4.6 Article

Modelling the occurrence of heat waves in maximum and minimum temperatures over Spain and projections for the period 2031-60

期刊

GLOBAL AND PLANETARY CHANGE
卷 161, 期 -, 页码 244-260

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.gloplacha.2017.11.015

关键词

Extreme heat events; Non-homogeneous Poisson process; Bivariate models; Climate projections; Climate change

资金

  1. Ministerio de Ciencia e Innovacion (Spanish Department of Science) [CGL2009-09646]
  2. Ministerio de Medio Ambiente (Spanish Department of Environment) [ESTCENA 2009/0017]
  3. Diputacion General de Aragon [228152/3-E22]

向作者/读者索取更多资源

The occurrence of extreme heat events in maximum and minimum daily temperatures is modelled using a non homogeneous common Poisson shock process. It is applied to five Spanish locations, representative of the most common climates over the Iberian Peninsula. The model is based on an excess over threshold approach and distinguishes three types of extreme events: only in maximum temperature, only in minimum temperature and in both of them (simultaneous events). It takes into account the dependence between the occurrence of extreme events in both temperatures and its parameters are expressed as functions of time and temperature related covariates. The fitted models allow us to characterize the occurrence of extreme heat events and to compare their evolution in the different climates during the observed period. This model is also a useful tool for obtaining local projections of the occurrence rate of extreme heat events under climate change conditions, using the future downscaled temperature trajectories generated by Earth System Models. The projections for 2031-60 under scenarios RCP4.5, RCP6.0 and RCP8.5 are obtained and analysed using the trajectories from four earth system models which have successfully passed a preliminary control analysis. Different graphical tools and summary measures of the projected daily intensities are used to quantify the climate change on a local scale. A high increase in the occurrence of extreme heat events, mainly in July and August, is projected in all the locations, all types of event and in the three scenarios, although in 2051-60 the increase is higher under RCP8.5. However, relevant differences are found between the evolution in the different climates and the types of event, with a specially high increase in the simultaneous ones.

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