@article{fdi:010074506, title = {{M}ulti-decadal to centennial hydro-climate variability and linkage to solar forcing in the {W}estern {M}editerranean during the last 1000 years}, author = {{B}rahim, {Y}. {A}. and {W}assenburg, {J}. {A}. and {C}ruz, {F}. {W}. and {S}ifeddine, {A}bdelfettah and {S}cholz, {D}. and {B}ouchaou, {L}. and {D}assie, {E}. {P}. and {J}ochum, {K}. {P}. and {E}dwards, {R}. {L}. and {C}heng, {H}.}, editor = {}, language = {{ENG}}, abstract = {{H}ere we present a new composite record from two well-dated speleothem records from two caves in {N}orthern {M}orocco. {T}he high-resolution record covers the last millennium allowing to detect multi-decadal to centennial periodicities. {O}ver the industrial period, delta {O}-18 values of our speleothems are shown to be dominated by the main mode of decadal variability in the {N}orth {A}tlantic region: the {N}orth {A}tlantic {O}scillation ({NAO}). {S}tatistical analyses confirm the previously reported multi-decadal variability related to the influence of the {A}tlantic {M}ultidecadal {O}scillation ({AMO}) in the region. {H}igh power and persistent centennial-scale periodicities, similar to the {V}ries-{S}uess 200-year solar cycle, are observed as well. {I}ndeed, comparison between solar activity reconstructions and our record confirms the in-phase relationship on centennial time-scales. {L}ow delta {O}-18 values, and hence negative phases of {NAO} that bring precipitation towards the {W}estern {M}editerranean, are observed during well-known solar minima periods. {T}he results are consistent with previous models which describe low irradiance as a trigger for southward shifts of precipitation-bearing westerlies during winter.}, keywords = {{ATLANTIQUE} {NORD} ; {MEDITERRANEE} ; {MAROC}}, booktitle = {}, journal = {{S}cientific {R}eports - {N}ature}, volume = {8}, numero = {}, pages = {art. 17446 [8 p.]}, ISSN = {2045-2322}, year = {2018}, DOI = {10.1038/s41598-018-35498-x}, URL = {https://www.documentation.ird.fr/hor/fdi:010074506}, }