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These problems point to increasingly polluted coastal environment caused by natural processes and human activities. These coupled activities are also consider as factor of global warming, resulting in sea-level rise. However, there are huge uncertainties still remain over the magnitude and rate of sea-level rise, which usually based on the regional scale studies, trough tectonic and geologic processes are difference in each coastal zone. Normally, beaches are dynamic environments. Shorelines are supposed to naturally shift and change with the tide and respond to changes in sea level. But when humans develop near the water, we further disrupt a beach’s ability to move and halt the natural processes that allow sand to replenish on its own. Intensified climate extremes combined with RSLR pose an increasing threat for future coastal security due to the complex and non-linear relationship between RSLR and erosion48,49. RSLR has been happening at an accelerated rate50,51, a trend projected to continue during the present century due to global warming52–55. The potential effects of RSLR can already be observed in areas undergoing strong land subsidence, such as in Semarang , where subsidence rates amount to 10 centimeters per year largely due to extensive groundwater extraction56. This has caused erosion in the order of 1.5 km close the city (Fig.6d–f) in the last decade, thus also increasing its exposure to coastal hazards. The morphological activity along the Caspian coasts is related with changes of Caspian Sea Level , mainly due to the variability of precipitation over the Volga River basin “personalized name new kids on the block tumbler”

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