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High temporal variability not trend dominates Mediterranean precipitation

  • Sergio M. Vicente-Serrano*
  • , Yves Tramblay
  • , Fergus Reig
  • , José C. González-Hidalgo
  • , Santiago Beguería
  • , Michele Brunetti
  • , Ksenija Cindrić Kalin
  • , Leonardo Patalen
  • , Aleksandra Kržič
  • , Piero Lionello
  • , Miguel M. Lima
  • , Ricardo M. Trigo
  • , Ahmed M. El-Kenawy
  • , Ali Eddenjal
  • , Murat Türkes
  • , Aristeidis Koutroulis
  • , Veronica Manara
  • , Maurizio Maugeri
  • , Wafae Badi
  • , Shifa Mathbout
  • Renato Bertalanič, Lilia Bocheva, Ismail Dabanli, Alexandru Dumitrescu, Brigitte Dubuisson, Salah Sahabi-Abed, Fayez Abdulla, Abbas Fayad, Sabina Hodzic, Mirjana Ivanov, Ivan Radevski, Dhais Peña-Angulo, Jorge Lorenzo-Lacruz, Fernando Domínguez-Castro, Luis Gimeno-Sotelo, Ricardo García-Herrera, Magí Franquesa, Amar Halifa-Marín, Maria Adell-Michavila, Ivan Noguera, David Barriopedro, Jose M. Garrido-Perez, Cesar Azorin-Molina, Miguel Andres-Martin, Luis Gimeno, Raquel Nieto, Maria Carmen Llasat, Yannis Markonis, Rabeb Selmi, Soumaya Ben Rached, Slavica Radovanović, Jean Michel Soubeyroux, Aurélien Ribes, Mohamed Elmehdi Saidi, Siham Bataineh, El Mahdi El Khalki, Sayed Robaa, Amina Boucetta, Karam Alsafadi, Nikos Mamassis, Safwan Mohammed, Beatriz Fernández-Duque, Sorin Cheval, Sara Moutia, Aleksandra Stevkov, Silvana Stevkova, M. Yolanda Luna, Vera Potopová
*Bu çalışma için yazışmadan sorumlu yazar
  • Consejo Superior de Investigaciones Científicas
  • University of Zaragoza
  • Univ. de Montpellier IRD
  • Instituto Universitario Ciencias Ambientales (IUCA)
  • Consejo Superior de Investigaciones Científicas
  • National Research Council of Italy
  • Meteorological and Hydrological Service
  • Republic Hydrometeorological Institute of Serbia
  • University of Salento
  • University of Lisbon
  • Mansoura University
  • Libyan National Meteorological Centre
  • Bogazici University
  • Technical University of Crete
  • University of Milan
  • Direction Générale de la Météorologie
  • European University Cyprus
  • University of Barcelona
  • Environmental Agency of the Republic
  • Bulgarian Academy of Sciences
  • Meteo Romania (National Meteorological Administration)
  • Météo France
  • Office National de la Météorologie
  • Jordan University of Science and Technology
  • University of Saskatchewan
  • Bosnia and Herzegovina Federal Hydrometeorological Institute
  • Institute of Hydrometeorology and Seismology of Montenegro
  • SS Cyril and Methodius University in Skopje
  • Universidad de La Rioja
  • University of Vigo
  • Complutense University
  • IGEO (UCM-CSIC)
  • Centre for Ecology and Hydrology
  • Moncada
  • Galicia Supercomputing Center (CESGA)
  • Czech University of Life Sciences Prague
  • National Institute of Meteorology
  • Université de Toulouse
  • Cadi Ayyad University
  • Mohammed VI Polytechnic University
  • Cairo University
  • Xiamen University
  • National Technical University of Athens
  • University of Debrecen
  • Ecole Hassania des Travaux Publics
  • Hydrometeorological Service of Republic of North Macedonia
  • Agencia Estatal de Meteorología (AEMET)
  • Czech Academy of Sciences

Araştırma sonucu: Dergiye katkıMakalebilirkişi

66 Atıf (Scopus)

Özet

State-of-the-art climate models project a substantial decline in precipitation for the Mediterranean region in the future1. Supporting this notion, several studies based on observed precipitation data spanning recent decades have suggested a decrease in Mediterranean precipitation2, 3–4, with some attributing a large fraction of this change to anthropogenic influences3,5. Conversely, certain researchers have underlined that Mediterranean precipitation exhibits considerable spatiotemporal variability driven by atmospheric circulation patterns6,7 maintaining stationarity over the long term8,9. These conflicting perspectives underscore the need for a comprehensive assessment of precipitation changes in this region, given the profound social, economic and environmental implications. Here we show that Mediterranean precipitation has largely remained stationary from 1871 to 2020, albeit with significant multi-decadal and interannual variability. This conclusion is based on the most comprehensive dataset available for the region, encompassing over 23,000 stations across 27 countries. While trends can be identified for some periods and subregions, our findings attribute these trends primarily to atmospheric dynamics, which would be mostly linked to internal variability. Furthermore, our assessment reconciles the observed precipitation trends with Coupled Model Intercomparison Project Phase 6 model simulations, neither of which indicate a prevailing past precipitation trend in the region. The implications of our results extend to environmental, agricultural and water resources planning in one of the world’s prominent climate change hotspots10.

Orijinal dilİngilizce
Sayfa (başlangıç-bitiş)658-666
Sayfa sayısı9
DergiNature
Hacim639
Basın numarası8055
DOI'lar
Yayın durumuYayınlandı - 20 Mar 2025

Bibliyografik not

Publisher Copyright:
© The Author(s) 2025.

BM SKH

Bu sonuç, aşağıdaki Sürdürülebilir Kalkınma Hedefine/Hedeflerine katkıda bulunur

  1. SKH 6 - Temiz Su ve Sanitasyon
    SKH 6 Temiz Su ve Sanitasyon
  2. SKH 8 - İnsana Yakışır İş ve Ekonomik Büyüme
    SKH 8 İnsana Yakışır İş ve Ekonomik Büyüme
  3. SKH 13 - İklim Eylemi
    SKH 13 İklim Eylemi

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