Volume 36 Issue 11
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LI He Ping, MA Yu Xia, QIN Peng Peng, WANG Wan Ci, LIU Zong Rui, ZHAO Yu Han, YANG Li Jie. Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China[J]. Biomedical and Environmental Sciences, 2023, 36(11): 1095-1099. doi: 10.3967/bes2023.140
Citation: LI He Ping, MA Yu Xia, QIN Peng Peng, WANG Wan Ci, LIU Zong Rui, ZHAO Yu Han, YANG Li Jie. Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China[J]. Biomedical and Environmental Sciences, 2023, 36(11): 1095-1099. doi: 10.3967/bes2023.140

Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China

doi: 10.3967/bes2023.140
Funds:  This study was supported by the National Natural Science Foundation of China [No. 41975141].
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  • Author Bio:

    LI He Ping, male, born in 1998, Master, majoring in the health effects of ambient temperature

    MA Yu Xia, female, born in 1974, Professor, majoring in weather and climate effects on health

  • &These authors contributed equally to this work.
  • Received Date: 2023-06-25
  • Accepted Date: 2023-08-22
  • &These authors contributed equally to this work.
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  • [1] Ma P, Zhang Y, Wang XZ, et al. Effect of diurnal temperature change on cardiovascular risks differed under opposite temperature trends. Environ Sci Pollut Res, 2021; 28, 39882−91. doi:  10.1007/s11356-021-13583-5
    [2] Lee W, Bell ML, Gasparrini A, et al. Mortality burden of diurnal temperature range and its temporal changes: A multi-country study. Environ Int, 2018; 110, 123−30. doi:  10.1016/j.envint.2017.10.018
    [3] Xiao Y, Meng CZ, Huang SL, et al. Short-term effect of temperature change on non-accidental mortality in Shenzhen, China. Int J Environ Res Public Health, 2021; 18, 8760. doi:  10.3390/ijerph18168760
    [4] Gasparrini A. Distributed lag linear and non-linear models in R: the package dlnm. J Stat Softw, 2011; 43, 1−20.
    [5] Yang J, Liu HZ, Ou CQ, et al. Global climate change: impact of diurnal temperature range on mortality in Guangzhou, China. Environ Pollut, 2013; 175, 131−6. doi:  10.1016/j.envpol.2012.12.021
    [6] Zheng H, Wang YQ, Cang YQ. Investigation on the four seasons of Harbin and division of season index. Heilongjiang Meteorol, 2001; 32−3. (In Chinese
    [7] Phosri A, Sihabut T, Jaikanlaya C. Short-term effects of diurnal temperature range on hospital admission in Bangkok, Thailand. Sci Total Environ, 2020; 717, 137202. doi:  10.1016/j.scitotenv.2020.137202
    [8] Zhan ZY, Zhao Y, Pang SJ, et al. Temperature change between neighboring days and mortality in United States: A nationwide study. Sci Total Environ, 2017; 584−585, 1152−61.
    [9] Zanobetti A, O'Neill MS, Gronlund CJ, et al. Summer temperature variability and long-term survival among elderly people with chronic disease. Proc Natl Acad Sci USA, 2012; 109, 6608−13. doi:  10.1073/pnas.1113070109
    [10] Lian H, Ruan YP, Liang RJ, et al. Short-term effect of ambient temperature and the risk of stroke: a systematic review and meta-analysis. Int J Environ Res Public Health, 2015; 12, 9068−88. doi:  10.3390/ijerph120809068
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Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China

doi: 10.3967/bes2023.140
Funds:  This study was supported by the National Natural Science Foundation of China [No. 41975141].
  • Author Bio:

  • &These authors contributed equally to this work.
&These authors contributed equally to this work.
LI He Ping, MA Yu Xia, QIN Peng Peng, WANG Wan Ci, LIU Zong Rui, ZHAO Yu Han, YANG Li Jie. Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China[J]. Biomedical and Environmental Sciences, 2023, 36(11): 1095-1099. doi: 10.3967/bes2023.140
Citation: LI He Ping, MA Yu Xia, QIN Peng Peng, WANG Wan Ci, LIU Zong Rui, ZHAO Yu Han, YANG Li Jie. Association between Temperature Changes and Cardiovascular Mortality Risk in A High-latitude City in Northeast China[J]. Biomedical and Environmental Sciences, 2023, 36(11): 1095-1099. doi: 10.3967/bes2023.140
  • In recent decades, regional and global climate change has increased the frequency of extreme weather events (e.g., hurricanes, cold spells, and heat waves). The diurnal temperature range (DTR) and temperature change between neighboring days (TCN), which are indicators of short-term temperature shifts, have been found to be significantly associated with cardiovascular morbidity or mortality[1]. A worldwide study on the effects of temporal changes on mortality burden in 10 countries found that a negative impact of high DTR on mortality in a short time and a 10 °C increment in DTR increased the risk of overall mortality by 3.10%[2]. Another study on the link between TCN and multiple disease mortalities in the United States also revealed that the cumulative RR (relative risk) of extremely positive TCN significantly affected cardiovascular mortality with an RR of 1.52 (95% CI: 1.40–1.65)[2]. Given that most relevant studies were confined to large central and eastern cities in China[1,3], the generalizability of the results remains uncertain. Therefore, in the current study, we used the distributed lag non-linear model (DLNM) to explore the specific relationships between DTR/TCN and cardiovascular mortality risk and evaluate the health effects of different patterns in Harbin, a high-latitude city in China. The relevant findings of our study may provide evidence for medical meteorology research at high latitudes in China and provide a theoretical basis for local services.

    Daily cardiovascular mortality in Harbin during 3 years (from January 1, 2014 to December 21, 2016) was obtained from the Harbin Center for Disease Control and Prevention. The causes of death were coded according to the 10th edition of the International Classification of Diseases (ICD-10), containing 10 specific cardiovascular diseases, from I00 to I99. The main daily meteorological elements were obtained from the Harbin Meteorological Bureau, and the main daily air pollutants were collected from the Harbin Environmental Protection Bureau.

    Daily death caused by cardiovascular disease is a low-probability event, which is considered to satisfy the Poisson distribution. In the present study, the natural cubic spline function of the DLNM was used to evaluate the effects of DTR and TCN on cardiovascular mortality across different sex groups and periods with lag days[4]. The specific model formulas are

    $$ {Y}_{t}\sim Poisson\left({\mu }_{t}\right) $$ (1)
    $$ \begin{aligned} \mathit{log}({\mu }_{t})=& \alpha +\beta DT{R}_{t,l}+{\sum }_{i}ns\left(weathe{r}_{i}/pollutan{t}_{i},d{f}_{i}\right)\\ & +ns(Time,df=7\times 3)+Do{w}_{t}+Holida{y}_{t} \end{aligned} $$ (2)
    $$ \begin{aligned} \mathit{log}({\mu }_{t})= & \alpha +\beta TC{N}_{t,l}+{\sum }_{i}ns\left(weathe{r}_{i}/pollutan{t}_{i},d{f}_{i}\right)\\& +ns(Time,df=7\times 3)+Do{w}_{t}+Holida{y}_{t} \end{aligned} $$ (3)

    where $ t $ denotes the observational day (t = 1, 2, 3, …, 1096), $ {\mu }_{t} $ is the estimated single cardiovascular mortality on day $ t $, $ \alpha $ represents the intercept, $ DT{R}_{t,l} $ and $ TC{N}_{t,l} $ are the cross matrix function for DTR and TCN, respectively, and $ l $ is the lag parameter of DLNM. $ \beta $ signifies the vector of the coefficients for $ DT{R}_{t,l} $ and $ TC{N}_{t,l} $,$ ns $ is the cubic natural splines of nonlinear parameters, $ weathe{r}_{i} $ denotes the meteorological factors including air pressure, relative humidity and mean temperature, $ pollutan{t}_{i} $ denotes air pollutant factors of SO2 and NO2, $ d{f}_{i} $ is degree of freedom, $ Time $ represents the time variable of the Gregorian calendar, $ Do{w}_{t} $ is an indicator variable and represents the day of the week, and $ Holida{y}_{t} $ is an indicator variable for which 1 denotes a legal holiday, and 0 denotes other days.

    In light of extensive previous research, the degrees of freedom (df) for all meteorological and pollutant parameters were set as 3, and the df in the cross matrix of DTR and TCN was selected as 4 in this study[5]. Environmental factors were selected based on the Spearman’s correlation with cardiovascular mortality (Supplementary Table S1, available in www.besjournal.com). To eliminate long-term trends and seasonality, the df of time was seven per year with a maximum lag time of 10 days. For explanation and quantification, we took the 5th percentile as the lowest extreme value and the 95th percentile as the highest extreme values for DTR and TCN. In addition, the records were divided into diverse subgroups with respect to sex (male and female), and according to monthly average temperatures in Harbin[6], we stratified the entire study into three periods: full year, hot season (June to August), and cold season (November to March of the following year). A two-sample Z-test was conducted to examine whether the differences between the subgroups were statistically significant (see Supplementary Table S2, available in www.besjournal.com). All the mathematical analyses were performed using R language (version 4.2.2, URL: https://cran.r-project.org/), and DLNM was based on the “dlnm” package (version 2.4.7). The two-sided test was applied to all the statistical results, and P < 0.05 was deemed to be statistically significant.

    Variables PM2.5 PM10 SO2 CO NO2 O3_8h Wind Rain Temp Pres Suntime Rh Mortality
    PM2.5 1.000
    PM10 0.945** 1.000
    SO2 0.611** 0.612** 1.000
    CO 0.778** 0.726** 0.534** 1.000
    NO2 0.818** 0.800** 0.743** 0.770** 1.000
    O3_8h −0.297** −0.248** −0.513** −0.293** −0.370** 1.000
    Wind −0.153** −0.072* −0.196** −0.248** −0.372** 0.121** 1.000
    Rain −0.163** −0.181** −0.210** −0.157** −0.236** 0.104** 0.115** 1.000
    Temp −0.473** −0.442** −0.758** −0.519** −0.590** 0.734** 0.108** 0.217** 1.000
    Pres 0.427** 0.383** 0.597** 0.483** 0.577** −0.540** −0.265** −0.321** −0.762** 1.000
    Suntime −0.259** −0.235** −0.189** −0.145** −0.123** 0.360** −0.110** −0.261** 0.205** 0.017 1.000
    Rh 0.009 −0.102** 0.005 0.164** 0.007 −0.199** −0.343** 0.317** −0.013 −0.070* −0.442** 1.000
    Mortality 0.097** 0.121** 0.216** 0.082** 0.136** −0.106** 0.051 −0.096** −0.229** 0.169** −0.020 −0.164** 1.000
      Note. **P < 0.01.

    Table S1.  Spearman correlation analysis of cardiovascular mortality and environmental elements

    Variables High DTR Low DTR High TCN Low TCN
    Male vs. Female 0.103 0.154 0.974 0.042
    Hot vs. Full year 0.139 0.906 0.119 0.573
    Cold vs. Full year 0.015 0.126 0.134 0.021
    Cold vs. Hot 0.043 0.013 0.031 0.038

    Table S2.  Two-sample Z-test between groups at different levels of DTR and TCN, values indicate P, with P < 0.05 representing significant differences

    The daily cardiovascular mortality was 71 per day over the full year; 43.11% of cases were in the cold season (74 per day), and 23.02% of cases were in the hot season (65 per day) (Supplementary Table S3, available in www.besjournal.com). Cardiovascular mortality was higher among males than females, and in winter than in summer. The average TCN value recorded in different stages were all approximately close to 0 °C, and the mean DTR value in the cold season (11.20 °C) was slightly higher than that in the hot season (9.20 °C). The average daily concentrations of NO2 (62.80 μg/m3) and SO2 (79.80 μg/m3) in the cold season were much higher than those in the hot season when NO2 were 34.70 μg/m3 and SO2 were 8.10 μg/m3. The time-series analysis of calendars for the daily average DTR and TCN from 2014 to 2016 (S1) showed that the high values of DTR were essentially distributed between January and May, and the low values were essentially distributed between June and September. In other periods, monthly variations in the DTR values fluctuated within a limited range. The value of TCN varied less from June to September and remained around 0 °C, and in other months, the high TCN values were predominant, while the low levels were less frequent. The differences in the daily and weekly changes in the indicators were not significant. The temporal distribution characteristics of DTR and TCN may be related to the local climatic characteristics and geographical background.

    Variables Mean (SD) Minimun Percentile Maximun
    5th 25th 50th 75th 95th
    Full year
    DTR (°C) 10.6 (3.7) 1.5 4.8 8.0 10.4 13.1 17.3 21.5
    TCN (°C) 0.0 (3.2) –15.2 –5.3 –1.6 0.1 1.8 5.0 11.6
    Mean Temperature (°C) 5.3 (15.4) –26.1 –19.4 –9.4 7.5 19.6 25.3 29.0
    Relative Humidity (%) 65.4 (15.0) 15.0 36.0 57.0 67.0 76.0 88.0 97.0
    Air Pressure (hPa) 1000.3 (9.5) 973.2 986.2 993.0 999.6 1007.6 1016.2 1025.2
    NO2 (μg/m3) 48.5 (20.7) 15.0 23.0 34.0 43.0 59.0 88.2 145.0
    SO2 (μg/m3) 41.1 (45.2) 3.0 6.0 9.0 21.0 61.0 139.3 234.0
    CVD mortality 71 (13) 41 52 63 70 79 93 133
    Male 41 (8) 15 29 36 40 46 56 75
    Female 30 (7) 14 20 25 29 34 42 62
    Cold season
    DTR (°C) 11.2 (3.8) 2.8 5.0 8.6 10.6 13.7 17.8 21.5
    TCN (°C) 0.1 (3.8) –12.0 –7.0 –2.0 0.2 2.3 6.0 11.6
    Mean Temperature (°C) –10.3 (8.5) –26.1 –22.3 –16.7 –11.9 –4.9 6.1 13.5
    Relative Humidity (%) 66.0 (12.7) 19.0 43.0 60.0 67.0 74.0 87.0 97.0
    Air Pressure (hPa) 1007.6 (7.1) 989.2 995.2 1002.9 1008.0 1012.7 1019.2 1025.2
    NO2 (μg/m3) 62.8 (21.0) 17.0 34.0 48.0 60.0 73.3 102.0 145.0
    SO2 (μg/m3) 79.8 (46.3) 18.0 30.0 45.0 67.0 102.0 182.5 234.0
    CVD mortality 74 (13) 41 55 65 72 81 95 133
    Male 42 (8) 19 30 37 42 47 58 71
    Female 31 (7) 14 21 26 30 35 45 62
    Hot season
    DTR (°C) 9.2 (2.7) 3.7 4.8 7.1 9.3 11.1 13.9 16.9
    TCN (°C) 0.0 (1.8) –5.9 –3.2 –1.0 0.1 1.1 2.6 5.9
    Mean Temperature (°C) 22.7 (2.8) 14.2 18.4 20.6 22.6 24.7 27.1 29.0
    Relative Humidity (%) 72.4 (10.6) 43.0 52.7 66.0 73.0 80.8 89.0 96.0
    Air Pressure (hPa) 991.7 (4.3) 974.6 984.3 989.0 991.8 994.8 998.4 1001.8
    NO2 (μg/m3) 34.7(9.5) 17.0 21.0 28.0 33.5 40.0 52.0 69.0
    SO2 (μg/m3) 8.1 (3.2) 3.0 4.0 6.0 8.0 10.0 13.0 29.0
    CVD mortality 65 (11) 41 49 57 64 72 84 132
    Male 38 (8) 15 28 33 37 43 51 75
    Female 27 (6) 15 19 23 27 31 37 57

    Table S3.  Basic statistics of meteorological factors, concentrations of air pollutants and cardiovascular mortality in Harbin, China, from 2014 to 2016

    As shown in Figure 1, the high frequency of DTR was mostly distributed in the range of 6–14 °C, while that of TCN was more frequently in the range of −2–2 °C. The 10-day cumulative risk curve of both DTR and TCN demonstrated a consistent upward trend as temperature changes increased, with a peak value of 1.17 (95% CI: 1.08–1.26) at 16 °C for DTR and 1.86 (95% CI: 1.18–2.92) at 11.50 °C for TCN. High DTR and TCN values represent more dramatic short-term temperature changes that could have a more significant impact on human health. Thus, high DTR and TCN levels contributed to a greater effect on cardiovascular mortality than low levels.

    Figure 1.  Cumulative RRs over 10 days on the cardiovascular mortality with the frequency distribution histograms of DTR (diurnal temperature range) and TCN (temperature change between neighboring days) in Harbin, China, from 2014 to 2016, with the reference values of 6 °C and 0 °C, respectively.

    Sex differences at high and low DTR and TCN are shown in Figure 2. Generally, the average RRs of the DTR and TCN with high levels of sex were greater than those with low levels on each lag day. The RRs of females and males at high levels (P95) of DTR and TCN initially increased, and then decreased with lag days. The RRs of DTR in males and females increased to a maximum on the second day (lag 2), with values of 1.02 (95% CI: 0.99–1.04), 1.02 (95% CI: −1.00–1.05), and 1.03 (95% CI: 1.00–1.05), respectively. The largest RR for TCN in males was 1.03 (95% CI: 1.01–1.05) on the fourth day (lag 4). In addition, the RR of TCN in females had a maximum value of 1.050 (95% CI: −1.00–1.10) on the same day; other RR values were not significant at low levels. The cumulative effects (Supplementary Table S4, available in www.besjournal.com) showed that the RR values of high DTR and TCN were greater in females than in males, indicating that the females were more vulnerable to both DTR and TCN than males. This phenomenon might be linked to individual physiological structures, immune functions, and hormone levels, such as the specific physical mechanisms in males, which prompted them to be more resilient to environmental temperatures than females, and the absence or deficiency of this mechanism caused females to be more susceptible to temperature changes[3].

    Figure 2.  Effects of extreme high (P95) and low (P5) DTR (diurnal temperature range) and TCN (temperature change between neighboring days) on the gender-specific cardiovascular mortality in Harbin, China, from 2014 to 2016.

    Figure 3 shows the effects of low (P5) and high (P95) DTR and TCN levels on cardiovascular mortality under seasonal stratification. The RRs of low DTR and TCN showed no apparent effects on cardiovascular mortality in any season. In the entire year, the RRs corresponding to a high DTR and TCN revealed a consistent pattern of variation and reached a maximum on the second day (lag 2). In the cold season, the effects of temperature changes were more hysteretic; the RR values for all groups increased gradually with lag time, and the maximum RRs occurred at lag 10 for high DTR and at lag 7 for high TCN. In the hot season, the effects of temperature changes were more transient; the largest RRs occurred on the same day and thereafter decreased with lag days. The RR values of high-DTR were higher in the hot season, whereas those of high-TCN were much greater in the cold season (Supplementary Table S4). Winter heating in northern cities and vulnerability to thermal adaptation might lead to an underestimation of the effect of cold temperatures on cardiovascular mortality. The estimated effects of TCN on cardiovascular mortality were greater than those of DTR. In general, people, especially office workers, stay indoors during the time of day when the temperature drastically changes, which may result in an underestimated pathogenic effect of DTR[7]. The heat island effect caused by the urban and suburban temperature differences may enhance the health effects of DTR and TCN. Furthermore, a dramatic inter-day change in temperature could increase the adverse effects of average temperatures on mortality, and this additional impact carried by average temperature would, in turn, amplify the effect of TCN on mortality[8].

    Figure 3.  The effects of extreme low (P5) and high (P95) DTR (diurnal temperature range) and TCN (temperature change between neighboring days) on cardiovascular mortality under seasonal stratifications.

    The underlying physiological mechanisms of DTR/TCN on daily cardiovascular mortality remain unclear. A reasonable explanation is that sudden changes in ambient temperature surpass the limits of the body’s initial tolerance; automatic temperature regulation systems cannot adapt well to such a variation in the environment in the short term, leading to an increase in blood pressure, immune reaction, and inflammatory response while affecting many other physical functions[9]. Other potential pathogenic factors, including the increase of superficial blood circulation, hypotension, salt depletion, and dehydration, would be an additional burden to the cardio-cerebral-vascular system, which might ultimately cause the occurrence of stroke or myocardial infarction[10].

    The current study has several limitations. First, owing to the large regional differences in population vulnerability, climatic conditions, and socioeconomic status, the findings of this study should be generalized to other regions of China or the world. Second, the collected daily cardiovascular mortality data were confined to selected hospitals and did not include more patients; therefore, the impacts of temperature changes on mortality were biased and probably underestimated. Additionally, individual-level factors, such as occupation, education level, and economic conditions, were not considered; the use of air conditioning reduced the temperature differential effect, while outdoor workers could bear greater risk.

    The authors declare no conflicts of interest. This article does not contain any studies with human participants or animals performed by any of the authors.

    SubgroupsDTRTCN
    High levelLow levelHigh levelLow level
    Full year1.164 (1.079, 1.256)a0.942 (0.849, 1.044)1.211 (1.073, 1.366)a0.745 (0.639, 0.869)
    Hot season1.333 (1.088, 1.633)a0.945 (0.847, 1.055)1.030 (0.751, 1.412)0.787 (0.536, 1.157)
    Cold season1.285 (1.135, 1.454)a0.904 (0.843, 0.969)1.367 (1.067, 1.750)a0.609 (0.473, 0.785)
    Males1.136 (1.041, 1.240)a0.896 (0.795, 1.010)1.261 (1.097, 1.449)a0.793 (0.672, 0.937)
    Females1.186 (1.072, 1.312)a1.017 (0.886, 1.167)1.262 (1.074, 1.483)a0.855 (0.704, 1.037)

    Table S4.  The cumulative effects of stratified seasons and genders within lag 0–10 days

    Figure S1.  Calendars of time series analysis for daily average DTR and TCN in Harbin, China, from 2014 to 2016. aP < 0.05.

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