Uncertainties in Representative Concentration Pathway (RCP) scenarios and Antarctic Ice Sheet (AIS) melt propagate into uncertainties in projected mean sea-level (MSL) changes and extreme sea-level (ESL) events. Here we quantify the impact of RCP scenarios and AIS contributions on 21st-century ESL changes at tide-gauge sites across the globe using extreme-value statistics. We find that even under RCP2.6, almost half of the sites could be exposed annually to a present-day 100-year ESL event by 2050. Most tropical sites face large increases in ESL events earlier and for scenarios with smaller MSL changes than extratropical sites. Strong emission reductions lower the probability of large ESL changes but due to AIS uncertainties, cannot fully e...
Estimating the future evolution of the Antarctic Ice Sheet (AIS) is critical for improving future se...
The land ice contribution to global mean sea level rise has not yet been predicted1 using ice sheet ...
We present gravitationally self-consistent predictions of sea level change that would follow the dis...
Uncertainties in Representative Concentration Pathway (RCP) scenarios and Antarctic Ice Sheet (AIS) ...
Mechanisms such as ice-shelf hydrofracturing and ice-cliff collapse may rapidly increase discharge f...
The potential for break-up of Antarctic ice shelves by hydrofracturing and following ice cliff insta...
Presented at the PALSEA Express 2020 virtual meeting on September 16, 2020. Project funding by: NSF...
Increases in ocean temperatures in the Filchner Ronne region of Antarctica are likely to result in i...
Atmospheric warming is projected to increase global mean surface temperatures by 0.3 to 4.8 degrees ...
Global warming is expected to drive increasing extreme sea levels (ESLs) and flood risk along the wo...
The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐enhanced climate ...
Estimating the future evolution of the Antarctic Ice Sheet (AIS) is critical for improving future se...
The land ice contribution to global mean sea level rise has not yet been predicted1 using ice sheet ...
We present gravitationally self-consistent predictions of sea level change that would follow the dis...
Uncertainties in Representative Concentration Pathway (RCP) scenarios and Antarctic Ice Sheet (AIS) ...
Mechanisms such as ice-shelf hydrofracturing and ice-cliff collapse may rapidly increase discharge f...
The potential for break-up of Antarctic ice shelves by hydrofracturing and following ice cliff insta...
Presented at the PALSEA Express 2020 virtual meeting on September 16, 2020. Project funding by: NSF...
Increases in ocean temperatures in the Filchner Ronne region of Antarctica are likely to result in i...
Atmospheric warming is projected to increase global mean surface temperatures by 0.3 to 4.8 degrees ...
Global warming is expected to drive increasing extreme sea levels (ESLs) and flood risk along the wo...
The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐enhanced climate ...
Estimating the future evolution of the Antarctic Ice Sheet (AIS) is critical for improving future se...
The land ice contribution to global mean sea level rise has not yet been predicted1 using ice sheet ...
We present gravitationally self-consistent predictions of sea level change that would follow the dis...