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  • Age; AGE; Arid environment; Caesium-137, activity; Caesium-137, activity, error; Carbon, organic, total; Carbon, organic, total, error, relative; Carbon, organic/Nitrogen, total ratio; Carbon, organic/Nitrogen, total ratio, error; Carbon, organic/Sulfur ratio, error; Carbon, organic total/Sulfur, total, ratio; Carbon and nitrogen and sulfur (CNS) isotope element analyzer, Elementar, Vario EL III; Climate change; Coastal impacts; DEPTH, sediment/rock; Element analyser, Thermo Scientific FLASH2000; GC; Geochemistry; Grain size, mean; Gravity corer; Lacustrine_lagoon_THIII; Lead-210 activity per mass, excess; Lead-210 activity per mass, excess, error; Morocco; Radium-226 activity per mass; Radium-226 activity per mass, error; remote sensing; Saharan wetlands; Sedimentary chlorophyll; Sedimentary chlorophyll, error; δ13C; δ13C, error  (1)
  • Coastal dynamics  (1)
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  • 1
    Publication Date: 2023-11-02
    Description: The core was collected manually from a boat employing a gravity core sampler. The core was sliced every two centimeters in the field, packed in individual identified plastics bags, and kept refrigerated. The THIII sediment core (N 28°01.626, W 12°16.558), measuring 48 cm, was recovered in one of the sections of the main water entrance channel in the Lagoon. This site is approximately seven meters deep and lies between two islets of exposed sediment dominated by marine grass specimens of *Zostera noltii*. During the sampling, salinity at the site was 40 PSU (Practical Salinity Unit). Due to its proximity to the inlet, this site is highly influenced by the seawater entrance and ocean nutrients. Aiming the recognition of the environmental changes at this point of the lagoon, we have performed the following measurements in the core's sediments: isotopic ratio of C, dating (210Pb and 137Cs calibration), sedimentation rate, mean grain size, Chlorophyll, Total Organic Carbon (TOC), C/N elemental ratio and C/S elemental ratio.
    Keywords: Age; AGE; Arid environment; Caesium-137, activity; Caesium-137, activity, error; Carbon, organic, total; Carbon, organic, total, error, relative; Carbon, organic/Nitrogen, total ratio; Carbon, organic/Nitrogen, total ratio, error; Carbon, organic/Sulfur ratio, error; Carbon, organic total/Sulfur, total, ratio; Carbon and nitrogen and sulfur (CNS) isotope element analyzer, Elementar, Vario EL III; Climate change; Coastal impacts; DEPTH, sediment/rock; Element analyser, Thermo Scientific FLASH2000; GC; Geochemistry; Grain size, mean; Gravity corer; Lacustrine_lagoon_THIII; Lead-210 activity per mass, excess; Lead-210 activity per mass, excess, error; Morocco; Radium-226 activity per mass; Radium-226 activity per mass, error; remote sensing; Saharan wetlands; Sedimentary chlorophyll; Sedimentary chlorophyll, error; δ13C; δ13C, error
    Type: Dataset
    Format: text/tab-separated-values, 378 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: 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 Journal of Geophysical Research: Oceans 121 (2016): 5134–5163, doi:10.1002/2015JC011468.
    Description: The pathways and physical mechanisms associated with intrusions of cold, nutrient-rich South Atlantic Central Water (SACW) on the continental shelf of the Espírito Santo Basin (ESB), off southeast Brazil (18°S–22°S), are investigated. To this end, a set of process-oriented, Primitive-Equation (PE) numerical models are used, together with an independent and more complete PE model, available observations and simple theoretical ideas. SACW enters the model ESB shelf mostly through two preferential pathways along the Tubarão Bight (TB, 19.5°S–22°S). These pathways are found to be locations where an equatorward along-isobath pressure gradient force (PGFy*) of inline image m s−2) develops in response to steady wind forcing. This equatorward PGFy* is essentially in geostrophic balance, inducing onshore flow across the shelf edge, and most of the shelf proper. The Brazil Current (BC) imparts an additional periodic (in the along-shelf direction) PGFy* on the shelf. The intrinsic pycnocline uplifting effect of the BC in making colder water available at the shelf edge is quantified. The BC also induces local intrusions by inertially overshooting the shelf edge, consistent with estimated Rossby numbers of inline image0.3–0.5. In addition, the planetary β-effect is related to a background equatorward PGFy*. A modified Arrested Topographic Wave model is shown to be a plausible rationalization for the shelf-wide spreading of the pressure field imparted by the BC at the shelf edge. The deep-ocean processes examined here are found to enhance the onshore transport of SACW, while wind forcing is found to dominate it at leading order.
    Description: The first author acknowledges support from the S~ao Paulo Research Foundation (Fundac¸~ao de Amparo a Pesquisa do Estado de S~ao Paulo, FAPESP), via grants 2013/11465–4 and 2014/03451–6. Kenneth Brink acknowledges support from NSF (grant OCE-1433953). Ilson da Silveira acknowledges support from FAPESP 08/58101–9, CNPq 3071122/2010–7, and CAPES 2201/2014. Wilton Arruda acknowledges support from CNPq (MCTI/CNPq/Universal 14/2014, grant 443162/2014–0), and from INCT–Mar– COI, MCTI/CNPq grant 565062/2010–7. Renato Martins acknowledges support from Petr oleo Brasileiro S/A (AMBES Project, PT–133.01.10636).
    Description: 2017-01-30
    Keywords: Cross-shelf transport ; Brazil current ; Coastal dynamics ; South Atlantic Central Water ; Deep-ocean forcing ; Arrested topographic wave
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
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