English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

Sea level is a very changeable surface. Furthermore, the land may also be moving, in a slower rate, generating relative sea level changes. The causes of relative sea level changes are variable, but the ones that cause more intense variations are related to climate. During Little Ice Age (LIA) Northern Hemisphere's summer temperatures fell significantly below the AD 1961‐1990 range. This climate situation was responsible for a greater discharge of rivers, which could lead to a greater transportation of sediments to the coastline. During these cold periods, sea level was lower than in present time. All this could imply a coastline progradation, with the successive abandon of older beach ridges, reinforcing the sandy supply for dune building. The coastal situation should be, in some sense, the opposite of the situations that we face today. In present warm period, rivers carry less sediment than during LIA. Moreover, the recent sea level rise contributes to a coastal migration inlands and the erosion of previous beaches and dunes. Our investigation on ancient marine levels and Holocene cemented dunes suggests that the area near Esmoriz (20 km south of Porto, NW Portuguese coast) is probably subsiding. This possible subsidence, together with recent sea level rise, induced by the end of LIA, could explain the severe coastal erosion that is taking place at Espinho area (15 km south of Porto) since the middle of the XIX century. This example shows clearly the complexity of relative sea-level changes. Because of this complexity, sea level curves are not similar worldwide, as they depend on the interference of multiple time-scales phenomena.

Climate, tectonics and beach erosion: the case of Espinho (NW Portuguese coast)