Hydrology and Earth System Sciences
Hydrology and Earth System Sciences
HESS
Articles | Volume 26, issue 23
Articles | Volume 26, issue 23
https://doi.org/10.5194/hess-26-6055-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-26-6055-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 26, issue 23
Research article
 | 
05 Dec 2022
Research article |  | 05 Dec 2022

Declining water resources in response to global warming and changes in atmospheric circulation patterns over southern Mediterranean France

Camille Labrousse, Wolfgang Ludwig, Sébastien Pinel, Mahrez Sadaoui, Andrea Toreti, and Guillaume Lacquement

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Arnell, N. W., van Vuuren, D. P., and Isaac, M.: The implications of climate policy for the impacts of climate change on global water resources, Global Environ. Chang., 21, 592–603, https://doi.org/10.1016/j.gloenvcha.2011.01.015, 2011. 
BD Carthage Métropole: Hydrological Data Bank Hosted at the French Ministry of the Environment and of Sustainable Development, https://geo.data.gouv.fr/fr/datasets/38d5c85219924e0f5355b551b0453ed942a03b8f, last access: 21 February 2021. 
Beranová, R. and Kyselý, J.: Links between circulation indices and precipitation in the Mediterranean in an ensemble of regional climate models, Theor. Appl. Climatol., 123, 693–701, https://doi.org/10.1007/s00704-015-1381-6, 2016. 
Bholowalia, P. and Kumar, A.: EBK-Means: A Clustering Technique based on Elbow Method and K-Means in WSN, Int. J. Comp. Appl., 105, 17–24, 2014. 
Bueh, C. and Nakamura, H.: Scandinavian pattern and its climatic impact, Q. J. Roy. Meteor. Soc., 133, 2117–2131, https://doi.org/10.1002/qj.173, 2007. 
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The interest of this study is to demonstrate that we identify two zones in our study area whose hydroclimatic behaviours are uneven. By investigating relationships between the hydroclimatic conditions in both clusters for past observations with the overall atmospheric functioning, we show that the inequalities are mainly driven by a different control of the atmospheric teleconnection patterns over the area.
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