One that touches on the local difference in sea level rise from the average.
http://www.knmi.nl/bibliotheek/knmipubWR/WR2009-05.pdfThis international scientific assessment has been carried out at the request of the
Dutch Delta Committee. The Committee requested that the assessment explore
the high-end climate change scenarios for flood protection of the Netherlands. It
is a state-of–the art scientific assessment of the upper bound values and longer
term projections (for sea level rise up to 2200) of climate induced sea level rise,
changing storm surge conditions and peak discharge of river Rhine. It comprises
a review of recent studies, model projections and expert opinions of more than
20 leading climate scientists from different countries around the North Sea,
Australia and the USA. Although building on the previous IPCC AR4 (2007) and
KNMI (2006) assessments, this report deliberately explores low probability/high
impact scenarios, which will pose significant threats to the safety of people and
infrastructure and capital invested below sea level. According to its high-end
estimates global mean sea level may rise in the range of 0.55 - 1.10 m in 2100
and 1.5 - 3.5 m in 2200, when higher temperature rise scenarios (up to 6 °C by
2100) and increased ice discharge from Antarctica are considered. This would
correspond with local sea levels along the coast of the Netherlands of up to
maximally 1.20 m in 2100 and 4 m in 2200. An increase in peak discharge of
river Rhine of 3 to 19% for 2050 and 6 to 38% for 2100 is foreseen. The storm
regime along the Dutch North Sea coast in terms of maximum surge level will
probably not change significantly in this extreme climate change frame.