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Magdalena Andres

Researcher at Woods Hole Oceanographic Institution

Publications -  47
Citations -  1334

Magdalena Andres is an academic researcher from Woods Hole Oceanographic Institution. The author has contributed to research in topics: Gulf Stream & Continental shelf. The author has an hindex of 19, co-authored 41 publications receiving 1044 citations. Previous affiliations of Magdalena Andres include University of Rhode Island.

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Geochemical segmentation of the Mid-Atlantic Ridge north of Iceland and ridge-hot spot interaction in the North Atlantic

TL;DR: In this article, the isotopic compositions of Pb are somewhat decoupled from those of other isotopic systems due to nonlinear mixing relationships between isotope compositions of different elements and elemental fractionation by magmatic processes.
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Observations of Kuroshio flow variations in the East China Sea

TL;DR: In this paper, a 23-month study using inverted echo sounders and acoustic Doppler current profilers (ADCPs) along the regularly sampled PN-line was performed to investigate the kuroshio velocity structure and transport in the East China Sea.
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On the recent destabilization of the Gulf Stream path downstream of Cape Hatteras

TL;DR: Mapped satellite altimetry reveals interannual variability in the position of initiation of Gulf Stream meanders downstream of Cape Hatteras, and in situ data suggest that this shift has increased both upper-ocean/deep-offshore interaction events at Line W and open ocean/shelf interactions across the Middle Atlantic Bight (MAB) shelf break.
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Study of the Kuroshio/Ryukyu Current System Based on Satellite-Altimeter and in situ Measurements

TL;DR: In this article, a 12-year time series of ECS-Kuroshio transport crossing the C-line (KT) is used to determine an empirical relationship between sea-level anomaly difference (SLA) across the Kuroshio in the East China Sea and net transport near 28°N.
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Direct interaction between the Gulf Stream and the shelfbreak south of New England

TL;DR: Sea surface temperature imagery, satellite altimetry, and a surface drifter track reveal an unusual tilt in the Gulf Stream path that brought Gulf Stream water to 39.9°N near the Middle Atlantic Bight shelfbreak in October 2011, and near-bottom temperature measurements from lobster traps on the outer continental shelf show distinct warming events in November and December 2011.