Evidence map›Paper›PMID 41690987›Full record

ArticleScientific reports2026

Water vapor transport observed at a coastal Mediterranean site during the summer of 2021 and compared with ERA5.

Fabio Madonna, Ilaria Gandolfi, Yassmin Hesham Essa, Benedetto De Rosa, Simone Gagliardi, Domenico Madonna, Fabrizio Marra, Maria Assunta Menniti, Donato Summa, Emanuele Tramutola and 3 more

Abstract read
In one paragraph

Article in Scientific reports, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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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

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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

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0 citing papers in PubMed.

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4 · The record

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5 · Who and what money

Authors and funding

13 authors.

Fabio MadonnaDepartment of Physics, University of Salerno, Fisciano, Italy. fmadonna@unisa.it.
Ilaria GandolfiIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Yassmin Hesham EssaInstitute for Atmospheric and Environmental Sciences, Goethe University Frankfurt (GUF-IAU), Frankfurt am Main, Germany.
Benedetto De RosaIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Simone GagliardiIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Domenico MadonnaIstituto Salesiano Sant'Antonio di Padova, Soverato, Italy.
Fabrizio MarraIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Maria Assunta MennitiCentro Studi e Ricerca Ambiente Marino (CESRAM), Soverato, Italy.
Donato SummaIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Emanuele TramutolaIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Faezeh Karimian SaracksDepartment of Physics, University of Salerno, Fisciano, Italy.
Filomena RomanoIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.
Marco RosoldiIstituto di Metodologie per l'Analisi Ambientale (CNR-IMAA), Consiglio Nazionale delle Ricerche, Tito Scalo, Italy.

Funding

ACTRIS-2 654109
6 · The paper itself

Abstract

Extreme events in the Mediterranean have increased in frequency and intensity over the past decade, and this trend is expected to continue. Characterizing these events using reliable observational datasets is essential for understanding the processes driving their development. This study uses observational data collected during the Mediterranean Experiment for Sea Salt And Dust Ice Nuclei (MESSA-DIN) from July to September 2021, at the coastal site of Soverato, on the Ionian coast of Southern Italy, to characterize the intense water vapor transport over the Mediterranean basin during the severe summer of 2021. Furthermore, we compare the observations to the atmospheric reanalysis ERA5 and describe the synoptic environment over the study period. The results highlight the role of water vapor transport in weather systems and local atmospheric processes, underscoring the importance of high-resolution water vapor atmospheric profiling to enhance the accuracy of extreme rainfall and flood forecasting. While ERA5 performed well in capturing synoptic-scale patterns, it exhibited a dry bias of up to 3 g kg-1 compared to microwave radiometer retrievals in the 450–650 hPa vertical layer. This bias likely reflects limitations in the reanalysis representation of tropospheric moisture transport, particularly from dominant North African inflows, in addition to contributions from remote Atlantic pathways and local sources.

Indexed as

Extreme eventsMediterraneanObservationsRenalaysisWater vapor

Identifiers

PMID41690987
PMCPMC12996470

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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.