A New Centennial Sea‐Level Record for Antalya, Eastern Mediterranean

  • U. Ozturk
  • , N. Marwan
  • , S. von Specht
  • , O. Korup
  • , J. Jensen

Veröffentlichungen: Beitrag in FachzeitschriftArtikelPeer Reviewed

Abstract

Quantitative estimates of sea-level rise in the Mediterranean Basin become increasingly accurate thanks to detailed satellite monitoring. However, such measuring campaigns cover several years to decades, while longer-term sea-level records are rare for the Mediterranean. We used a data archeological approach to reanalyze monthly mean sea-level data of the Antalya-I (1935–1977) tide gauge to fill this gap. We checked the accuracy and reliability of these data before merging them with the more recent records of the Antalya-II (1985–2009) tide gauge, accounting for an eight-year hiatus. We obtain a composite time series of monthly and annual mean sea levels spanning some 75 years, providing the longest record for the eastern Mediterranean Basin, and thus an essential tool for studying the region's recent sea-level trends. We estimate a relative mean sea-level rise of 2.2 ± 0.5 mm/year between 1935 and 2008, with an annual variability (expressed here as the standard deviation of the residuals, σ residuals = 41.4 mm) above that at the closest tide gauges (e.g., Thessaloniki, Greece, σ residuals = 29.0 mm). Relative sea-level rise accelerated to 6.0 ± 1.5 mm/year at Antalya-II; we attribute roughly half of this rate (~3.6 mm/year) to tectonic crustal motion and anthropogenic land subsidence. Our study highlights the value of data archeology for recovering and integrating historic tide gauge data for long-term sea-level and climate studies.

OriginalspracheEnglisch
Seiten (von - bis)4503-4517
Seitenumfang15
FachzeitschriftJournal of Geophysical Research: Oceans
Jahrgang123
Ausgabenummer7
DOIs
PublikationsstatusVeröffentlicht - Juli 2018
Extern publiziertJa

Fördermittel

We are particularly grateful to the General Command of Mapping for their cooperation in data sharing (https://www.hgk.msb.gov.tr/harita-dergisi) and acknowledge Erdinc Sezen for his valuable comments and precious explanations about the historical data and local aspects of the Gulf of Adalya Basin. We also appreciate Robert Dill for providing extensive information concerning nonlinear natural factors that affect vertical land motion. We thank Sönke Dangendorf for his support, and appreciate formal reviews by Andre Stettner-Davis, Darwin Fox, and the Editor, who greatly improved an earlier manuscript. We acknowledge using the 20th Century Reanalysis V2 data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA (https://www.esrl.noaa.gov/psd/); the Global CMT Project data (www.globalcmt.org); and the PSMSL data, UK (http://www.psmsl.org/data/). This study was funded by Deutsche Forschungsgemeinschaft (DFG) within the NatRiskChange Graduate School (GRK 2043/1) at the University of Potsdam. The raw and offsets corrected Antalya (1935–2009) time series are provided as supporting information. We are particularly grateful to the General Command of Mapping for their cooperation in data sharing (https:// www.hgk.msb.gov.tr/harita-dergisi) and acknowledge Erdinc Sezen for his valuable comments and precious explanations about the historical data and local aspects of the Gulf of Adalya Basin. We also appreciate Robert Dill for providing extensive information concerning nonlinear natural factors that affect vertical land motion. We thank Sönke Dangendorf for his support, and appreciate formal reviews by Andre Stettner-Davis, Darwin Fox, and the Editor, who greatly improved an earlier manuscript. We acknowledge using the 20th Century Reanalysis V2 data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA (https:// www.esrl.noaa.gov/psd/); the Global CMT Project data (www.globalcmt.org); and the PSMSL data, UK (http://www. psmsl.org/data/). This study was funded by Deutsche Forschungsgemeinschaft (DFG) within the NatRiskChange Graduate School (GRK 2043/1) at the University of Potsdam. The raw and offsets corrected Antalya (1935–2009) time series are provided as supporting information.

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