School of Public Health, Khoy University of Medical Sciences, Khoy, Iran.
Environmental Health Engineering Research Center, Kerman University of Medical Sciences, Kerman, Iran; Monash Centre for Occupational & Environmental Health, School of Public Health and Preventive Medicine, Monash University, Melbourne, Australia.
J Therm Biol. 2020 Dec;94:102745. doi: 10.1016/j.jtherbio.2020.102745. Epub 2020 Oct 4.
Few studies have investigated the different extreme temperature effects (heat-cold) of one geographical location at the same time in Iran. This study was conducted to assess the impact of heat and cold waves on mortality in Urmia city, which has a cold and mountainous climate. Distributed Lag Non-linear Models combined with a quasi-Poisson regression were used to assess the impact of heat (HW) and cold waves (CW) on mortality in subgroups, controlled for potential confounders such as long-term trend of daily mortality, day of week effect, holidays, mean temperature, humidity, wind speed and air pollutants. The heat/cold effect was divided into two general categories A-main effect (the effect caused by temperature), B-added effect (the effect caused by persistence of extreme temperature). Results show that there was no relation between HW and respiratory and cardiovascular death, but in main effects, HW significantly increased, the risk of Non-Accidental Death (NAD) in lag 0 (Cumulative Excess Risk (CER) = 31(CI; 4-65)). Also in added effects, HW had a significant effect on NAD (CER = 31(CI; 5, 51), CER = 26(CI; 6, 48)). There was no relation between CW and respiratory death and cardiovascular death, but in added effects, CW significantly decreased, the risk of non-accidental death in initial lags (CER = -19 (CI; -35, -2)). It seems that high temperatures and heat waves increase the risk of non-accidental mortality in northwest of Iran.
鲜有研究同时在伊朗同一地理位置调查不同极端温度(热-冷)的影响。本研究旨在评估热浪和寒潮对乌尔米亚市死亡率的影响,该市气候寒冷多山。分布滞后非线性模型与拟泊松回归相结合,用于评估热(HW)和寒潮(CW)对死亡率的影响,在控制长期趋势、工作日效应、节假日、平均温度、湿度、风速和空气污染物等潜在混杂因素的情况下,对亚组进行评估。将热/冷效应分为两类:A-主要效应(由温度引起的效应)和 B-附加效应(由极端温度持续引起的效应)。结果表明,HW 与呼吸和心血管死亡之间没有关系,但在主要效应中,HW 显著增加了非意外死亡(NAD)的风险,在滞后 0 时(累积超额风险(CER)= 31(CI;4-65))。在附加效应中,HW 对 NAD 也有显著影响(CER = 31(CI;5,51),CER = 26(CI;6,48))。CW 与呼吸死亡和心血管死亡之间没有关系,但在附加效应中,CW 显著降低了初始滞后时非意外死亡的风险(CER = -19(CI;-35,-2))。在伊朗西北部,高温和热浪似乎增加了非意外死亡率的风险。