Evidence map›Paper›PMID 41702883›Full record

ArticleNature communications2026

Human-induced climate change amplification on storm dynamics in Valencia's 2024 catastrophic flash flood.

Carlos Calvo-Sancho, Javier Díaz-Fernández, Juan Jesús González-Alemán, Amar Halifa-Marín, Mario Marcello Miglietta, Cesar Azorin-Molina, Andreas F Prein, Ana Montoro-Mendoza, Pedro Bolgiani, Ana Morata and 1 more

Abstract read
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

11 authors.

Carlos Calvo-SanchoDepartment of Applied Mathematics. Faculty of Computer Engineering, Universidad de Valladolid, Valladolid, Spain. carlos.calvo.sancho@uva.es.ORCID http://orcid.org/0000-0003-2457-9793
Javier Díaz-FernándezDepartment of Applied Mathematics. Faculty of Computer Engineering, Universidad de Valladolid, Valladolid, Spain.
Juan Jesús González-AlemánSpanish State Meteorological Agency (AEMET), Department of Science, Madrid, Spain.ORCID http://orcid.org/0000-0001-5940-7356
Amar Halifa-MarínInstituto Pirenaico de Ecología, Consejo Superior de Investigaciones Científicas (IPE-CSIC), Zaragoza, Spain.
Mario Marcello MigliettaNational Research Council of Italy, Institute of Atmospheric Sciences and Climate (CNR-ISAC), Padua, Italy.ORCID http://orcid.org/0000-0003-2898-1595
Cesar Azorin-MolinaCentro de Investigaciones sobre Desertificación, Consejo Superior de Investigaciones Científicas (CIDE, CSIC-UV-GVA), Climate, Atmosphere and Ocean Laboratory (Climatoc-Lab), Moncada, Valencia, Spain.
Andreas F PreinInstitute of Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland.
Ana Montoro-MendozaDepartment of Applied Mathematics. Faculty of Computer Engineering, Universidad de Valladolid, Valladolid, Spain.
Pedro BolgianiDepartment of Earth Physics and Astrophysics, Faculty of Physics, Complutense University of Madrid, Madrid, Spain.ORCID http://orcid.org/0000-0002-7096-5831
Ana MorataSpanish State Meteorological Agency (AEMET), Department of Science, Madrid, Spain.
María Luisa MartínDepartment of Applied Mathematics. Faculty of Computer Engineering, Universidad de Valladolid, Valladolid, Spain.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Global warming alters the hydrological cycle, increasing heavy rainfall events worldwide. In October 2024, Valencia (Spain) experienced rainfall accumulations in a few hours surpassing annual averages (771.8 mm in 16 h in the official weather station at Turís) and breaking the record for one hour rainfall accumulation in Spain (184.6 mm), resulting in 230 fatalities. Here, we present a physical-based attribution study employing a km-scale pseudo-global warming storyline approach to assess the contribution of anthropogenic climate change. We show that present-day conditions led to a 20% °C⁻¹ increase in 1-hour rainfall intensity, exceeding Clausius-Clapeyron scaling. This intensification was driven by enhanced atmospheric moisture from warmer sea surface temperatures, leading to increased convective available potential energy, stronger updrafts, and microphysical changes including elevated graupel concentrations. These results demonstrate that anthropogenic climate change could intensify the occurrence of flash-floods in the Western Mediterranean region: in this particular case, it intensified the 6-h rainfall rate by 21%, amplified the area with total rainfall above 180 mm by 55%, and increased the volume of total rain within the Jucar River catchment by 19% compared to the pre-industrial era. This study highlights the urgent need for effective adaptation strategies and improved urban planning to reduce the growing risks of hydrometeorological extremes in a rapidly warming world.

Identifiers

PMID41702883
PMCPMC12913788

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.