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  "author": "Rick Hennekam (Royal Netherlands Institute for Sea 
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  "author": "Rick Hennekam (Royal Netherlands Institute for Sea 
            
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Research)",
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Research)",
            
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  "author_email": "rick.hennekam@nioz.nl",
            
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  "code": "7b.b.zj",
            
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  "contributor": "Royal Netherlands Institute for Sea Research 
            
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(NIOZ)",
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(NIOZ)",
            
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\"Hennekam\",\"orcid\":\"0000-0002-8823-4519\",\"affiliation\":\"Royal 
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\"Hennekam\",\"orcid\":\"0000-0002-8823-4519\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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\"contactemailaddress\":\"rick.hennekam@nioz.nl\",\"formatted\":\"Rick 
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\"contactemailaddress\":\"rick.hennekam@nioz.nl\",\"formatted\":\"Rick 
            
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Hennekam - Royal Netherlands Institute for Sea Research - ORCID: 
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Hennekam - Royal Netherlands Institute for Sea Research - ORCID: 
            
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0000-0002-8823-4519 - Corresponding Author - 
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0000-0002-8823-4519 - Corresponding Author - 
            
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illem\",\"lastname\":\"Toonen\",\"orcid\":null,\"affiliation\":\"Vrije 
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illem\",\"lastname\":\"Toonen\",\"orcid\":null,\"affiliation\":\"Vrije 
            
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Universiteit 
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Universiteit 
            
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ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Willem 
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ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Willem 
            
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Toonen - Vrije Universiteit Amsterdam - ORCID: 
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Toonen - Vrije Universiteit Amsterdam - ORCID: 
            
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\"Fei\",\"lastname\":\"Peng\",\"orcid\":null,\"affiliation\":\"Lanzhou 
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\"Fei\",\"lastname\":\"Peng\",\"orcid\":null,\"affiliation\":\"Lanzhou 
            
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spondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Fei 
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spondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Fei 
            
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Peng - Lanzhou University - ORCID: \"}]",
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Peng - Lanzhou University - ORCID: \"}]",
            
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  "deposit_date": "2025-08-20",
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  "deposit_date": "2025-08-20",
            
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  "depositor": "Rick Hennekam (rick.hennekam@nioz.nl)",
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  "depositor": "Rick Hennekam (rick.hennekam@nioz.nl)",
            
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  "distribution_date": "2025-08-20",
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  "distribution_date": "2025-08-20",
            
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
            
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Institute for Sea Research)",
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Institute for Sea Research)",
            
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  "doi_date_published": "2025-09-16T10:37:47.8938156",
            
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  "funding_references": "[{\"name\":\"National Natural Science 
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  "funding_references": "[{\"name\":\"National Natural Science 
            
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Foundation of 
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Foundation of 
            
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wardnumber\":\"42101002\",\"awardtitle\":null,\"formatted\":\"National 
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wardnumber\":\"42101002\",\"awardtitle\":null,\"formatted\":\"National 
            
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Natural Science Foundation of China - 42101002 
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Natural Science Foundation of China - 42101002 
            
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-\"},{\"name\":\"Natural Science Foundation of Gansu 
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-\"},{\"name\":\"Natural Science Foundation of Gansu 
            
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wardnumber\":\"25JRRA690\",\"awardtitle\":null,\"formatted\":\"Natural 
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wardnumber\":\"25JRRA690\",\"awardtitle\":null,\"formatted\":\"Natural 
            
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Science Foundation of Gansu Province - 25JRRA690 -\"}]",
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Science Foundation of Gansu Province - 25JRRA690 -\"}]",
            
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  "maintainer": "Rick",
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  "maintainer": "Rick",
            
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  "name": 
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  "name": 
            
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eveals-nao-driven-decadal-to-multi-centennial-variability---xrf-core",
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eveals-nao-driven-decadal-to-multi-centennial-variability---xrf-core",
            
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  "notes": "These files contain raw X-ray fluorescence (XRF) core 
49
  "notes": "These files contain raw X-ray fluorescence (XRF) core 
            
49
scanning data and line scan data of the Buggenum and Ravenstein cores 
50
scanning data and line scan data of the Buggenum and Ravenstein cores 
            
50
used in Peng et al. (2025). The abstract of that publication: A 
51
used in Peng et al. (2025). The abstract of that publication: A 
            
51
central challenge in assessing climate-driven flood regimes is 
52
central challenge in assessing climate-driven flood regimes is 
            
52
constructing long-term paleoflood records with sufficient temporal 
53
constructing long-term paleoflood records with sufficient temporal 
            
53
resolution to identify both short- and long-term variability. To 
54
resolution to identify both short- and long-term variability. To 
            
54
address this, we performed grain-size and X-ray fluorescence scanning 
55
address this, we performed grain-size and X-ray fluorescence scanning 
            
55
analyses on two cores from paleochannels in the Lower Meuse (the 
56
analyses on two cores from paleochannels in the Lower Meuse (the 
            
56
Netherlands). The downcore ln(Zr/Rb) ratio proves to be a reliable 
57
Netherlands). The downcore ln(Zr/Rb) ratio proves to be a reliable 
            
57
grain-size proxy, allowing reconstruction of flood-related sediment 
58
grain-size proxy, allowing reconstruction of flood-related sediment 
            
58
input variations. We find the flood intensity record displays a 
59
input variations. We find the flood intensity record displays a 
            
59
~300-yr cycle, synchronous to that observed in the North Atlantic 
60
~300-yr cycle, synchronous to that observed in the North Atlantic 
            
60
Oscillation record, and both records are synchronous at this band. 
61
Oscillation record, and both records are synchronous at this band. 
            
61
Importantly, a persistent quasi-decadal (7-10 years) oscillation 
62
Importantly, a persistent quasi-decadal (7-10 years) oscillation 
            
62
indicate a persistently active flooding regime and hydrological 
63
indicate a persistently active flooding regime and hydrological 
            
63
stationarity throughout the Late Holocene. This study advances 
64
stationarity throughout the Late Holocene. This study advances 
            
64
paleoflood methodology by demonstrating that paleochannel infills 
65
paleoflood methodology by demonstrating that paleochannel infills 
            
65
provide valuable archives for reconstructing flood histories across 
66
provide valuable archives for reconstructing flood histories across 
            
66
multi-annual to millennial intervals, thus enhancing our ability to 
67
multi-annual to millennial intervals, thus enhancing our ability to 
            
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track hydrological responses to climate variability across multiple 
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track hydrological responses to climate variability across multiple 
            
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timescales.",
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timescales.",
            
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