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Evolution of the minimum mortality temperature (1983-2018): Is Spain adapting to heat?

机译:最低死亡率温度的演变(1983-2018):西班牙适应热吗?

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摘要

The objective of this study was to analyze at the level of Spain's 52 provinces province level the temporal evolution of minimum mortality temperatures (MMT) from 1983 to 2018, in order to determine whether the increase in MMT would be sufficient to compensate for the increase in environmental temperatures in Spain for the period. It also aimed to analyze whether the rate of evolution of MMT would be sufficient, were it to remain constant, to compensate for the predicted increase in temperatures in an unfavorable (RCP 8.5) emissions scenario for the time horizon 2051-2100. The independent variable was made up of maximum daily temperature data (Tmax) for the summer months in the reference observatories of each province for the 1983-2018 period. The dependent variable was daily mortality rate due to natural causes (1CD 10: A00-R99). For each year and province, MMT was determined using a quadratic or cubic fit (p < 0.05). Based on the annual MMT values, a linear fit was carried out that allowed for determining the time evolution of MMT. These values were compared with the evolution of Tmax registered in each observatory during the 1983-2018 analyzed period and with the predicted values of Tmax obtained for an RCP8.5 scenario for the period 2051-2100. The rate of global variance in Tmax in the summer months in Spain during the 1983-2018 period was 0.41 °C/ decade, while MMT across the whole country increased at a rate of 0.64 °C/decade. Variations in the provinces were heterogeneous. For the 2051-2100 time horizon, there was predicted increase in Tmax values of 0.66 °C/de-cade, with marked geographical differences. Although at the global level it is possible to speak of adaptation, the heterogeneities among the provinces suggest that the local level measures are needed in order to facilitate adaptation in those areas where it is not occurring.
机译:本研究的目的是分析西班牙52个省份省级水平,从1983年到2018年的最低死亡率温度(MMT)的时间演变,以确定MMT的增加是否足以弥补增加的增加西班牙环境温度为期。它还旨在分析MMT的演化速率是否足够,是为了保持恒定,以补偿预测的温度的温度增加(RCP 8.5)排放场景,为时间范围2051-2100。独立变量是在1983 - 2018年期间每个省份参考观察区的夏季最大的日常温度数据(TMAX)。由于天然原因(1CD 10:A00-R99),依赖变量是每日死亡率。对于每年和省,MMT使用二次或立方拟合测定(P <0.05)。基于年度MMT值,进行线性配合,允许确定MMT的时间演变。将这些值与在1983-2018分析期间在每个天文学中登记的Tmax的演变进行了比较,并且在2051-2100期间获得RCP8.5场景的TMAX的预测值。 1983 - 2018年期间西班牙夏季全球差异在夏季的速度为0.41°C /十年,而整个国家的MMT以0.64°C /十年的速度增加。省份的变化是异质的。对于2051-2100的时间范围,预测TMAX值的增加0.66°C / de-Cade,具有标记的地理差异。虽然在全球层面,有可能谈论适应,但省份之间的异质性表明,需要局部级别措施,以便促进适应不会发生的领域。

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