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  • 1
    Keywords: Ocean circulation Atlantic Ocean ; Ocean-atmosphere interaction Atlantic Ocean ; Ocean circulation Atlantic Ocean ; Ocean-atmosphere interaction Atlantic Ocean ; Aufsatzsammlung ; Atlantischer Ozean ; Meeresströmung ; Atmosphäre
    Type of Medium: Book
    Pages: XV, 506 S. , Ill., graph. Darst.
    ISBN: 0444512675
    Series Statement: Elsevier oceanography series 68
    DDC: 551.46213
    RVK:
    Language: English
    Note: Includes bibliographical references and index
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  • 2
    Online Resource
    Online Resource
    Oxford :Elsevier Science & Technology,
    Keywords: Ocean circulation - Atlantic Ocean. ; Electronic books.
    Description / Table of Contents: Recent results from modeling and observational studies demonstrate that the tropical Atlantic is a critical region for processes that maintain the meridional overturning circulation, such as cross-equatorial exchanges, and for sea surface temperature variability that impacts on climate variability of the coupled tropical ocean/atmosphere system. 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. A clear understanding of the dynamics of processes that affect the flow of mass and heat between the southern and the northern hemispheres in the upper few hundred meters in the tropical Atlantic and of those associated to the ocean circulation or to surface signals, from decadal, inter-annual to mesoscale periods, becomes necessary to better evaluate their contribution to the interhemispheric mass exchange. These processes are believed to be largely responsible in driving the sea surface temperature, which in turn, is a critical parameter to investigate ocean-atmospheric interactions. Output produced by regional models is also used to complement the observations and to provide additional information on their spatial and temporal variability. The subtropical cells, by bringing water masses subducted in the subtropics to the equator, and zonal currents investigated here contribute to the interhemispheric water exchange. Special attention is also given to the warm and salty anticyclonic rings shed by the North Brazil Current, which are now known to have a much broader impact, not only on interhemispheric water mass transfer, but also on the environment of remote regions. Observations from different sources are blended together, are used to validate model outputs and are also assimilated into
    Type of Medium: Online Resource
    Pages: 1 online resource (523 pages)
    Edition: 1st ed.
    ISBN: 9780080534893
    Series Statement: Issn Series ; v.Volume 68
    DDC: 551.46/213
    Language: English
    Note: Front Cover -- INTERHEMISPHERIC WATER EXCHANGE IN THE ATLANTIC OCEAN -- Copyright Page -- CONTENTS -- Preface -- Chapter 1. Circulation, variability and near-equatorial meridional flow in the central tropical Atlantic -- 1. Introduction -- 2. Methods and data -- 3. The water masses -- 4. Results -- 5. Discussion -- Chapter 2. Comparison of hydrographic and altimeter based estimates of sea level height variability in the Atlantic Ocean -- 1.Introduction -- 2. Data and methods -- 3. Analysis -- 4. Discussion -- 5. Summary -- Chapter 3. Estimation of the tropical Atlantic circulation from altimetry data using a reduced-rank stationary Kalman filter -- 1. Introduction -- 2. Model of the tropical Atlantic -- 3. Approach for assimilating SHA -- 4. Identical twin assimilation experiment -- 5. Assimilation of the TOPEX/Poseidon SHA -- 6. Summary and conclusions -- Appendix: Derivation of reduced-rank Kalman filter -- Chapter 4. A synthetic float analysis of upper-limb meridional overturning circulation interior ocean pathways in the tropical/subtropical Atlantic -- 1. Introduction -- 2. Background and goals -- 3. Analysis procedures -- 4. Eulerian Analysis -- 5. Lagrangian analysis -- 6. Case study and mechanisms -- 7. Discussion -- Appendix 1: Diagnosis of vertical velocity -- Appendix 2: Spatial interpolation of model variables to floats -- Appendix 3: Float advection -- Chapter 5. A seasonal and interannual study of the western equatorial Atlantic upper thermocline circulation variability -- 1. Introduction -- 2. Estimates of current velocity from SSH slopes and curvatures -- 3. Data -- 4. Data proessing -- 5. Comparison of in situ data and altimeter-derived fields -- 6. Analysis of the circulation fields -- 7. Inter-hemispheric transports and transport pathways -- 8. Summary and conclusions. , Appendix: Preparation of band-limited circulatoin and transport fields -- Chapter 6. Fate of the equatorial undercurrent in the Atlantic -- 1. Introduction -- 2. Model and data handling -- 3. Results -- 4. Summary and conclusions -- Chapter 7. The flow of AAIW along the equator -- 1. Introduction -- 2. The model configuration -- 3. Synthesis of theory and observations -- 4. Summary -- Chapter 8. Planetary equatorial trapped waves in the Atlantic Ocean from TOPEX/Poseidon altimetry -- 1. Introduction -- 2. Sea height and sea surface temperature data -- 3. Equatorially Trapped Modes -- 4. Results -- 5. Discussion -- 6. Summary and conclusions -- Chapter 9. Pathways and variability at intermediate depths in the tropical Atlantic -- 1. Introduction -- 2. Data and methods -- 3. Large scale flow patterns -- 4. Temporal and spatial variability between 5°S and 7°S -- 5. Discussion and conclusions -- Chapter 10. A comparison of kinematic evidence for tropical cells in the Atlantic and Pacific oceans -- 1. Introduction -- 2. Data and analyses -- 3. Results -- 4. Discusion -- Chapter 11. Subtropical cells in the Atlantic Ocean: An observational summary -- 1. Introduction -- 2. Subduction -- 3. Pathways between the subduction regions and the upwelling regions -- 4. Upwelling in the tropical Atlantic -- 5. Near surface return flow to the subduction areas -- 6. Summary and remaining questions -- Chapter 12. Spectral, formal, and nonlinear stability in a layered quasigeostrophic model with application to the Atlantic North Equatorial Current -- 1. Introduction -- 2. Theory -- 3. Data -- 4. Summary and conclusions -- Appendix A: Energy and Casimir matrices -- Appendix B: Dispersion relatio -- Appendix C: Eigenvalue problem in ψ fcoordinates -- Chapter 13. Synoptic study of warm rings in the North Brazil Current retroflection region using satellite altimetry. , 1. Introduction -- 2. Region of study -- 3. Data -- 4. Two-layer model approximation -- 5. Results and discussion -- 6. Summary -- Chapter 14. North Brazil Current rings and the variability in the latitude of the retroflection -- 1. Introduction -- 2. Methodology -- 3. Dynamic height field -- 4. Latitude of penetration and number of rings shed -- 5. Rings volume and temperature transport -- 6. Summary -- Chapter 15. North Brazil Current rings and transport of southern waters in a high resolution numerical simulation of the North Atlantic -- 1. Introduction -- 2. Model configuration -- 3. The North Brazil Current system from the model and observations: The seasonal circulation -- 4. The North Brazil rings, sea surface height variability and effect on transports through the Lesser Antilles passages -- 5. Transport of southern Atlantic waters by rings -- 6. Discussion and conclusions -- Chapter 16. Cross-gyre transport by North Brazil Current rings -- 1. Introduction -- 2. Data and Methods -- 3. Results -- 4. Discussion and conclusions -- Chapter 17. Impact of North Brazil Current rings on the local circulation and coral reef fish recruitment to Barbados, West Indies -- 1. Introduction -- 2. Methods -- 3. Results -- 4. Discussion -- Chapter 18. Wind bursts and enhanced evaporation in the tropical and subtropical Atlantic Ocean -- 1. Introduction and background -- 2. Result -- 3. Concluding remarks -- Chapter 19. Spatial-temporal evolution of the low frequency climate variability in the tropical Atlantic -- 1. Introduction -- 2. Data and processing -- 3. Results -- 4. Conclusions -- Index.
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics Letters A 153 (1991), S. 181-185 
    ISSN: 0375-9601
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Wave Motion 14 (1991), S. 93-99 
    ISSN: 0165-2125
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-02-08
    Description: The Atlantic Meridional Overturning Circulation (AMOC) is a key mechanism of heat, freshwater, and carbon redistribution in the climate system. The precept that the AMOC has changed abruptly in the past, notably during and at the end of the last ice age, and that it is “very likely” to weaken in the coming century due to anthropogenic climate change is a key motivation for sustained observations of the AMOC. This paper reviews the methodology and technology used to observe the AMOC and assesses these ideas and systems for accuracy, shortcomings, potential improvements, and sustainability. We review hydrographic techniques and look at how these traditional techniques can meet modern requirements. Transport mooring arrays (TMAs) provide the “gold standard” for sustained AMOC observing, utilizing dynamic height, current meter, and other instrumentation and techniques to produce continuous observations of the AMOC. We consider the principle of these systems and how they can be sustained and improved into the future. Techniques utilizing indirect measurements, such as satellite altimetry, coupled with in situ measurements, such as the Argo float array, are also discussed. Existing technologies that perhaps have not been fully exploited for estimating AMOC are reviewed and considered for this purpose. Technology is constantly evolving, and we look to the future of technology and how it can be deployed for sustained and expanded AMOC measurements. Finally, all of these methodologies and technologies are considered with a view to a sustained and sustainable future for AMOC observation.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 6
    Publication Date: 2014-08-06
    Description: Focal adhesion kinase (FAK) is a nonreceptor tyrosine kinase (NRTK) with key roles in integrating growth and cell matrix adhesion signals, and FAK is a major driver of invasion and metastasis in cancer. Cell adhesion via integrin receptors is well known to trigger FAK signaling, and many of the players...
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Publication Date: 2020-07-08
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-07-05
    Description: XBT has been proven to be an invaluable tool in the measurement of temperature in the upper layers of the ocean. The effortlessness and low cost of XBT-based surveys has made possible the build-up of an impressive dataset used for inferring dynamic properties such as dynamic height, geostrophic velocity, and sound speed. However, for the proper estimation of such properties, the corresponding salinity fields are also required. Due to the inherent difficulty of in-situ measurements, the salinity can be estimated from XBT data based on the close relationship that exists between temperature and salinity in most of the ocean’s waters. The salinity field can be also estimated by objective analysis based in coarse in-situ observations or by data assimilation techniques, combining numerical observations and models. In recent years, with the increasing power of computers and the availability of immense amounts of data, the use of Neural Networks has been increasingly used to solve complex problems. An effort is underway to develop a Machine Learning (ML) model for the estimation of salinity along temperature profiles measured by XBTs. The preliminary results of a model using a stack of fully connected neural networks are promising. Using data from the AX18 and AX08 lines in the South Atlantic, it is found that when the input variables include the XBT location (longitude and latitude) and the depths, the accuracy is considerably increased as compared with when only temperature is used. In the sequence, the model will also incorporate remotely sensed surface properties.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
    Publication Date: 2023-07-06
    Description: The South Atlantic Meridional Overturning Circulation (SAMOC) observing system has evolved tremendously since 2007, and has substantially improved our understanding of the dynamics and variability of the upper, deep, and abyssal South Atlantic circulation from daily to interannual time-scales. However, the SAMOC daily time series derived from moored arrays are still relatively short and are only available at 11°S and 34.5°S. To expand the SAMOC time series in space and time, we derived monthly zonal trans-basin temperature (T) and salinity (S) sections since 1993 at four latitudes (20°S, 25°S, 30°S, and 34.5°S) based on historical relationships between T, S, and satellite sea level. The resulting meridional overturning circulation (MOC) and meridional heat transport (MHT) estimates at 20°S, 25°S, and 30°S are significantly correlated with each other at near zero lag, however correlations with the estimates at 34.5°S are somewhat lower. Although the overturning contribution dominates changes in the MHT at all four latitudes, the gyre contribution increases southward, reaching 30% of the explained MHT variability at 34.5°S. These 30-year monthly records indicate that the dominant mechanism controlling the MOC/MHT variability alternates between wind forcing and internal ocean dynamics. Therefore, both mechanisms must be monitored to fully capture changes in the MOC/MHT. These estimates demonstrate a linkage between the tropical Pacific forcing and heat content changes in the subtropical South Atlantic, as well as the impact of the MOC/MHT on extreme weather events, and provide context for measurements obtained from the SAMOC moored arrays.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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