Last edited by Shale
Sunday, July 19, 2020 | History

3 edition of Interhemispheric water exchange in the Atlantic Ocean found in the catalog.

Interhemispheric water exchange in the Atlantic Ocean

Interhemispheric water exchange in the Atlantic Ocean

  • 166 Want to read
  • 4 Currently reading

Published by Elsevier in Amsterdam, Boston .
Written in English

    Subjects:
  • Ocean circulation -- Atlantic Ocean,
  • Ocean-atmosphere interaction -- Atlantic Ocean

  • Edition Notes

    Includes bibliographical references and index

    Statementedited by G.J. Goni and P. Malanotte-Rizzoli
    SeriesElsevier oceanography series -- 68
    ContributionsGoni, G. J, Malanotte-Rizzoli, Paola, 1946-
    Classifications
    LC ClassificationsGC228.6.A73 I55 2003
    The Physical Object
    Paginationxv, 506 p. :
    Number of Pages506
    ID Numbers
    Open LibraryOL17103036M
    ISBN 100444512675
    LC Control Number2003059218

    Originality Statement I hereby declare that this submission is my own work and to the best of my knowl-edge it contains no materials previously published or written by another per. The South Atlantic por Gerold Wefer, , disponible en Book Depository con envío gratis.

    Abstract. Our view of the ocean’s role in climate change has changed substantially during the past ten years. Back then, changes in ocean circulation and deep-ocean carbon storage have been perceived as key players in climate change in that they have the capacity to cause changes in regional and interhemispheric marine heat transports and ocean- atmosphere carbon exchange thereby altering.   Eventually, the water mixes with warmer water and returns to the Atlantic to complete the circulation. The principal engine of this global circulation, often called the Ocean Conveyor, is the difference in salt content between the Atlantic and Pacific Oceans. Before the Isthmus of Panama existed, Pacific surface waters flowed into the Atlantic.

      David Frum is a staff writer at The Atlantic and the author of Trumpocalypse: Restoring American Democracy. In and , he was a speechwriter for President George W. Bush.   The ballast water management standards are being phased in over a period of time. New ships must meet the ballast water treatment standard. Existing ships should exchange ballast water mid-ocean but they will need to meet the ballast water treatment standard by the date of .


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Interhemispheric water exchange in the Atlantic Ocean Download PDF EPUB FB2

Interhemispheric Water Exchange in the Atlantic Ocean COVID Update: We are currently shipping orders daily. However, due to transit disruptions in some geographies, deliveries may be delayed.

To provide all customers with timely access to content, we are offering 50% off Science and Technology Print & eBook bundle Edition: 1. A.L. Gordon The interhemispheric exchange of the warm water within the upper kilometer of the tropical Atlantic is the main theme of the excellent collection of research papers or chapters composing the book.

Get this from a library. Interhemispheric water exchange in the Atlantic Ocean. [G J Goni; Paola Malanotte-Rizzoli;] -- Recent results from modeling and observational studies demonstrate that the tropical Atlantic is a critical region for processes that maintain. Journals & Books; Help; Elsevier Oceanography Series.

Articles and issues. Latest volume All volumes. Search in this book series. Interhemispheric Water Exchange in the Atlantic Ocean. Edited by G.J. Goni, P select article Comparison of hydrographic and altimeter based estimates of sea level Interhemispheric water exchange in the Atlantic Ocean book variability in the Atlantic Ocean.

https. (ebook) Interhemispheric Water Exchange in the Atlantic Ocean () from Dymocks online store. Recent results from modeling and observational studies. We are open, in-store and online.

Some orders may experience a slight delay due to COVID restrictions. Interhemispheric Water Exchange in the Atlantic Ocean Details The theme of this book is the inter-hemispheric and inter-gyre exchanges of heat, salt and fresh water, while its goal is to improve the knowledge of the tropical Atlantic dynamics and how it affects the global ocean.

The interhemispheric exchange of the warm water within the upper kilometer of the tropical Atlantic is the main theme of the excellent collection of research papers or chapters composing the book Interhemispheric Wa ter Exchange in the Atlantic Ocean edited by G. Goñi and Interhemispheric Water Exchange in the Atlantic Ocean.

We find that before the Industrial Revolution, deep water formed in the northern Atlantic Ocean carried about gigatonnes of carbon annually to the Southern Hemisphere, providing support for.

Located in the southeast Atlantic Ocean (° S, ° E, 4,m water depth), at the northern margin of the modern Antarctic Circumpolar Current (ACC), the core is ideally positioned to. In the two-layer circulation schemes presented by Stommel () and Gordon (), the setting up of the thermohaline circulation cell in the Atlantic Ocean is obtained through interhemispheric exchanges that are restricted to the western boundary.

Books in this series have a strong reference value, and vary from advanced level monographs to multi-author, edited volumes and university-level textbooks. Benefits for contributing to the series include: All publishing costs covered by Elsevier; 10% royalty rate to Editor/ lead Author; 30% discount on all Elsevier books.

This interhemispheric SST dipole indicates an inverse correlation between the AMO and South Atlantic SST, which can be physically explained by the ocean heat redistribution caused by changes in the Atlantic meridional overturning circulation (AMOC), and several studies have adopted the dipole as a proxy for AMOC variations (Latif et al a.

The import of relatively salty water masses from the Indian Ocean to the Atlantic is considered to be important for the operational mode of the Atlantic Meridional Overturning Circulation (AMOC). However, the occurrence and the origin of changes in this import behavior on millennial and glacial/interglacial timescales remains equivocal.

Describes the inter-hemispheric and inter-gyre exchanges of heat, salt, and fresh water. This book aims to improve the knowledge of the tropical Atlantic dynamics and how it affects the global ocean.

It uses output produced by regional models to complement the observations and to provide information on their spatial and temporal variability. between the wind-driven upwelling in the channel and deep-water formation at high northern latitudes.

Diapycnal mixing in the ocean interior can lead to warming and upwelling of deep waters. However, for parameters most representative of the present ocean mixing seems to play a. Rainer Zahn's 86 research works with 4, citations reads, including: Down-core sedimentary Sr-Nd isotope records from two Cape Basin sediment cores in the South Atlantic.

AbstractThis study presents a physical mechanism on how low-frequency variability of the South Atlantic meridional heat transport (SAMHT) may influence decadal variability of atmospheric circulatio. Abstract. A case is made that the Atlantic’s conveyor circulation carries roughly gigatons of carbon (as ΣCO 2) from the northern to the southern return transport of this carbon (as CO 2) through the atmosphere would maintain a ppm south to north gradient in atmospheric CO 2 content.

Such a gradient would go a long way toward explaining the current lower than expected. We find that the highest resolution climate model (∼10 km ocean, ∼50 km atmosphere) resolves Northwest Atlantic circulation and water mass distribution most accurately.

The CO 2 doubling response from this model shows that upper‐ocean (0– m) temperature in the Northwest Atlantic Shelf warms at a rate nearly twice as fast as the. Interhemispheric water exchange in the Atlantic Ocean edited by G.J. Goni and P. Malanotte-Rizzoli (Elsevier oceanography series, 68) Elsevier, alk.

paper. Figure 1: Agulhas leakage variability and interhemispheric climate change across the penultimate glacial-interglacial cycle.

(A) North Atlantic Ice Rafted Debris (IRD, black) from ODP site (Oppo et al. ) and tetraunsaturated alkenones (Cred) from MD (Martrat et al. ). (B, C) Seawater stable oxygen isotopes (δ 18 O SW) and sea surface temperatures (SST) from MDInterhemispheric Atlantic seesaw response during the last Vigorous exchange between the Indian and The Atlantic Ocean receives warm, saline water from the Indo-Pacific Ocean through.Today, the formation of North Atlantic Deep Water (NADW) transports heat to the Southern Ocean (34, 35), suggesting that past changes in NADW may have played an important role in the heat flux to Antarctic ice-sheet marine margins (36–38).