Coastal inundation due to sea level rise and extreme sea state and its potential impacts: Çukurova Delta case

With the rising sea level becoming a more pressing issue to coastal areas, a comprehensive analysis has been conducted to assess the vulnerability of the Çukurova Delta under the projected inundation by the end of the century. The level of inundation was estimated from a multimission satellite altimetry sea level anomaly and significant wave height data between September 1992 and February 2012. Superposed to the clear annual oscillation with 6.2 cm amplitude peaking around the beginning of October, the mean sea level signal exhibits a positive trend of 3.4 ± 0.1 mm/year over the altimetric data period. The extreme wave height with a 100-year return period is estimated to be about 6.1 ± 0.03 m, based on extreme probability distribution of the significant wave height data. In addition, taking the effects of tidal and meteorological forcings on the sea level into account, the maximum level of flooding expected to occur by the year 2100 reaches up to 6.7 m. GIS-based inundation mapping on the high resolution elevation model indicates that 69% of the area would be at risk of flooding. Nearshore settlements, lagoons, and the agricultural lands are the most severely impacted areas due to the inundation. The results can contribute to enhancing wetland conservation and management in the Çukurova Delta.

Coastal inundation due to sea level rise and extreme sea state and its potential impacts: Çukurova Delta case

With the rising sea level becoming a more pressing issue to coastal areas, a comprehensive analysis has been conducted to assess the vulnerability of the Çukurova Delta under the projected inundation by the end of the century. The level of inundation was estimated from a multimission satellite altimetry sea level anomaly and significant wave height data between September 1992 and February 2012. Superposed to the clear annual oscillation with 6.2 cm amplitude peaking around the beginning of October, the mean sea level signal exhibits a positive trend of 3.4 ± 0.1 mm/year over the altimetric data period. The extreme wave height with a 100-year return period is estimated to be about 6.1 ± 0.03 m, based on extreme probability distribution of the significant wave height data. In addition, taking the effects of tidal and meteorological forcings on the sea level into account, the maximum level of flooding expected to occur by the year 2100 reaches up to 6.7 m. GIS-based inundation mapping on the high resolution elevation model indicates that 69% of the area would be at risk of flooding. Nearshore settlements, lagoons, and the agricultural lands are the most severely impacted areas due to the inundation. The results can contribute to enhancing wetland conservation and management in the Çukurova Delta.

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Turkish Journal of Earth Sciences-Cover
  • ISSN: 1300-0985
  • Yayın Aralığı: Yılda 6 Sayı
  • Yayıncı: TÜBİTAK
Sayıdaki Diğer Makaleler

Mineralogical and physicochemical properties of talc from Emirdağ, Afyonkarahisar, Turkey

Bahri ERSOY, Sedef DİKMEN, Ahmet YILDIZ, Remzi GÖREN, Ömer ELİTOK

The Upper Cretaceous calciclastic submarine fan deposits in the Eastern Pontides, NE Turkey: facies architecture and controlling factors

Dilek SOFRACIOĞLU, Raif KANDEMİR

The Anzer glacial valley, at an elevation of over 2300 m in the Eastern Black Sea region of Turkey, exhibits evidence for a lowtemperature hydrothermal system (40 100 °C). Low-temperature hydrothermal systems usually do not receive attention since they are not useful for energy production. However,

Abdullah KARAMAN

Low-sulfidation epithermal Au-Ag mineralization in the Sındırgı District, Balıkesir Province, Turkey

Hüseyin YILMAZ, Fatma Nuran SÖNMEZ, Erhan AKAY, Ahmet Kerim ŞENER, Seda TEZEL TUFAN

The mineralogy and geochemistry of Neogene sediments from eastern Turkey, southeast of Arapgir (Malatya)

Dicle BAL AKKOCA, Zeynep BAYTAŞOĞLU

Coastal inundation due to sea level rise and extreme sea state and its potential impacts: Çukurova Delta case

Özlem SİMAV, Dursun Zafer ŞEKER, Cem GAZİOĞLU

The geochemistry and petrology of the ophiolitic rocks from the Kahramanmaraş region, southern Turkey

Utku BAĞCI

Colour origin of red sandstone beds within the Hüdai Formation (Early Cambrian), Aydıncık (Mersin), southern Turkey

Muhsin EREN Selahattin KADİR

A method based on the Van der Hoven spectrum for performance evaluation in prediction of wind speed

Elif KAYA, Burak BARUTÇU, Şükran Sibel MENTEŞ

Geology and diagenesis of a zeolitic Foça tuff unit deposited in a Miocene phreatomagmatic lacustrine environment (western Anatolia)

Mustafa ALBAYRAK, Abdullah Mete ÖZGÜNER