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  • Elsevier  (1)
  • Newark :American Geophysical Union,  (1)
  • 1
    Online Resource
    Online Resource
    Newark :American Geophysical Union,
    Keywords: Ocean circulation. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (217 pages)
    Edition: 1st ed.
    ISBN: 9781118847251
    Series Statement: Geophysical Monograph Series
    DDC: 551.46138
    Language: English
    Note: Intro -- The Mediterranean Sea: Temporal Variability and Spatial Patterns, Geophysical Monograph 202 -- Copyright -- Contents -- Contributors -- Preface -- 1 Introduction to The Mediterranean Sea: Temporal Variability and Spatial Patterns -- References -- 2 Spatiotemporal Variability of the Surface Circulation in the Western Mediterranean: A Comparative Study Using Altimetry and Modeling -- 2.1. Introduction -- 2.2. Data and Methods -- 2.2.1. Data -- 2.2.2. Methods -- 2.3. Results -- 2.3.1. Mean Surface Circulation -- 2.3.2. Eddy Kinetic Energy -- 2.3.3. Surface Circulation Variability Using EOFs -- 2.4. Summary and Discussion -- References -- 3 Exchange Flow through the Strait of Gibraltar as Simulated by a σ-Coordinate Hydrostatic Model and a z-Coordinate Nonhydrostatic Model -- 3.1. Introduction -- 3.2. Models Description and Initialization -- 3.2.1. POM -- 3.2.2. MITgcm -- 3.3. Models Validation -- 3.4. Results -- 3.4.1. Internal Bore Evolution -- 3.4.2. Three-layer definition and properties -- 3.4.3. Hydraulics -- 3.4.4. Sensitivity Experiments -- 3.5. Discussion and Conclusion -- References -- 4 Mixing in the Deep Waters of the Western Mediterranean -- 4.1. Introduction -- 4.2. Evolution of the Deep Waters -- 4.3. Mixing Estimates -- 4.4. Mixing Processes -- 4.5. Discussion -- References -- 5 The 2009 Surface and Intermediate Circulation of the Tyrrhenian Sea as Assessed by an Operational Model -- 5.1. Introduction -- 5.2. Model Description -- 5.2.1. The Numerical Model -- 5.2.2. Boundary Conditions and Hindcast Procedure -- 5.3. The Seasonal Variability of the Circulation During 2009 -- 5.3.1. The Surface Circulation -- 5.3.2. The Intermediate Circulation -- 5.4. Water Masses and Transports -- 5.5. Summary -- Appendix -- References -- 6 The Eastern Mediterranean Transient: Evidence for Similar Events Previously? -- 6.1. Introduction. , 6.2. Lessons from the Actual EMT -- 6.3. Historic T-S Signatures in Comparison with Potential Effects of EMT-Type Events -- 6.4. Discussion and Conclusion -- References -- 7 Deep-Water Variability and Interbasin Interactions in the Eastern Mediterranean Sea -- 7.1. Introduction -- 7.2. Methodology -- 7.3. Basinwide and Interbasin Variability -- 7.4. Intrabasin Variability -- 7.5. Simple Statistics -- 7.6. Discussion and Conclusions -- References -- 8 An Internal Mechanism Driving the Alternation of the Eastern Mediterranean Dense/Deep Water Sources -- 8.1. Introduction -- 8.2. Datasets and Model Description -- 8.2.1. Data Series -- 8.2.2. Model Description -- 8.2.3. Atmospheric Forcing -- 8.2.4. River Discharge Data -- 8.2.5. Boundary Conditions -- 8.2.6. Model Run -- 8.3. Results and Discussion -- 8.3.1. Evolution of the Hydrological Characteristics -- 8.3.2. Evolution of the Atmospheric Forcing -- 8.3.3. Salinity Lateral Redistribution -- 8.3.4. The Role of Lateral Advection -- 8.3.5. Flows through Straits-Salinity and Heat -- 8.4. Summary and Conclusions -- References -- 9 Thermohaline Variability and Mesoscale Dynamics Observed at the Deep-Ocean Observatory E2M3A in the Southern Adriatic Sea -- 9.1. Introduction -- 9.2. Datasets and Methods -- 9.3. Results -- 9.3.1. Thermohaline Variability in the Southern Adriatic between 2006 and 2010 -- 9.3.2. Heat and Salt Content Changes -- 9.3.3. Dense Water Formation Episodes Observed at the E2M3A Site -- 9.3.4. On the Relationship between Thermodynamic Forcing and Current Excitation: Identification of Eddylike Patterns -- 9.4. Conclusions -- References -- Index -- Supplemental Images.
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  • 2
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    Elsevier
    In:  Ocean Modelling, 7 (1-2). pp. 145-163.
    Publication Date: 2020-10-16
    Description: An idealized numerical model of the tropical Atlantic Ocean is used to study the structure, energetics and heat flux of the Atlantic tropical instability waves (TIWs). The model results compare well with the observations, and they both show that, unlike commonly assumed, the TIWs in the Atlantic exist on both sides of the equator and are generated not only in the summer but from May to January. Furthermore it is demonstrated that the Atlantic TIWs are generated by barotropic instability of the shear between the equatorial undercurrent and the northern south equatorial current and make a surprisingly small contribution to the heat budget of the equatorial mixed layer. The model results reveal that the often published strong meridional heat flux divergence of the TIWs is largely compensated for by their vertical heat flux divergence.
    Type: Article , PeerReviewed
    Format: text
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