Climatology of heatwaves in South America identified through ERA5 reanalysis data

Abstract

The rise in the Earth's global average surface temperature and the increase of extreme weather events have been the focus of scientific discussion in the last decades. Extreme heat combined with other environmental extremes, like high concentrations of air pollution, may induce health problems-especially in socioeconomically vulnerable populations. Spring in South America requires particular attention due to its association with hot, dry weather and air pollution in most parts of the continent. This paper intends to better comprehend the behaviour of heatwaves during the austral winter-spring transition. We propose identifying the spatial coverage, frequency and intensity of heatwaves in homogeneous areas of maximum air temperature near the surface (T max ). We employed cluster analyses during the period between July and October for 41 years through the ERA5 reanalysis. Homogeneous T max areas in South America were defined by cluster analyses that indicated three homogeneous T max regions, as follows: a larger area of the continent including the tropical region (Area 1), eastern and southeastern South America (Area 2) and southernmost and steep areas in the Andes (Area 3). The heatwave events identified via ERA5 reanalysis were classified according to their intensity (intense, moderate and weak events). Spatial frequency and trend analyses were also performed regarding the intensity and persistence of heatwave episodes. These methods allowed the identification of the behavioural aspect of heatwaves spanning the last four decades. The Mann-Kendall statistical test (MK) was applied in order to analyse the heatwave trend with a statistical significance level of 5%. A total of 191 heatwave episodes were identified. Of this total, 47.12, 35.60 and 17.28% of episodes occurred in Areas 2, 3 and 1, respectively. The hotter area extending from northeast to southwest in central South America stood out by its largest frequencies of intense heatwave episodes. Across the continent there was a significant increase in the intensity and persistence of heatwaves over the period of 1979 through to 2019. K E Y W O R D S2-m temperature, climate change, extreme weather events, heatwaves, hot weather, South America, temperature extremes

Spatial–Temporal Analysis of a Summer Heat Wave Associated with Downslope Flows in Southern Brazil: Implications in the Atmospheric Boundary Layer

“…A less studied type of interaction concerns the coexistence of heat waves (HWs) and DWs [11,13,[25][26][27][28]. From a meteorological point of view, an HW can be defined as a sustained and unusual period of elevated air temperatures [29][30][31][32][33][34]. Although progress has been made in understanding the synoptic-scale characteristics of HWs (see, e.g., [11,28,[35][36][37][38], among many others), the role of ABL dynamics in this phenomenon remains poorly explored and documented.…”