How well would modern-day oceanic property distributions be known with paleoceanographic-like observations?
Gebbie, Geoffrey A.
Streletz, Gregory J.
Spero, Howard J.
MetadataShow full item record
KeywordWater mass geometry; Tracer distributions; Inverse methods; Last Glacial Maximum; Identical twin experiment; Isotope records
Compilations of paleoceanographic observations for the deep sea now contain a few hundred points along the oceanic margins, mid-ocean ridges, and bathymetric highs, where seawater conditions are indirectly recorded in the chemistry of buried benthic foraminiferal shells. Here we design an idealized experiment to test our predictive ability to reconstruct modern-day seawater properties by considering paleoceanographic-like data. We attempt to reconstruct the known, modern-day global distributions by using a state estimation method that combines a kinematic tracer transport model with observations that have paleoceanographic characteristics. When a modern-like suite of observations (Θ, practical salinity, seawater δ18O, inline image, PO4, NO3, and O2) is used from the sparse paleolocations, the state estimate is consistent with the withheld data at all depths below 1500 m, suggesting that the observational sparsity can be overcome. Physical features, such as the interbasin gradients in deep inline image and the vertical structure of Atlantic inline image, are accurately reconstructed. The state estimation method extracts useful information from the pointwise observations to infer distributions at the largest oceanic scales (at least 10,000 km horizontally and 1500 m vertically) and outperforms a standard optimal interpolation technique even though neither dynamical constraints nor constraints from surface boundary fluxes are used. When the sparse observations are more realistically restricted to the paleoceanographic proxy observations of δ13C, δ18O, and Cd/Ca, however, the large-scale property distributions are no longer recovered coherently. At least three more water mass tracers are likely needed at the core sites in order to accurately reconstruct the large-scale property distributions of the Last Glacial Maximum.
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 31 (2016): 472–490, doi:10.1002/2015PA002917.
Suggested CitationPaleoceanography 31 (2016): 472–490
Showing items related by title, author, creator and subject.
Smartphone-based distributed data collection enables rapid assessment of shorebird habitat suitability Thieler, E. Robert; Zeigler, Sara L.; Winslow, Luke A.; Hines, Megan K.; Read, Jordan S.; Walker, Jordan I. (Public Library of Science, 2016-11-09)Understanding and managing dynamic coastal landscapes for beach-dependent species requires biological and geological data across the range of relevant environments and habitats. It is difficult to acquire such information; ...
Robinson, Laura F.; Adkins, Jess F.; Fernandez, Diego P.; Burnett, Donald S.; Wang, S.-L.; Gagnon, Alexander C.; Krakauer, Nir (American Geophysical Union, 2006-05-24)In this study we use microsampling techniques to explore diagenetic processes in carbonates. These processes are important as they can affect the accuracy of U series chronometry. Fission track maps of deep-sea scleractinian ...
Distribution of postsynaptic density (PSD)-95 and Ca2+/calmodulin-dependent protein kinase II at the PSD Petersen, Jennifer D.; Chen, Xiaobing; Vinade, Lucia; Dosemeci, Ayse; Lisman, John E.; Reese, Thomas S. (Society for Neuroscience, 2003-12-03)Postsynaptic densities (PSDs) contain proteins that regulate synaptic transmission. We determined the positions of calcium/calmodulin-dependent protein kinase II (CaMKII) and PSD-95 within the three-dimensional structure ...