Results 31 to 40 of about 238,924 (290)
The Depositional Record, EarlyView.A classical peripheral foreland basin is bounded longitudinally by a pair of marginal ocean basins (DeCelles & Giles, 1996). The WTFB sediments transfer to adjacent marginal ocean basins. The western Taiwan foreland basin (WTFB) is regarded as a classical peripheral foreland basin, longitudinally bounded by the southern Okinawa Trough (SOT) to the ...
Cheng‐Shing Chiang +2 more
wiley +1 more source
Erratum : GEOTRACES radium isotopes interlaboratory comparison experiment [PDF]
, 2012 Author Posting. © Association for the Sciences of Limnology and Oceanography, 2012. This article is posted here by permission of Association for the Sciences of Limnology and Oceanography for personal use, not for redistribution. The definitive version
Charette, Matthew A. +6 more
core +1 more source
The first 25 years of satellite carbonate sedimentology: What have we learned?
The Depositional Record, EarlyView.Observations of the suspension and transport of carbonate sediments from reefs, banks and shallow shelves have been made by satellite instruments for ca 25 years. With an increasing number of instruments in space, providing advanced observational capabilities, remarkable insights have been gained concerning carbonate sedimentological processes. Details
James G. Acker, R. Jude Wilber
wiley +1 more source
Shape Optimization for the Mitigation of Coastal Erosion via Smoothed Particle Hydrodynamics [PDF]
arXiv, 2022 Adjoint-based shape optimization most often relies on Eulerian flow field formulations. However, since Lagrangian particle methods are the natural choice for solving sedimentation problems in oceanography, extensions to the Lagrangian framework are desirable. For the mitigation of coastal erosion, we perform shape optimization for fluid flows, that are
arxiv
Report on the new boat "Alexander Agassiz" of the La Jolla Marine Station [PDF]
, 1908 The San Diego Marine Biological Association was briefly known as the La Jolla Marine Station, and then became the Scripps Institution of Oceanography in 1912.
University of California
core
Reviews of Geophysics, 1983 Interest and activity in the equatorial oceans (defined arbitrarily as that part of the oceans within ten degrees of the equator) have undergone a remarkable expansion in the last four years. The previous IUGG report (O'Brien, 1979) listed about one hundred references – the present one lists over two hundred and fifty.
Cane, Mark A., Sarachik, E. S.
openaire +4 more sources
Ecohydrology, Volume 18, Issue 2, March 2025.ABSTRACT Water transport timescales (WTTs) quantify how long it takes for water to travel through or remain in a system and are often cast as indicators of ecosystem function and health. Such timescales are known to be affected by vegetation in various environments. We quantify the impact of floodplain vegetation on WTTs within the Wax Lake Delta (WLD),
Madoche Jean Louis, Matthew Hiatt
wiley +1 more source
Fisheries oceanography – processes, patterns & variability- Winter School on towards Ecosystem Based Management of Marine Fisheries – Building Mass Balance Trophic and Simulation Models [PDF]
, 2004 Oceanography is the scientific discipline concerned with all aspects of the world's oceans and seas, including their physical and chemical properties, their origin and geologic framework, and the life forms that inhabit the marine environment ...
Rajagopalan, M, Vijayakumaran, K
core
Food Bioengineering, EarlyView.BslA is a promising tool to create an robust self‐emulsifying biocatalysis platform by reducing the droplet sizes of emulsion and improving its stability. It could guarantee the efficient hydrolysis of astaxanthin esters catalyzed by Est3‐14 without extra emusifier, increasing the yield of free astaxanthin to 184 μg·mL−1.
Xiaoxuan Yao +7 more
wiley +1 more source
Large Time existence For 1D Green-Naghdi equations [PDF]
arXiv, 2009 We consider here the $1D $ Green-Naghdi equations that are commonly used in coastal oceanography to describe the propagation of large amplitude surface waves. We show that the solution of the Green-Naghdi equations can be constructed by a standard Picard iterative scheme so that there is no loss of regularity of the solution with respect to the initial
arxiv