INFLUENCE OF METEOROLOGICAL VARIABLES ON PEOPLE WITH CARDIOVASCULAR DISEASES IN BUCHAREST, ROMANIA (2011-2012)
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INFLUENCE OF METEOROLOGICAL VARIABLES ON PEOPLE WITH CARDIOVASCULAR DISEASES IN BUCHAREST, ROMANIA (2011-2012) MIRUNA-MIHAELA MICHEU 1, MARIUS-VICTOR BIRSAN 2†, ION-ANDREI NITA 2,3, MEDA-DANIELA ANDREI 2,4, DELIA NEBUNU 1, CAMELIA ACATRINEI 1, LUCIAN SFÎCĂ 3, RÓBERT SZÉP 5,6, ÁGNES KERESZTESI 5,6,7, PABLO FERNÁNDEZ DE ARRÓYABE HERNÁEZ 8, SEBASTIAN ONCIUL 1,9, ALEXANDRU SCAFA-UDRISTE 1,9, MARIA DOROBANTU 1,9 1 ) Clinical Emergency Hospital of Bucharest, Department of Cardiology. Bucharest, Romania. 2 ) Meteo Romania (National Meteorological Administration), Bucharest, Romania. 3 ) Alexandru Ioan Cuza University of Iași, Faculty of Geography, Iași, Romania. 4 ) University of Bucharest, Faculty of Physics, Doctoral School, Bucharest, Romania. 5 ) Institute for R&D in Hunting and Mountain Resources. Miercurea Ciuc, Romania. 6 ) Sapientia Hungarian University of Transylvania, Faculty of Economics, Socio-Human Science and Engineering, Department of Bioengineering. Miercurea Ciuc, Romania. 7 ) University of Pécs, Faculty of Natural Sciences, Doctoral School of Chemistry. Pécs, Hungary. 8 ) University of Cantabria, Faculty of Philosophy and Arts, Department of Geography, GEOBIOMET Research Group. Santander, Spain. 9 ) Carol Davila University of Medicine and Pharmacy, Department 4-Cardiothoracic Pathology. Bucharest, Romania. † ) Corresponding author. E-mail: marius.birsan@gmail.com Abstract. The study investigates the influence of weather on people with acute cardiovascular syndromes (ACS) in Bucharest, Romania, using daily records from October 2011 until December 2012. The highest number of cases with ACS occurred in February 2012, which was an abnormally cold month. Data aggregated at weekly scale show no significant correlations between the total number of ACS and the meteorological variables. However, after classifying the medical data into subgroups, we found statistically significant positive correlations (p < 0.05) between the number of female patients diagnosed with unstable angina and the Temperature-Humidity Index, as well as with air temperature. Key words: meteorological conditions; air temperature; thermal comfort; urban environment; acute coronary syndromes; extreme weather. 1. INTRODUCTION The study of the weather effects on human comfort is essential for assessing the impacts of climate variability and change on the human heath, especially in urban environments. Acute coronary syndrome (ACS) is one of the leading causes of early death and disease burden worldwide [1]. ACS comprises a spectrum of clinical conditions characterized by sudden onset of critical myocardial ischemia or necrosis, namely unstable angina (UA), non–ST-segment elevation myocardial infarction (NSTEMI), and ST-segment elevation myocardial infarction (STEMI)
2 [2]. Evidence from a plethora of studies conducted mostly in North America, Asia and Western Europe designates weather conditions as modifiers of cardiovascular morbidity and mortality [3–11]. However, considerably less information exists for Eastern Europe. Exposure to extreme temperatures has been showed to trigger various biological responses associated with increased atherothrombotic events. Potential mechanisms of cold-induced ACS include increased sympathetic activation with subsequent vasoconstriction, tachyarrhythmias and arterial hypertension, as well as hematological changes such as haemoconcentration, increase in blood viscosity, concentrations of clotting factors and platelet counts [12]. As for heat-related adaptive mechanisms, there is an intensification of skin blood flow and sweat rate to enable heat dissipation. The shift of blood flow from the central circulation to the skin along with dehydration impose a great effort on the cardiovascular system which has to maintain the perfusion of vital organs by increasing the cardiac output [13]. Even if at individual level the climate-related risk is rather small compared to other well-known risk factors (e.g., dyslipidemia and smoking), it represents a significant at population level, considering the huge number of people affected [12]. Importantly, weather-associated adverse health effects can be limited if using appropriate prevention strategies. Of note, not everyone is equally at risk, as the effects of meteorological variables might be more prominent in some particular sub-populations. Results cannot be generalized from other populations, since distinct features such as demographic and genetic factors may influence the impact of climate on human health. Therefore, it is important to identify country-specific weather-related health hazard and vulnerable groups as foundation for tailored public health interventions. Here we present the first study exploring hospital admissions associated with weather conditions in Bucharest, Romania, based on observational data from October 2011 until December 2012. The year 2012 was chosen because it was a year of weather extremes, subject to both cold and heat waves. This year was characterized by a winter with alternating blizzard and frost (the second coldest February on record), a rainy spring (the third most rainy May on record), which contributed, by the addition of water vapor in the atmosphere, at a high Temperature-Humidity, especially at the beginning of summer, and a very hot summer (first warmest July on record). The preceding three months of 2011 were also analyzed. Hence, even if short, this period brings a full image of different types of biometeorological stress, which are specific for the region. In 2012, the mean annual air temperature over Romania was 10°C, which is 1.1°C above the standard climatological normal (1961-1990). Positive anomalies of mean monthly air temperature varied between +0.3°C in March and +4.5°C in July, while negative anomalies were recorded in February and December, with –5.6°C and –1.5°C below the monthly climatological normal, respectively. In Bucharest, positive anomalies were recorded in the same ten months, ranging from +0.9°C (May) to +5.3°C (July). The largest negative anomaly was recorded in February: – 5.9°C, the coldest winter month of the last decade in Romania (Fig. 1).
3 2. DATA AND METHODS 2.1. LOCATION Bucharest is the capital of Romania and the largest city in the country, being located in the southeastern part of the country, less than 60 km north to the Danube river. The city has a humid continental climate (Dfa), with warm to hot, humid summers and cold, moderately snowy winters. Because of its position on the Romanian Plain, the winters can get windy, although some winds are diminished due to urbanization. Air temperature drops below 0°C during winter, and in summer can reach 35-40°C and rarely even more (e.g., 41.5°C recorded on 7 August 2012 at the Bucharest-Filaret weather station). Climatic changes in the region show increasing warm thermal extremes [14,15], resulting in increased sub- daily maximum precipitation [16,17]. Fig. 1 – Monthly mean air temperature anomalies (°C) for the study period with respect to the climatological normals (1961–1990). Observational data is from the Bucharest-Filaret station. 2.2. MEDICAL DATA We retrospectively analyzed the number of daily hospital admissions for ACS at the Clinical Emergency Hospital of Bucharest, Romania, during 15 months (10/2011-12/2012). The diagnosis was made according to the ESC guidelines [2,18]. Clinical data were collected by reviewing the medical record of each patient and were fully anonymized prior to any analysis. The study complied with the declaration of Helsinki and was approved by the Institutional Ethics Committee. Because of the retrospective nature of the study, the patients’ informed consent was not required.
4 2.3. METEOROLOGICAL DATA The meteorological data used in this study consists in daily records of air pressure, air temperature (average, minimum and maximum), wind speed, relative humidity from the Bucharest-Filaret weather station, covering the period Oct 2011- Dec 2012. Two indices that estimate the heat- and cold-related human discomfort were also computed: the temperature−humidity index (THI) and the wind chill equivalent temperature chart index (WCT), respectively. THI estimates the temperature felt by the human body in the warm season, by means of air temperature and relative humidity and is defined as [19,20]: THI = (TA × 1.8 + 32) − (0.55 − 0.55 × RH/100) × (TA × 1.8 − 26) (1) where TA is the air temperature (°C) and RH is the relative humidity measured at 2 m above ground. For the cold season, we used WCT [21] recommended by WMO [22]: WCT = 13.12 + 0.6215 × TA − 11.37 × FF100.16 + 0.3965 TA × FF100.16 (2) where TA is the air temperature (°C) measured at a standard level (2 m), and FF10 is the wind speed (km/h) measured at 10 m. The thresholds for various human discomfort classes are as follows: • Heat: uncomfortably hot: 66 ≤ THI < 80; severe danger from heat: THI ≥ 80; • Cold: uncomfortably cold: −20°C < WCT ≤ 0°C; extremely cold: −35°C < WCT ≤ −20°C; severe danger from cold: WCT ≤ −35°C. 2.4. METHODS Spearman’s rho is a nonparametric rank-based correlation coefficient used to estimate the monotone association between two random variables. It is computed from the difference d between the ranks of independently sorted variables x and y: 6 !!!! !!! ! =1− ! (3) !(!! − 1) Under the null hypothesis of no correlation between x and y, the distribution of ρ can be approximated by a normal distribution with mean µρ and variance σρ2 given by: !!!! !!! = 1/(! − 1)! (4) The random variables x and y are considered correlated at the significance level α (for a two-tailed test) if: ! > !! ! ! − 1! (5)
5 3. RESULTS Between October 2011 and December 2012, there were 920 hospital admissions for ACS. Over two thirds of cases were people of age over 60 years, and 68% were men. Baseline patient characteristics stratified by medical data, gender and age (
6 THI and WCT indices, as well as with air temperature (average, maximum and minimum). Fig. 2 – Number of monthly cases of acute myocardial infarction and unstable angina. Lower row shows the number of cases for people of age ≥60 years. Fig. 3 shows the evolution of ACS cases, which looks connected to air temperature. The cases are gradually multiplying from December to February, with the installation and persistence of winter very cold air mass. Later, there is a drop in the number of patients until May, with the gradual increase in air temperature and reduced heat stress. From June until August, the number of cases increases again, as temperature and warm thermal stress increase. In September, when it
7 wasn't so hot, the number of cases decreases, while in October it rises again due to high air temperature and pressure variations. From November to December, the number of cases decreases with the gradual decrease in air temperature. Fig. 3 – Evolution of the meteorological parameters during the study period.
8 In recent years, a plethora of studies addressed the relationship between weather conditions and ACS – whether as a whole or as a specific clinical entity. However, a direct comparison with prior findings is difficult due to heterogeneity in study design and statistical method. Inconsistent results have been reported in different populations and different geographical settings, as revealed by a comprehensive meta-analysis including 23 studies [23]. Accordingly, cold expo- sure, as well as exposure to heat waves were associated with an increased risk of AMI. Noteworthy, the latitude proved to be a modifier of ambient temperature - AMI relationship, namely an increase in latitude being associated with a decreased risk of the aforesaid disease due to cold exposure. Low temperatures have been associated with an increase in the incidence of ACS in studies conducted in regions with different climate. In Lithuania, Vencloviene et al. [24] indicated that more emergency calls for ACS were registered during the cold period. In a nationwide study covering 16 years of medical and weather data from 1998 to 2013 in Sweden [25], low air temperature, low atmospheric air pressure, high wind velocity, and shorter sunshine duration were linked with the occurrence of AMI, with the most evident association observed for air temperature. Particularly, ambient temperature remained negatively correlated with the risk of AMI even after stratifying into NSTEMI and STEMI in all health care regions except for northern areas. Seasonal variation of AMI incidence has been reported also in Germany, with lowest incidence and lowest mortality being witnessed in summer season [26]. In Japan, Honda et al. revealed that lower minimum temperature on the second day preceding the onset is an independent risk factor for AMI, particularly in female and elderly patients [27]. But the findings as regards the vulnerable subpopulations vary within studies. In a large population-based study comprising 81029 AMI cases in Beijing, a statistically significant correlation was found between short-term exposure to low temperatures and hospital admissions, males and subjects over 65 years old being more prone to the adverse effects of cold weather [28]. For northern Spain, Royé et al. [29] found that ambient temperature and particulate matter with a diameter smaller than 10 µm can be used as predictor for hospital admissions for AMI. Based on climate scenarios projecting increases in apparent summer temperatures of more than 4°C in eastern USA, Limaye et al. estimate that there will be 11,000 additional deaths due to warming in 2069 [30]. While many reports described winter peaks in cardiovascular hospitalization, recent evidence acknowledges heat exposure as a triggering factor for acute cardiac events, suggesting that the relationship is not linear, but U-shaped, with higher incidence in extremely low or high temperatures [31], which is in line with our results. Group-specific analysis revealed that the impact of high environmental temperature is age- and sex-dependent. Gebhard et al. identified increase outside air temperature and sunshine hours as positive predictors for the occurrence of STEMI in young women (≤55 years) but not in older women or men [32]. A study conducted in Hefei between July 1, 2015, and October 31, 2017 showed that the influence of increase air temperature on cardiovascular hospital admissions was stronger for females and in subjects over 65 years old – compared to male and younger patients who were more sensitive to low temperature [33]. Last but not least, this area of research needs further investigation, on longer time intervals (multi-decadal), since there is clear evidence of long-term changes in
9 air temperature, relative humidity and wind speed [34,35], as well as in large-scale atmospheric circulation in the region [36,37]. Another improvenemt would be to take additional factors into account, in particular air pollution [38] – are required to confirm the results and determine country-specific weather-related health hazard and vulnerable groups as foundation for tailored public health interventions. 5. CONCLUSIONS To the best of our knowledge, this is the first study exploring the association between meteorological conditions and ACS hospitalizations in Bucharest, Romania. For this purpose, we incorporated a variety of meteorological variables and performed sub-group analysis in terms of clinical entities, gender and age, so that specific conclusions can be drawn. The main limitation of our study concerns the time extent of the data records, which consist of only 15 months. Nevertheless, the 2012 year is considered a particularly capricious year from the climatic point of view (not only in Romania, but worldwide), containing both extreme cold episodes, as well as extensive heat waves. The main result regards the significant positive correlation between women diagnosed with UA and air temperature. However, further studies covering longer time periods are required to confirm the results and determine country-specific weather-related health hazard and vulnerable groups as foundation for tailored public health interventions. REFERENCES [1] S.L. James, et al., Lancet. 392, 1789-1858 (2018). https://doi.org/10.1016/S0140- 6736(18)32279-7 [2] M. Roffi, et al., Eur. Heart J. 37 (2016) 267–315. https://doi.org/10.1093/eurheartj/ehv320 ESC. [3] S. Danet, et al., Circulation 100(1):E1-7. (1999). https://doi.org/10.1161/01.CIR.100.1.e1. [4] M. Morabito, et al., Int. J. Cardiol. 105, 288-293 (2005). [5] S. Goerre, et al., Impact of weather and climate on the incidence of acute coronary syndromes, Int. J. Cardiol. (2007). https://doi.org/10.1016/j.ijcard.2006.06.015. [6] M.J. Claeys, et al., Lancet 386, 369-375 (2015). [8] I. Shiue, D.R. Perkins, N. Bearman, Environ. Sci. Pollut. Res. 23, 298-306 (2016). [9] W.B. Goggins, E.Y.Y. Chan, Int. J. Cardiol. 228, 537-542 (2017). [10] L. Bai, et al., Increased coronary heart disease and stroke hospitalisations from ambient temperatures in Ontario, Heart. (2018). https://doi.org/10.1136/heartjnl-2017-311821. [11] Y. Tian, et al., PLoS Med. 16, e1002738 (2019). https://doi.org/10.1371/journal.pmed.1002738. [12] M.J. Claeys, S. Rajagopalan, T.S. Nawrot, R.D. Brook, Climate and environmental triggers of acute myocardial infarction, Eur. Heart J. (2017). https://doi.org/10.1093/eurheartj/ehw151. [13] W.L. Kenney, D.H. Craighead, L.M. Alexander, Heat waves aging and human cardiovascular health, Med. Sci. Sports Exerc. (2014). https://doi.org/10.1249/MSS.0000000000000325. [14] L. Sfîcă, et al., Synoptic conditions generating heatwaves and warm spells in Romania, Atmosphere (Basel) 8(3), 50 (2017). https://doi.org/10.3390/atmos8030050. [15] M.V. Birsan, D.M. Micu, A.I. Nita, E. Mateescu, R. Szép, Á. Keresztesi, Spatio-temporal changes in annual temperature extremes over Romania (1961-2013), Rom. J. Phys. 64, 816 (2019). [16] A. Busuioc, et al., Changes in the large-scale thermodynamic instability and connection with rain shower frequency over Romania: verification of the Clausius-Clapeyron scaling, Int. J. Climatol. 36, 2015-2034 (2016). https://doi.org/10.1002/joc.4477.
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