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Is sea level rise accelerating in the Chesapeake Bay? A demonstration of a novel new approach for analyzing sea level data
Author(s) -
Ezer Tal,
Corlett William Bryce
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl053435
Subject(s) - sea level rise , chesapeake bay , sea level , climatology , environmental science , bay , oceanography , coastal sea , geology , meteorology , climate change , estuary , geography
Sea level data from the Chesapeake Bay are used to test a novel new analysis method for studies of sea level rise (SLR). The method, based on Empirical Mode Decomposition and Hilbert‐Huang Transformation, separates the sea level trend from other oscillating modes and reveals how the mean sea level changes over time. Bootstrap calculations test the robustness of the method and provide confidence levels. The analysis shows that rates of SLR have increased from ∼1–3 mm y −1 in the 1930s to ∼4–10 mm y −1 in 2011, an acceleration of ∼0.05–0.10 mm y −2 that is larger than most previous studies, but comparable to recent findings by Sallenger and collaborators. While land subsidence increases SLR rates in the bay relative to global SLR, the acceleration results support Sallenger et al.'s proposition that an additional contribution to SLR from climatic changes in ocean circulation is affecting the region.