Sea level rise can bring disastrous outcomes to people living in coastal regions by increasing flood risk or inducing stronger storm surges. We study long-term linear trends in monthly maximum sea levels by applying extreme value methods. The monthly maximum sea levels are extracted from multiple tide gauges around the coastal regions of the world over a period of as long as 169 years. Due to instrument changes, location changes, earthquakes, land reclamation, dredging, etc., the sea level data could contain inhomogeneous shifts in their means, which can substantially impact trend estimates if ignored. To rigorously quantify the long-term linear trends and return levels for the monthly maximum sea level data, we use a genetic algorithm to e...
Tide gauge data are used to estimate trends in global sea level for the period from 1955 to 2007. Li...
Sea level change prior to 1993 is described by time varying amplitudes of spatial EOFs, in analogy t...
It is sometimes assumed that changes in risks of coastal flooding can be computed by just adding mea...
This dissertation examines long-term trends in extreme environmental events with considerations for ...
The paper presents the sea level rises (SLR) computed for the United States tide gauges with more th...
A quasi-global sea level data set from tide gauges has been used to investigate extreme sea level ev...
We analyze the Permanent Service for Mean Sea Level (PSMSL) database of sea level time series using ...
Extreme sea levels at European coasts and their changes over the twentieth and twenty-first centurie...
Extreme sea levels along the densely monitored coasts of the North Atlantic Ocean and the Gulf of Me...
The paper provides an estimate of the latest relative and absolute rates of rise and accelerations o...
We demonstrate that long-term tidally induced changes in extreme sea levels affect estimates of majo...
Although there are over 1,800 globally distributed tide gauge stations, only a few hundred of them a...
International audienceDetection and attribution of human influence on sea level rise are important t...
Abstract. Mean sea level is a variable of considerable in-terest in meteorological and oceanographic...
We analyze a set of 20 tide gauge records covering the contiguous United States (US) coastline and t...
Tide gauge data are used to estimate trends in global sea level for the period from 1955 to 2007. Li...
Sea level change prior to 1993 is described by time varying amplitudes of spatial EOFs, in analogy t...
It is sometimes assumed that changes in risks of coastal flooding can be computed by just adding mea...
This dissertation examines long-term trends in extreme environmental events with considerations for ...
The paper presents the sea level rises (SLR) computed for the United States tide gauges with more th...
A quasi-global sea level data set from tide gauges has been used to investigate extreme sea level ev...
We analyze the Permanent Service for Mean Sea Level (PSMSL) database of sea level time series using ...
Extreme sea levels at European coasts and their changes over the twentieth and twenty-first centurie...
Extreme sea levels along the densely monitored coasts of the North Atlantic Ocean and the Gulf of Me...
The paper provides an estimate of the latest relative and absolute rates of rise and accelerations o...
We demonstrate that long-term tidally induced changes in extreme sea levels affect estimates of majo...
Although there are over 1,800 globally distributed tide gauge stations, only a few hundred of them a...
International audienceDetection and attribution of human influence on sea level rise are important t...
Abstract. Mean sea level is a variable of considerable in-terest in meteorological and oceanographic...
We analyze a set of 20 tide gauge records covering the contiguous United States (US) coastline and t...
Tide gauge data are used to estimate trends in global sea level for the period from 1955 to 2007. Li...
Sea level change prior to 1993 is described by time varying amplitudes of spatial EOFs, in analogy t...
It is sometimes assumed that changes in risks of coastal flooding can be computed by just adding mea...