We investigate the changes in surface water salinity intrusion lengths for estuaries around the world under influence of climate change. To do this, we make use of information from global data sets on present river geometry and present and predicted future river discharges, mean sea levels and tidal ranges, which we combine with various models for salt intrusion lengths. The used predictions are based on the RCP8.5 climate scenario and we use 2050 as time horizon, with the 10-percentile lowest discharge as representative value used as input in the intrusion length calculations. The salt intrusion models are two parametric descriptions and a semi-analytical model. With this, we calculate absolute and relative changes in salt intrusion length for a selection of estuaries around the world, to eventually scale up the analysis and develop a global map of changes in salt intrusion around the world under influence of climate change. The results so far indicate that many estuaries may be expected to experience a relative increase of salt intrusion length of over 10%. We also investigate which of the changing forcings most strongly affects the intrusion lengths and what type of estuary is most sensitive to changes. For most systems, the changes in river discharge characteristics are the most influential change, exceeding the influence of sea level rise. This study highlights the importance of studying the effect of climate change on estuarine salt intrusion in more detail, both in global analyses as in system specific detailed studies.@en