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  • Springer  (2)
  • Tokyo :Springer Japan,  (1)
  • 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
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In order to understand long-term changes in the temperature structure of the upper western North Pacific, we compared thermal conditions in two pentads, 1938–42 (P34) and 1978–82 (P78). The 1938–42 data were taken mostly by the Japanese Imperial Navy in a series of hydrographic surveys. The 1978–82 data were mostly XBT data taken as part of the TRANSPAC program. For each pentad, the data were interpolated to a set of standard depths, put through quality control procedures and averaged on a 1o×1o grid. A large area of the central subtropical gyre was warmer during P78, while the southern subtropical gyre, in the area of the North Equatorial Current was warmer during P34. This suggests that the transports of the Kuroshio and North Equatorial currents were larger during P78. Properties of North Pacific subtropical mode water (NPSTMW) were compared between pentads. It was found that NPSTMW was thicker, more uniform in temperature and more confined geographically during P34. A greater thickness is shown to result from stronger wintertime cooling during P34. Changes in the geographic extent of NPSTMW probably result from reduced advection by the Kuroshio current system during P34. The reason for the reduced advection maybe the Kuroshio was in a large meander state for a larger fraction of the earlier pentad, which can cut off advection west of the Izu Ridge.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 51 (1995), S. 1-19 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The distribution and characteristics of Subtropical Mode Water (STMW) south of Honshu, the main island of Japan, were investigated using CTD, XBT, and dissolved oxygen data taken by the research vessels in the spring of 1988 and 1989. A comparatively low inventory of STMW was shown in spring 1988 during the large-meander period of the Kuroshio south of Honshu, while in spring 1989 during the non-large-meander period, the observation showed a considerable inventory of STMW which had outcropped east of 140°E in the preceding winter. These observations, together with published temperature maps, surface current charts, time series of vertical temperature profiles along 140°E, and wintertime Monsoon Index consistently support the climatology of the STMW circulation recently presented by the authors. That is, the change of the Kuroshio Countercurrent associated with the large meander of the Kuroshio most likely cuts off the westward/southwestward advection of STMW from its formation area east of 140°E.
    Type of Medium: Electronic Resource
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