During the last century sea level rise strongly increased compared to sea level change in the last 2000 years. The present study investigates global and regional sea level change, simulated with the finite element sea-ice ocean model (FESOM). The major goal is to separate sea level change into steric and eustatic contributions and to estimate the influence of Greenland and Antarctic ice sheet melt on global and regional sea level. Modeled steric height variations show realistic regional geophysical patterns compared with steric height variations derived from altimetry measurements and GRACE. Compared to the time before the 1990 s, an increased global trend in steric sea level rise is found in estimates derived from the model and from satell...
A simulation of monthly global gravity coefficients has been created that represents time-variable h...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
During the last century sea level rise strongly increased compared to sea level change in the last 2...
During the last century sea level rise strongly increased compared to sea level change in the last 2...
Relative sea level change is estimated with a combination of methods. First a melting scenario with ...
Meltwater from the Greenland Ice Sheet (GIS) has been a major contributor to sea level change in the...
Variations in regional and global sea level are caused by different mechanisms. A major contributor ...
This study projects the sea level contribution from the Greenland ice sheet (GrIS) through to 2100, ...
Local sea level can deviate from mean global sea level because of both dynamic sea level (DSL) effec...
Relative sea level change of the recent past has several sources. Beside the thermo‐steric contribut...
Besides the warming of the ocean, sea level is mainly rising due to land ice mass loss of the major...
Observations of sea-level changes in the 20th century show a rise of 1 to 2 mm year−1, with accelera...
At present the biggest uncertainty in future sea level rise lies in the unknown contributions from ...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
A simulation of monthly global gravity coefficients has been created that represents time-variable h...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
During the last century sea level rise strongly increased compared to sea level change in the last 2...
During the last century sea level rise strongly increased compared to sea level change in the last 2...
Relative sea level change is estimated with a combination of methods. First a melting scenario with ...
Meltwater from the Greenland Ice Sheet (GIS) has been a major contributor to sea level change in the...
Variations in regional and global sea level are caused by different mechanisms. A major contributor ...
This study projects the sea level contribution from the Greenland ice sheet (GrIS) through to 2100, ...
Local sea level can deviate from mean global sea level because of both dynamic sea level (DSL) effec...
Relative sea level change of the recent past has several sources. Beside the thermo‐steric contribut...
Besides the warming of the ocean, sea level is mainly rising due to land ice mass loss of the major...
Observations of sea-level changes in the 20th century show a rise of 1 to 2 mm year−1, with accelera...
At present the biggest uncertainty in future sea level rise lies in the unknown contributions from ...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
A simulation of monthly global gravity coefficients has been created that represents time-variable h...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...
[1] We solve the sea-level equation to investigate the pattern of the gravitationally self-consisten...