Local sea-level changes differ significantly from global-mean sea-level change as a result of
(1) non-climatic, geological background processes;(2) atmosphere/ocean dynamics; and (3) …

Several processes contributing to coastal relative sea-level (RSL) change in the North
Atlantic Ocean are observed and/or predicted to have distinctive spatial expressions that …

We assess the relationship between temperature and global sea-level (GSL) variability over
the Common Era through a statistical metaanalysis of proxy relative sea-level …

The flood hazard in New York City depends on both storm surges and rising sea levels. We
combine modeled storm surges with probabilistic sea-level rise projections to assess future …

A mixing model derived from first principles describes the bulk density (BD) of intertidal
wetland sediments as a function of loss on ignition (LOI). The model assumes that the bulk …

Coastal flood hazard varies in response to changes in storm surge climatology and the sea
level. Here we combine probabilistic projections of the sea level and storm surge …

Sea-level rise is a significant indicator of broader climate changes, and the time of
emergence concept can be used to identify when modern rates of sea-level rise emerged …

We evaluate paleo‐, historical, and future sea‐level rise along the US mid‐Atlantic coast.
The rate of relative sea‐level rise in New Jersey decreased from 3.5±1.0 mm/yr at 7.5–6.5 …

Using newly‐discovered archival measurements, we construct an instrumental record of
water levels and storm tides in Boston (MA) since 1825. After ascertaining the 19th century …

Identifying physical processes responsible for historical coastal sea-level changes is
important for anticipating future impacts. Recent studies sought to understand the drivers of …