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  • 1
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (180 pages)
    Edition: 1st ed.
    ISBN: 9784431560531
    DDC: 551.5246
    Language: English
    Note: Intro -- Preface -- Contents -- 1 Oceanic fronts and jets around Japan: a review -- Abstract -- 1Oceanic fronts and their roles in climate -- 2A table of metrics -- 2.1 The dynamical properties of oceanic fronts -- 2.2 The metric table -- 3Kuroshio fronts -- 3.1 Kuroshio Extension front (KE front) -- 3.1.1 Metrics used to locate the KE front -- 3.1.2 The KE front and its impact on the atmosphere -- 3.2 Kuroshio south of Japan -- 3.3 Kuroshio along the shelf break of the East China Sea -- 3.4 Comparison to the Gulf Stream, Agulhas Current, and Antarctic Circumpolar Current -- 4Kuroshio-Oyashio confluence region -- 5Fronts in the subtropical North Pacific -- 5.1 Northern, Southern, and Eastern subtropical fronts -- 5.2 Hawaiian Lee Countercurrent -- 6Fronts in coastal and marginal seas -- 6.1 Tidal fronts of the Seto Inland Sea -- 6.2 Japan Sea subpolar front -- 7Summary and concluding remarks -- Acknowledgments -- Appendix -- Kuroshio Extension -- Kuroshio south of Japan -- Kuroshio along the shelf break of the East China Sea -- Gulf Stream -- Agulhas Current and Agulhas Return Current -- Antarctic Circumpolar Current-Subantarctic front (ACC-SAF) -- Kuroshio-Oyashio confluence region -- Northern, Southern, and Eastern Subtropical fronts (NSTF, SSTF, and ESTF) -- Hawaiian Lee Countercurrent -- Seto Inland Sea tidal front -- Japan Sea subpolar front -- FRA-JCOPE2 -- References -- 2 Climatological mean features and interannual to decadal variability of ring formations in the Kuroshio Extension region -- Abstract -- 1Introduction -- 2Data and methods -- 2.1 Datasets -- 2.2 Method for detecting a ring formation -- 3Climatological mean features -- 4Interannual to decadal variability -- 5Summary and discussion -- Acknowledgments -- References. , 3 Marine atmospheric boundary layer and low-level cloud responses to the Kuroshio Extension front in the early summer of 2012: three-vessel simultaneous observations and numerical simulations -- Abstract -- 1Introduction -- 2Intensive observation campaign -- 3Three-vessel simultaneous observation -- 3.1 Weather condition -- 3.2 Cloud base height -- 3.3 Downward longwave radiation and water vapor -- 4Model experiments -- 4.1 Experiment design -- 4.2 Simulation results -- 5Summary -- Acknowledgments -- Appendix: Simulations by the AR-WRF -- References -- 4 Heat and salt budgets of the mixed layer around the Subarctic Front of the North Pacific Ocean -- Abstract -- 1Introduction -- 2Data -- 3Method -- 3.1 Heat budget -- 3.2 Salinity budget -- 4Results -- 4.1 OML spatial distribution and properties -- 4.2 Seasonal cycle of the heat budget -- 4.2.1 Budget averaged in a large domain and spatial distribution -- 4.2.2 Budget comparison between north and south of the SAF -- 4.3 Salinity budget seasonal cycle -- 4.4 Temperature and salinity contributions to buoyancy loss -- 5Conclusion -- Acknowledgments -- References -- 5 Impact of downward heat penetration below the shallow seasonal thermocline on the sea surface temperature -- Abstract -- 1Introduction -- 2Data and methods -- 3Heat penetration depth in the subsurface layer -- 3.1 Relationship between Qnet and rate of change of HC in the vertical dimension -- 3.2 Definition of heat penetration depth -- 4Results -- 4.1 Seasonal changes in surface and subsurface temperatures -- 4.2 Relationship between Qnet_m and d(HCm)/dt and the role of the subsurface layer -- 4.3 Relationship between Qnet_m and d(HCm)/dt throughout the North Pacific Ocean -- 5Summary and discussion -- Acknowledgments -- Appendices -- Appendix 1: Monthly horizontal 5° × 5° gridded Argo profiles. , Appendix 2: Horizontal heat transport by Ekman transport and the geostrophic current and their relative importance to the downward Qnet in the North Pacific -- Appendix 3: Seasonal changes in temperature and HPD from Argo float data -- Appendix 4: Relationship between Qnet and dHC/dt based on OAFlux -- References -- 6 Early summertime interannual variability in surface and subsurface temperature in the North Pacific -- Abstract -- 1Introduction -- 2Observational data and model -- 2.1 MOAA-GPV -- 2.2 North Pacific OFES -- 3Results -- 3.1 Observed variability -- 3.2 Simulated variability -- 4Discussion -- 4.1 Possible mechanism -- 4.2 Possibility of air-sea interactions -- 4.3 Horizontal distribution of SST and SSS difference -- 5Summary -- Acknowledgments -- References -- 7 Local wind effect on the Kuroshio path state off the southeastern coast of Kyushu -- Abstract -- 1Introduction -- 2Observational evidence -- 2.1 Data and processing -- 2.1.1 Kuroshio path position data from MIRC -- 2.1.2 Sea surface geostrophic velocity and wind stress fields -- 2.2 Results of data analyses -- 2.2.1 Time series of Kuroshio small meander events 1982-2011 -- 2.2.2 Monthly mean fields of sea surface geostrophic velocity and wind stress -- 3Theoretical considerations -- 3.1 Method to approach the small meander formation process -- 3.2 Dynamics in the surface Ekman layer -- 3.3 Response of the jet to Ekman pumping: a two-layer quasi-geostrophic model -- 3.4 Small meander formation process: an approach from the path equation -- 4Numerical experiments -- 4.1 Model description and experiment design -- 4.2 Results of numerical experiments -- 5Conclusions and discussion -- Acknowledgments -- Appendix -- Method used to derive the sea surface geostrophic velocity dataset -- References. , 8 Unusually rapid intensification of Typhoon Man-yi in 2013 under preexisting warm-water conditions near the Kuroshio front south of Japan -- Abstract -- Sec1 -- 2Storm overview, data used, and the model -- 2.1 Overview of Typhoon Man-yi (2013) -- 2.1.1 History -- 2.1.2 Satellite observations -- 2.2 Data -- 2.3 Model -- 2.3.1 Atmosphere model -- 2.3.2 Ocean surface-wave model -- 2.3.3 Multilayer ocean model -- 2.3.4 Model topography -- 2.3.5 Exchange processes -- 2.4 Experimental design -- 3Results -- 3.1 Sea surface temperature -- 3.2 Results of simulated track, intensity and structural change of a storm -- 3.2.1 Track and intensity -- 3.2.2 Mesovortex and rapid intensification -- 3.2.3 Axisymmetric inner-core structure of Man-yi -- 3.2.4 Rapid intensification, preexisting oceanic conditions, and sea surface cooling -- 3.3 Torrential rainfall -- 4Discussion -- 4.1 Atmospheric and oceanic boundary layers and air-sea interactions -- 4.2 Poleward shift of the location of maximum intensity -- 4.3 Atmospheric environment -- 5Conclusions -- Acknowledgements -- References -- 9 Atlantic-Pacific asymmetry of subsurface temperature change and frontal response of the Antarctic Circumpolar Current for the recent three decades -- Abstract -- 1Introduction -- 2Data and method -- 3Results -- 3.1 Trends of temperature and inter-basin asymmetry in the subsurface layer -- 3.2 Patterns of meridional shift of the ACC and temperature change -- 4Discussion -- 4.1 Mechanism of the meridional shift of ACC -- 4.2 Changes in wind system and SST gradient -- 5Summary and conclusions -- Acknowledgments -- Appendix: Climatological fronts of OFES -- References.
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  • 2
    Keywords: Earth sciences ; Earth Sciences ; Climatology ; Oceanography ; Atmospheric sciences ; Earth sciences ; Climatology ; Oceanography ; Atmospheric sciences
    Description / Table of Contents: Oceanic fronts and jets around Japan: a review -- Climatological mean features and interannual to decadal variability of ring formations in the Kuroshio Extension region -- Marine atmospheric boundary layer and low-level cloud responses to the Kuroshio Extension front in the early summer of 2012: three-vessel simultaneous observations and numerical simulations -- Heat and salt budgets of the mixed layer around the Subarctic Front of the North Pacific Ocean -- Impact of downward heat penetration below the shallow seasonal thermocline on the sea surface temperature -- Early summertime interannual variability in surface and subsurface temperature in the North Pacific -- Local wind effect on the Kuroshio path state off the southeastern coast of Kyushu -- Unusually rapid intensification of Typhoon Man-yi in 2013 under pre-existing warm-water conditions near the Kuroshio front south of Japan -- Atlantic–Pacific asymmetry of subsurface temperature change and frontal response of the Antarctic Circumpolar Current for the recent three decades.
    Type of Medium: Online Resource
    Pages: Online-Ressource (XIV, 170 p. 130 illus., 105 illus. in color, online resource)
    Edition: 1st ed. 2016
    ISBN: 9784431560531
    Series Statement: SpringerLink
    Language: English
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  • 3
    Publication Date: 2024-02-07
    Description: Two decades of high-resolution satellite observations and climate modeling studies have indicated strong ocean–atmosphere coupled feedback mediated by ocean mesoscale processes, including semipermanent and meandrous SST fronts, mesoscale eddies, and filaments. The air–sea exchanges in latent heat, sensible heat, momentum, and carbon dioxide associated with this so-called mesoscale air–sea interaction are robust near the major western boundary currents, Southern Ocean fronts, and equatorial and coastal upwelling zones, but they are also ubiquitous over the global oceans wherever ocean mesoscale processes are active. Current theories, informed by rapidly advancing observational and modeling capabilities, have established the importance of mesoscale and frontal-scale air–sea interaction processes for understanding large-scale ocean circulation, biogeochemistry, and weather and climate variability. However, numerous challenges remain to accurately diagnose, observe, and simulate mesoscale air–sea interaction to quantify its impacts on large-scale processes. This article provides a comprehensive review of key aspects pertinent to mesoscale air–sea interaction, synthesizes current understanding with remaining gaps and uncertainties, and provides recommendations on theoretical, observational, and modeling strategies for future air–sea interaction research.
    Type: Article , PeerReviewed
    Format: text
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  • 4
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    ELSEVIER SCIENCE BV
    In:  EPIC3Dynamics of Atmospheres and Oceans, ELSEVIER SCIENCE BV, 50(1), pp. 55-77, ISSN: 0377-0265
    Publication Date: 2018-12-07
    Description: A semi-analytical model of the Panama throughflow is presented. The model expresses the throughflow transport as a function of deep water formation in the North Pacific and in the North Atlantic, and of the Panama Gateway depth. The model is derived from the integral of the momentum equation along a circumpolar path, and can be interpreted from the point of view of the vorticity balance. The important conditions are whether the deep water, whose location is considered to be above the bottom water formed around Antarctica, originates from the North Atlantic or from the North Pacific, and whether the Panama Gateway is shallower than the lower boundary of the deep water. The present model indicates that the barotropic transport through the Panama Gateway is eastward, except for the case where the deep water is formed in the North Pacific and the sill of the Panama Gateway is shallow. The baroclinic structure of the Panama throughflow depends on whether the deep water is formed in the North Pacific or in the North Atlantic. These qualitative implications of the model are consistent with recent numerical studies and proxy-based paleoceanographic studies. Numerical experiments performed in the present study reinforce confidence in the semi-analytical model.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
    Publication Date: 2018-12-07
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 6
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2012. 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 117 (2012): C02017, doi:10.1029/2011JC007369.
    Description: The upper ocean heat content variability in the East/Japan Sea was investigated using a 40 year temperature and salinity data set from 1968 to 2007. Decadal variability was identified as the dominant mode of variability in the upper ocean (0–300 m) aside from the seasonal cycle. The decadal variability is strong to the west of northern Honshu, west of the Tsugaru Strait, and west of southern Hokkaido. Temperature anomalies at 50–125 m exhibit a large contribution to the decadal variability, particularly in the eastern part of the East/Japan Sea. The vertical structure of regressed temperature anomalies and the spatial patterns of regressed 10°C isotherms in the East/Japan Sea suggest that the decadal variability is related to upper ocean circulation in the East/Japan Sea. The decadal variability also exhibits an increasing trend, which indicates that the regions showing large decadal variations experienced warming on decadal time scales. Further analysis shows that the decadal variability in the East/Japan Sea is not locally isolated but is related to variability in the northwestern Pacific.
    Description: This work was supported by grants from the Ministry of Land, Transport, and Maritime Affairs, Korea (Ocean Climate Variability Program and EAST-I Project).
    Description: 2012-08-09
    Keywords: East/Japan Sea ; Decadal variability ; Heat content ; Northwestern Pacific
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 7
    Publication Date: 2022-10-26
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Ponte, R. M., Carson, M., Cirano, M., Domingues, C. M., Jevrejeva, S., Marcos, M., Mitchum, G., van de Wal, R. S. W., Woodworth, P. L., Ablain, M., Ardhuin, F., Ballu, V., Becker, M., Benveniste, J., Birol, F., Bradshaw, E., Cazenave, A., De Mey-Fremaux, P., Durand, F., Ezer, T., Fu, L., Fukumori, I., Gordon, K., Gravelle, M., Griffies, S. M., Han, W., Hibbert, A., Hughes, C. W., Idier, D., Kourafalou, V. H., Little, C. M., Matthews, A., Melet, A., Merrifield, M., Meyssignac, B., Minobe, S., Penduff, T., Picot, N., Piecuch, C., Ray, R. D., Rickards, L., Santamaria-Gomez, A., Stammer, D., Staneva, J., Testut, L., Thompson, K., Thompson, P., Vignudelli, S., Williams, J., Williams, S. D. P., Woppelmann, G., Zanna, L., & Zhang, X. Towards comprehensive observing and modeling systems for monitoring and predicting regional to coastal sea level. Frontiers in Marine Science, 6, (2019): 437, doi:10.3389/fmars.2019.00437.
    Description: A major challenge for managing impacts and implementing effective mitigation measures and adaptation strategies for coastal zones affected by future sea level (SL) rise is our limited capacity to predict SL change at the coast on relevant spatial and temporal scales. Predicting coastal SL requires the ability to monitor and simulate a multitude of physical processes affecting SL, from local effects of wind waves and river runoff to remote influences of the large-scale ocean circulation on the coast. Here we assess our current understanding of the causes of coastal SL variability on monthly to multi-decadal timescales, including geodetic, oceanographic and atmospheric aspects of the problem, and review available observing systems informing on coastal SL. We also review the ability of existing models and data assimilation systems to estimate coastal SL variations and of atmosphere-ocean global coupled models and related regional downscaling efforts to project future SL changes. We discuss (1) observational gaps and uncertainties, and priorities for the development of an optimal and integrated coastal SL observing system, (2) strategies for advancing model capabilities in forecasting short-term processes and projecting long-term changes affecting coastal SL, and (3) possible future developments of sea level services enabling better connection of scientists and user communities and facilitating assessment and decision making for adaptation to future coastal SL change.
    Description: RP was funded by NASA grant NNH16CT00C. CD was supported by the Australian Research Council (FT130101532 and DP 160103130), the Scientific Committee on Oceanic Research (SCOR) Working Group 148, funded by national SCOR committees and a grant to SCOR from the U.S. National Science Foundation (Grant OCE-1546580), and the Intergovernmental Oceanographic Commission of UNESCO/International Oceanographic Data and Information Exchange (IOC/IODE) IQuOD Steering Group. SJ was supported by the Natural Environmental Research Council under Grant Agreement No. NE/P01517/1 and by the EPSRC NEWTON Fund Sustainable Deltas Programme, Grant Number EP/R024537/1. RvdW received funding from NWO, Grant 866.13.001. WH was supported by NASA (NNX17AI63G and NNX17AH25G). CL was supported by NASA Grant NNH16CT01C. This work is a contribution to the PIRATE project funded by CNES (to TP). PT was supported by the NOAA Research Global Ocean Monitoring and Observing Program through its sponsorship of UHSLC (NA16NMF4320058). JS was supported by EU contract 730030 (call H2020-EO-2016, “CEASELESS”). JW was supported by EU Horizon 2020 Grant 633211, Atlantos.
    Keywords: Coastal sea level ; Sea-level trends ; Coastal ocean modeling ; Coastal impacts ; Coastal adaptation ; Observational gaps ; Integrated observing system
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    Publication Date: 2022-10-26
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Stammer, D., Bracco, A., AchutaRao, K., Beal, L., Bindoff, N. L., Braconnot, P., Cai, W., Chen, D., Collins, M., Danabasoglu, G., Dewitte, B., Farneti, R., Fox-Kemper, B., Fyfe, J., Griffies, S. M., Jayne, S. R., Lazar, A., Lengaigne, M., Lin, X., Marsland, S., Minobe, S., Monteiro, P. M. S., Robinson, W., Roxy, M. K., Rykaczewski, R. R., Speich, S., Smith, I. J., Solomon, A., Storto, A., Takahashi, K., Toniazzo, T., & Vialard, J. Ocean climate observing requirements in support of climate research and climate information. Frontiers in Marine Science, 6, (2019): 444, doi:10.3389/fmars.2019.00444.
    Description: Natural variability and change of the Earth’s climate have significant global societal impacts. With its large heat and carbon capacity and relatively slow dynamics, the ocean plays an integral role in climate, and provides an important source of predictability at seasonal and longer timescales. In addition, the ocean provides the slowly evolving lower boundary to the atmosphere, driving, and modifying atmospheric weather. Understanding and monitoring ocean climate variability and change, to constrain and initialize models as well as identify model biases for improved climate hindcasting and prediction, requires a scale-sensitive, and long-term observing system. A climate observing system has requirements that significantly differ from, and sometimes are orthogonal to, those of other applications. In general terms, they can be summarized by the simultaneous need for both large spatial and long temporal coverage, and by the accuracy and stability required for detecting the local climate signals. This paper reviews the requirements of a climate observing system in terms of space and time scales, and revisits the question of which parameters such a system should encompass to meet future strategic goals of the World Climate Research Program (WCRP), with emphasis on ocean and sea-ice covered areas. It considers global as well as regional aspects that should be accounted for in designing observing systems in individual basins. Furthermore, the paper discusses which data-driven products are required to meet WCRP research and modeling needs, and ways to obtain them through data synthesis and assimilation approaches. Finally, it addresses the need for scientific capacity building and international collaboration in support of the collection of high-quality measurements over the large spatial scales and long time-scales required for climate research, bridging the scientific rational to the required resources for implementation.
    Description: This work was partly supported by the DFG funded excellence center CliSAP of the Universituat Hamburg (DS). AB was supported by the National Science Foundation through award NSF-1658174 and by the NOAA through award NA16OAR4310173. SM was supported by the Earth Systems and Climate Change Hub of the Australian Government’s National Environmental Science Program.
    Keywords: Ocean observing system ; Ocean climate ; Earth observations ; In situ measurements ; Satellite observations ; Ocean modeling ; Climate information
    Repository Name: Woods Hole Open Access Server
    Type: Article
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