Mega-heatwave temperatures due to combined soil desiccation and atmospheric heat accumulation View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2014-04-20

AUTHORS

Diego G. Miralles, Adriaan J. Teuling, Chiel C. van Heerwaarden, Jordi Vilà-Guerau de Arellano

ABSTRACT

Extreme heatwave events are expected to become increasingly common as a consequence of climate change. Analyses of the 2003 and 2010 mega-heatwaves in Europe suggest that atmospheric boundary-layer dynamics and feedbacks with the drying land surface lead to the build-up of heat in the atmosphere and extremely hot temperatures.

PAGES

345-349

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/ngeo2141

DOI

http://dx.doi.org/10.1038/ngeo2141

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1006668095


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