“…These short-term measurements of process rates (for example, sediment accretion, root expansion, belowground primary production and decomposition, autocompaction and soil shrink-swell) can be used to calibrate, parameterize and validate locally relevant models 36 to make longer-term predictions of coastal wetland response to changes in the rate of SLR. Thus, although RSET data provide direct, shortterm indications of marsh resilience, modelling allows prediction at the appropriate timescales for management action 35,42,43,58 . Second, to calculate the local difference between wetland elevation change and sea-level change so that absolute site vulnerability can be compared across sites over a broad geographic area (for example, a continent), RSETs need to be levelled (referenced) into a common regional vertical datum 59 .…”