Stagliorio; Saldiva, Paulo Hilario Nascimento; Lavigne, Eric; Correa, Patricia Matus; Ortega, Nicolás Valdés; Kan, Haidong; Osorio, Samuel; Kyselý, Jan; Urban, Aleš; Orru, Hans; Indermitte, Ene; Jaakkola, Jouni J.K.; Ryti, Niilo R.I.; Pascal, Mathilde; Huber, Veronika; Schneider, Alexandra; Katsouyanni, Klea; Analitis, Antonis; Entezari, Alireza; Mayvaneh, Fatemeh; Goodman, Patrick; Zeka, Ariana; Michelozzi, Paola; de’Donato, Francesca; Alahmad, Barrak; Diaz, Magali Hurtado; De la Cruz Valencia, César; Overcenco, Ala; Houthuijs, Danny; Ameling, Caroline; Rao, Shilpa; Di Ruscio, Francesco; Carrasco, Gabriel; Seposo, Xerxes; Nunes, Baltazar; Madureira, Joana; Holobaca, Iulian-Horia; Scovronick, Noah; Acquaotta, Fiorella; Forsberg, Bertil; Åström, Christofer; Ragettli, Martina S.; Guo, Yue-Liang Leon; Chen, Bing-Yu; Li, Shanshan; Colistro, Valentina; Zanobetti, Antonella; Schwartz, Joel; Dung, Do Van; Armstrong, Ben; Gasparrini, AntonioBackground: Minimum mortality temperature (MMT) is an important indicator to assess the temperature-mortality association, indicating long-term adaptation to local climate. Limited evidence about the geographical variability of the MMT is available at a global scale. Methods: We collected data from 658 communities in 43 countries under different climates. We estimated temperature-mortality associations to derive the MMT for each community using Poisson regression with distributed lag nonlinear models. We investigated the variation in MMT by climatic zone using a mixed-effects meta-analysis and explored the association with climatic and socioeconomic indicators. Results: The geographical distribution of MMTs varied considerably by country between 14.2 and 31.1 °C decreasing by latitude. For climatic zones, the MMTs increased from alpine (13.0 °C) to continental (19.3 °C), temperate (21.7 °C), arid (24.5 °C), and tropical (26.5 °C). The MMT percentiles (MMTPs) corresponding to the MMTs decreased from temperate (79.5th) to continental (75.4th), arid (68.0th), tropical (58.5th), and alpine (41.4th). The MMTs indreased by 0.8 °C for a 1 °C rise in a community's annual mean temperature, and by 1 °C for a 1 °C rise in its SD. While the MMTP decreased by 0.3 centile points for a 1 °C rise in a community's annual mean temperature and by 1.3 for a 1 °C rise in its SD. Conclusions: The geographical distribution of the MMTs and MMTPs is driven mainly by the mean annual temperature, which seems to be a valuable indicator of overall adaptation across populations. Our results suggest that populations have adapted to the average temperature, although there is still more room for adaptation.
- Global, regional, and national burden of mortality associated with cold spells during 2000–19: a three-stage modelling studyPublication . Gao, Yuan; Huang, Wenzhong; Zhao, Qi; Ryti, Niilo; Armstrong, Ben; Gasparrini, Antonio; Tong, Shilu; Pascal, Mathilde; Urban, Aleš; Zeka, Ariana; Lavigne, Eric; Madureira, Joana; Goodman, Patrick; Huber, Veronika; Forsberg, Bertil; Kyselý, Jan; Sera, Francesco; Guo, Yuming; Li, Shanshan; Gao, Yuan; Huang, Wenzhong; Zhao, Qi; Ryti, Niilo; Armstrong, Ben; Gasparrini, Antonio; Tong, Shilu; Pascal, Mathilde; Urban, Aleš; Zeka, Ariana; Lavigne, Eric; Madureira, Joana; Goodman, Patrick; Huber, Veronika; Forsberg, Bertil; Kyselý, Jan; Sera, Francesco; Bell, Michelle; Simon Hales; Honda, Yasushi; Jaakkola, Jouni J.K.; Tobias, Aurelio; Vicedo-Cabrera, Ana Maria; Abrutzky, Rosana; Coelho, Micheline de Sousa Zanotti Stagliorio; Saldiva, Paulo Hilario Nascimento; Correa, Patricia Matus; Ortega, Nicolás Valdés; Kan, Haidong; Osorio, Samuel; Roye, Dominic; Orru, Hans; Indermitte, Ene; Schneider, Alexandra; Katsouyanni, Klea; Analitis, Antonis; Carlsen, Hanne Krage; Mayvaneh, Fatemeh; Roradeh, Hematollah; Raz, Raanan; Michelozzi, Paola; de'Donato, Francesca; Hashizume, Masahiro; Kim, Yoonhee; Alahmad, Barrak; Cauchy, John Paul; Diaz, Magali Hurtado; Arellano, Eunice Elizabeth Félix; Valencia, César De la Cruz; Overcenco, Ala; Houthuijs, Danny; Ameling, Caroline; Rao, Shilpa; Carrasco, Gabriel; Seposo, Xerxes; Chua, Paul Lester Carlos; Silva, Susana das Neves Pereira da; Nunes, Baltazar; Holobaca, Iulian-Horia; Cvijanovic, Ivana; Mistry, Malcolm; Scovronick, Noah; Acquaotta, Fiorella; Kim, Ho; Lee, Whanhee; Íñiguez, Carmen; Åström, Christofer; Ragettli, Martina S.; Guo, Yue Leon; Pan, Shih-Chun; Colistro, Valentina; Zanobetti, Antonella; Schwartz, Joel; Dang, Tran Ngoc; Dung, Do Van; Guo, Yuming; Li, ShanshanBackground: Exposure to cold spells is associated with mortality. However, little is known about the global mortality burden of cold spells. Methods: A three-stage meta-analytical method was used to estimate the global mortality burden associated with cold spells by means of a time series dataset of 1960 locations across 59 countries (or regions). First, we fitted the location-specific, cold spell-related mortality associations using a quasi-Poisson regression with a distributed lag non-linear model with a lag period of up to 21 days. Second, we built a multivariate meta-regression model between location-specific associations and seven predictors. Finally, we predicted the global grid-specific cold spell-related mortality associations during 2000-19 using the fitted meta-regression model and the yearly grid-specific meta-predictors. We calculated the annual excess deaths, excess death ratio (excess deaths per 1000 deaths), and excess death rate (excess deaths per 100 000 population) due to cold spells for each grid across the world. Findings: Globally, 205 932 (95% empirical CI [eCI] 162 692-250 337) excess deaths, representing 3·81 (95% eCI 2·93-4·71) excess deaths per 1000 deaths (excess death ratio), and 3·03 (2·33-3·75) excess deaths per 100 000 population (excess death rate) were associated with cold spells per year between 2000 and 2019. The annual average global excess death ratio in 2016-19 increased by 0·12 percentage points and the excess death rate in 2016-19 increased by 0·18 percentage points, compared with those in 2000-03. The mortality burden varied geographically. The excess death ratio and rate were highest in Europe, whereas these indicators were lowest in Africa. Temperate climates had higher excess death ratio and rate associated with cold spells than other climate zones. Interpretation: Cold spells are associated with substantial mortality burden around the world with geographically varying patterns. Although the number of cold spells has on average been decreasing since year 2000, the public health threat of cold spells remains substantial. The findings indicate an urgency of taking local and regional measures to protect the public from the mortality burdens of cold spells. Funding: Australian Research Council, Australian National Health and Medical Research Council, EU's Horizon 2020 Project Exhaustion.
- Global, regional, and national burden of mortality associated with non-optimal ambient temperatures from 2000 to 2019: a three-stage modelling studyPublication . Zhao, Qi; Guo, Yuming; Ye, Tingting; Gasparrini, Antonio; Tong, Shilu; Overcenco, Ala; Urban, Aleš; Schneider, Alexandra; Entezari, Alireza; Vicedo-Cabrera, Ana Maria; Zanobetti, Antonella; Analitis, Antonis; Zeka, Ariana; Tobias, Aurelio; Nunes, Baltazar; Alahmad, Barrak; Armstrong, Ben; Forsberg, Bertil; Pan, Shih-Chun; Íñiguez, Carmen; Ameling, Caroline; De la Cruz Valencia, César; Åström, Christofer; Houthuijs, Danny; Dung, Do Van; Royé, Dominic; Indermitte, Ene; Lavigne, Eric; Mayvaneh, Fatemeh; Acquaotta, Fiorella; de'Donato, Francesca; Di Ruscio, Francesco; Sera, Francesco; Carrasco-Escobar, Gabriel; Kan, Haidong; Orru, Hans; Kim, Ho; Holobaca, Iulian-Horia; Kyselý, Jan; Madureira, Joana; Schwartz, Joel; Jaakkola, Jouni J.K.; Katsouyanni, Klea; Hurtado Diaz, Magali; Ragettli, Martina S.; Hashizume, Masahiro; Pascal, Mathilde; de Sousa Zanotti Stagliorio Coélho, Micheline; Valdés Ortega, Nicolás; Ryti, Niilo; Scovronick, Noah; Michelozzi, Paola; Matus Correa, Patricia; Goodman, Patrick; Nascimento Saldiva, Paulo Hilario; Abrutzky, Rosana; Osorio, Samuel; Rao, Shilpa; Fratianni, Simona; Dang, Tran Ngoc; Colistro, Valentina; Huber, Veronika; Lee, Whanhee; Seposo, Xerxes; Honda, Yasushi; Guo, Yue Leon; Bell, Michelle L.; Li, ShanshanBackground: Exposure to cold or hot temperatures is associated with premature deaths. We aimed to evaluate the global, regional, and national mortality burden associated with non-optimal ambient temperatures. Methods: In this modelling study, we collected time-series data on mortality and ambient temperatures from 750 locations in 43 countries and five meta-predictors at a grid size of 0·5° × 0·5° across the globe. A three-stage analysis strategy was used. First, the temperature-mortality association was fitted for each location by use of a time-series regression. Second, a multivariate meta-regression model was built between location-specific estimates and meta-predictors. Finally, the grid-specific temperature-mortality association between 2000 and 2019 was predicted by use of the fitted meta-regression and the grid-specific meta-predictors. Excess deaths due to non-optimal temperatures, the ratio between annual excess deaths and all deaths of a year (the excess death ratio), and the death rate per 100 000 residents were then calculated for each grid across the world. Grids were divided according to regional groupings of the UN Statistics Division. Findings: Globally, 5 083 173 deaths (95% empirical CI [eCI] 4 087 967-5 965 520) were associated with non-optimal temperatures per year, accounting for 9·43% (95% eCI 7·58-11·07) of all deaths (8·52% [6·19-10·47] were cold-related and 0·91% [0·56-1·36] were heat-related). There were 74 temperature-related excess deaths per 100 000 residents (95% eCI 60-87). The mortality burden varied geographically. Of all excess deaths, 2 617 322 (51·49%) occurred in Asia. Eastern Europe had the highest heat-related excess death rate and Sub-Saharan Africa had the highest cold-related excess death rate. From 2000-03 to 2016-19, the global cold-related excess death ratio changed by -0·51 percentage points (95% eCI -0·61 to -0·42) and the global heat-related excess death ratio increased by 0·21 percentage points (0·13-0·31), leading to a net reduction in the overall ratio. The largest decline in overall excess death ratio occurred in South-eastern Asia, whereas excess death ratio fluctuated in Southern Asia and Europe. Interpretation: Non-optimal temperatures are associated with a substantial mortality burden, which varies spatiotemporally. Our findings will benefit international, national, and local communities in developing preparedness and prevention strategies to reduce weather-related impacts immediately and under climate change scenarios.
- Projections of excess mortality related to diurnal temperature range under climate change scenarios: a multi-country modelling studyPublication . Lee, Whanhee; Kim, Yoonhee; Sera, Francesco; Gasparrini, Antonio; Park, Rokjin; Michelle Choi, Hayon; Prifti, Kristi; Bell, Michelle L.; Abrutzky, Rosana; Guo, Yuming; Tong, Shilu; de Sousa Zanotti Stagliorio Coelho, Micheline; Nascimento Saldiva, Paulo Hilario; Lavigne, Eric; Orru, Hans; Indermitte, Ene; Jaakkola, Jouni J.K.; Ryti, Niilo R.I.; Pascal, Mathilde; Goodman, Patrick; Zeka, Ariana; Hashizume, Masahiro; Honda, Yasushi; Hurtado Diaz, Magali; César Cruz, Julio; Overcenco, Ala; Nunes, Baltazar; Madureira, Joana; Scovronick, Noah; Acquaotta, Fiorella; Tobias, Aurelio; Vicedo-Cabrera, Ana Maria; Ragettli, Martina S.; Guo, Yue-Liang Leon; Chen, Bing-Yu; Li, Shanshan; Armstrong, Ben; Zanobetti, Antonella; Schwartz, Joel; Kim, HoBackground: Various retrospective studies have reported on the increase of mortality risk due to higher diurnal temperature range (DTR). This study projects the effect of DTR on future mortality across 445 communities in 20 countries and regions. Methods: DTR-related mortality risk was estimated on the basis of the historical daily time-series of mortality and weather factors from Jan 1, 1985, to Dec 31, 2015, with data for 445 communities across 20 countries and regions, from the Multi-Country Multi-City Collaborative Research Network. We obtained daily projected temperature series associated with four climate change scenarios, using the four representative concentration pathways (RCPs) described by the Intergovernmental Panel on Climate Change, from the lowest to the highest emission scenarios (RCP 2.6, RCP 4.5, RCP 6.0, and RCP 8.5). Excess deaths attributable to the DTR during the current (1985-2015) and future (2020-99) periods were projected using daily DTR series under the four scenarios. Future excess deaths were calculated on the basis of assumptions that warmer long-term average temperatures affect or do not affect the DTR-related mortality risk. Findings: The time-series analyses results showed that DTR was associated with excess mortality. Under the unmitigated climate change scenario (RCP 8.5), the future average DTR is projected to increase in most countries and regions (by -0·4 to 1·6°C), particularly in the USA, south-central Europe, Mexico, and South Africa. The excess deaths currently attributable to DTR were estimated to be 0·2-7·4%. Furthermore, the DTR-related mortality risk increased as the long-term average temperature increased; in the linear mixed model with the assumption of an interactive effect with long-term average temperature, we estimated 0·05% additional DTR mortality risk per 1°C increase in average temperature. Based on the interaction with long-term average temperature, the DTR-related excess deaths are projected to increase in all countries or regions by 1·4-10·3% in 2090-99. Interpretation: This study suggests that globally, DTR-related excess mortality might increase under climate change, and this increasing pattern is likely to vary between countries and regions. Considering climatic changes, our findings could contribute to public health interventions aimed at reducing the impact of DTR on human health.
- Rainfall events and daily mortality across 645 global locations: two stage time series analysisPublication . He, Cheng; Breitner-Busch, Susanne; Huber, Veronika; Chen, Kai; Zhang, Siqi; Gasparrini, Antonio; Bell, Michelle; Kan, Haidong; Royé, Dominic; Armstrong, Ben; Schwartz, Joel; Sera, Francesco; Vicedo-Cabrera, Ana Maria; Honda, Yasushi; Jaakkola, Jouni J.K.; Ryti, Niilo; Kyselý, Jan; Guo, Yuming; Tong, Shilu; de’Donato, Francesca; Michelozzi, Paola; Coelho, Micheline de Sousa Zanotti Staglior; Saldiva, Paulo Hilario Nascimento; Lavigne, Eric; Orru,Hans; Indermitte, Ene; Pascal, Mathilde; Goodman, Patrick; Zeka, Ariana; Kim, Yoonhee; Diaz, Magali Hurtado; Arellano, Eunice Elizabeth Félix; Overcenco, Ala; Klompmaker, Jochem; Rao, Shilpa; Palomares, Alfonso Diz-Lois; Carrasco, Gabriel; Seposo, Xerxes; das Neves Pereira da Silva, Susana; Joana Madureira; Holobaca, Iulian-Horia; Scovronick, Noah; Acquaotta, Fiorella; Kim, Ho; Lee, Whanhee; Hashizume, Masahiro; Tobias, Aurelio; Íñiguez, Carmen; Forsberg, Bertil; Ragettli, Martina S.; Guo, Yue Leon; Pan, Shih-Chun; Osorio, Samuel; Li, Shanshan; Zanobetti, Antonella; Dang, Tran Ngoc; Dung, Do Van; Schneider. AlexandraObjective: To examine the associations between characteristics of daily rainfall (intensity, duration, and frequency) and all cause, cardiovascular, and respiratory mortality. Design: Two stage time series analysis. Setting: 645 locations across 34 countries or regions. Population: Daily mortality data, comprising a total of 109 954 744 all cause, 31 164 161 cardiovascular, and 11 817 278 respiratory deaths from 1980 to 2020. Main outcome measure: Association between daily mortality and rainfall events with return periods (the expected average time between occurrences of an extreme event of a certain magnitude) of one year, two years, and five years, with a 14 day lag period. A continuous relative intensity index was used to generate intensity-response curves to estimate mortality risks at a global scale. Results: During the study period, a total of 50 913 rainfall events with a one year return period, 8362 events with a two year return period, and 3301 events with a five year return period were identified. A day of extreme rainfall with a five year return period was significantly associated with increased daily all cause, cardiovascular, and respiratory mortality, with cumulative relative risks across 0-14 lag days of 1.08 (95% confidence interval 1.05 to 1.11), 1.05 (1.02 to 1.08), and 1.29 (1.19 to 1.39), respectively. Rainfall events with a two year return period were associated with respiratory mortality only, whereas no significant associations were found for events with a one year return period. Non-linear analysis revealed protective effects (relative risk <1) with moderate-heavy rainfall events, shifting to adverse effects (relative risk >1) with extreme intensities. Additionally, mortality risks from extreme rainfall events appeared to be modified by climate type, baseline variability in rainfall, and vegetation coverage, whereas the moderating effects of population density and income level were not significant. Locations with lower variability of baseline rainfall or scarce vegetation coverage showed higher risks. Conclusion: Daily rainfall intensity is associated with varying health effects, with extreme events linked to an increasing relative risk for all cause, cardiovascular, and respiratory mortality. The observed associations varied with local climate and urban infrastructure.
- Regional variation in the role of humidity on city-level heat-related mortalityPublication . Guo, Qiang; Mistry, Malcolm N.; Zhou, Xudong; Zhao, Gang; Kino, Kanon; Wen, Bo; Yoshimura, Kei; Satoh, Yusuke; Cvijanovic, Ivana; Kim, Yoonhee; Ng, Chris Fook Sheng; Vicedo-Cabrera, Ana M.; Armstrong, Ben; Urban, Aleš; Katsouyanni, Klea; Masselot, Pierre; Tong, Shilu; Sera, Francesco; Huber, Veronika; Bell, Michelle L.; Kyselý, Jan; Gasparrini, Antonio; Hashizume, Masahiro; Oki, Taikan; Abrutzky, Rosana; Guo, Yuming; de Sousa Zanotti Stagliorio Coelho, Micheline; Nascimento Saldiva, Paulo Hilario; Lavigne, Eric; Ortega, Nicolás Valdés; Correa, Patricia Matus; Kan, Haidong; Osorio, Samuel; Roye, Dominic; Indermitte, Ene; Orru, Hans; Jaakkola, Jouni J K.; Ryti, Niilo; Pascal, Mathilde; Schneider, Alexandra; Analitis, Antonis; Entezari, Alireza; Mayvaneh, Fatemeh; Zeka, Ariana; Goodman, Patrick; de'Donato, Francesca; Michelozzi, Paola; Alahmad, Barrak; De la Cruz Valencia, César; Hurtado Diaz, Magali; Overcenco, Ala; Ameling, Caroline; Houthuijs, Danny; Rao, Shilpa; Carrasco, Gabriel; Seposo, Xerxes; Madureira, Joana; Silva, Susana; Holobaca, Iulian-Horia; Acquaotta, Fiorella; Scovronick, Noah; Kim, Ho; Lee, Whanhee; Tobias, Aurelio; Íñiguez, Carmen; Forsberg, Bertil; Ragettli, Martina S.; Pan, Shih-Chun; Guo, Yue Leon; Li, Shanshan; Schneider, Rochelle; Colistro, Valentina; Zanobetti, Antonella; Schwartz, Joel; Van Dung, Do; Ngoc Dang, Tran; Honda, YasushiThe rising humid heat is regarded as a severe threat to human survivability, but the proper integration of humid heat into heat-health alerts is still being explored. Using state-of-the-art epidemiological and climatological datasets, we examined the association between multiple heat stress indicators (HSIs) and daily human mortality in 739 cities worldwide. Notable differences were observed in the long-term trends and timing of heat events detected by HSIs. Air temperature (Tair) predicts heat-related mortality well in cities with a robust negative Tair-relative humidity correlation (CT-RH). However, in cities with near-zero or weak positive CT-RH, HSIs considering humidity provide enhanced predictive power compared to Tair. Furthermore, the magnitude and timing of heat-related mortality measured by HSIs could differ largely from those associated with Tair in many cities. Our findings provide important insights into specific regions where humans are vulnerable to humid heat and can facilitate the further enhancement of heat-health alert systems.