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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
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    In:  EPIC3Frontiers in Marine Science, 3, ISSN: 2296-7745
    Publication Date: 2017-01-26
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
    Publication Date: 2022-10-26
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Owens, W., Zilberman, N., Johnson, K., Claustre, H., Scanderbeg, M., Wijffels, S., & Suga, T. OneArgo: a new paradigm for observing the global ocean. Marine Technology Society Journal, 56(3), (2022): 84–90, https://doi.org/10.4031/MTSJ.56.3.8.
    Description: OneArgo is a major expansion of the Argo program, which has provided two decades of transformative physical data for the upper 2 km of the global ocean. The present Argo array will be expanded in three ways: (1) Global Core: the existing upper ocean measurements will be extended to high latitudes and marginal seas and with enhanced coverage in the tropics and western boundaries of the major ocean basins; (2) Deep: deep ocean measurements will be obtained for the 50% of the global oceans that are below 2,000-m depth; and (3) Biogeochemical: dissolved oxygen, pH, nitrate, chlorophyll, optical backscatter, and irradiance data will be collected to investigate biogeochemical variability of the upper ocean and the processes by which these cycles respond to a changing climate. The technology and infrastructure necessary for this expansion is now being developed through large-scale regional pilots to further refine the floats and sensors and to demonstrate the utility of these measurements. Further innovation is expected to improve the performance of the floats and sensors and to develop the analyses necessary to provide research-quality data. A fully global OneArgo should be operational within 5–10 years.
    Description: In the United States, the National Science Foundation–funded Global Ocean Biogeochemistry Array (GO-BGC; https://go-bgc.org).
    Keywords: Argo floats ; Argo sensors ; OneArgo ; Climate change ; Biogeochemical measurements
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2022-05-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Wong, A. P. S., Wijffels, S. E., Riser, S. C., Pouliquen, S., Hosoda, S., Roemmich, D., Gilson, J., Johnson, G. C., Martini, K., Murphy, D. J., Scanderbeg, M., Bhaskar, T. V. S. U., Buck, J. J. H., Merceur, F., Carval, T., Maze, G., Cabanes, C., Andre, X., Poffa, N., Yashayaev, I., Barker, P. M., Guinehut, S., Belbeoch, M., Ignaszewski, M., Baringer, M. O., Schmid, C., Lyman, J. M., McTaggart, K. E., Purkey, S. G., Zilberman, N., Alkire, M. B., Swift, D., Owens, W. B., Jayne, S. R., Hersh, C., Robbins, P., West-Mack, D., Bahr, F., Yoshida, S., Sutton, P. J. H., Cancouet, R., Coatanoan, C., Dobbler, D., Juan, A. G., Gourrion, J., Kolodziejczyk, N., Bernard, V., Bourles, B., Claustre, H., D'Ortenzio, F., Le Reste, S., Le Traon, P., Rannou, J., Saout-Grit, C., Speich, S., Thierry, V., Verbrugge, N., Angel-Benavides, I. M., Klein, B., Notarstefano, G., Poulain, P., Velez-Belchi, P., Suga, T., Ando, K., Iwasaska, N., Kobayashi, T., Masuda, S., Oka, E., Sato, K., Nakamura, T., Sato, K., Takatsuki, Y., Yoshida, T., Cowley, R., Lovell, J. L., Oke, P. R., van Wijk, E. M., Carse, F., Donnelly, M., Gould, W. J., Gowers, K., King, B. A., Loch, S. G., Mowat, M., Turton, J., Rama Rao, E. P., Ravichandran, M., Freeland, H. J., Gaboury, I., Gilbert, D., Greenan, B. J. W., Ouellet, M., Ross, T., Tran, A., Dong, M., Liu, Z., Xu, J., Kang, K., Jo, H., Kim, S., & Park, H. Argo data 1999-2019: two million temperature-salinity profiles and subsurface velocity observations from a global array of profiling floats. Frontiers in Marine Science, 7, (2020): 700, doi:10.3389/fmars.2020.00700.
    Description: In the past two decades, the Argo Program has collected, processed, and distributed over two million vertical profiles of temperature and salinity from the upper two kilometers of the global ocean. A similar number of subsurface velocity observations near 1,000 dbar have also been collected. This paper recounts the history of the global Argo Program, from its aspiration arising out of the World Ocean Circulation Experiment, to the development and implementation of its instrumentation and telecommunication systems, and the various technical problems encountered. We describe the Argo data system and its quality control procedures, and the gradual changes in the vertical resolution and spatial coverage of Argo data from 1999 to 2019. The accuracies of the float data have been assessed by comparison with high-quality shipboard measurements, and are concluded to be 0.002°C for temperature, 2.4 dbar for pressure, and 0.01 PSS-78 for salinity, after delayed-mode adjustments. Finally, the challenges faced by the vision of an expanding Argo Program beyond 2020 are discussed.
    Description: AW, SR, and other scientists at the University of Washington (UW) were supported by the US Argo Program through the NOAA Grant NA15OAR4320063 to the Joint Institute for the Study of the Atmosphere and Ocean (JISAO) at the UW. SW and other scientists at the Woods Hole Oceanographic Institution (WHOI) were supported by the US Argo Program through the NOAA Grant NA19OAR4320074 (CINAR/WHOI Argo). The Scripps Institution of Oceanography's role in Argo was supported by the US Argo Program through the NOAA Grant NA15OAR4320071 (CIMEC). Euro-Argo scientists were supported by the Monitoring the Oceans and Climate Change with Argo (MOCCA) project, under the Grant Agreement EASME/EMFF/2015/1.2.1.1/SI2.709624 for the European Commission.
    Keywords: global ; ocean ; pressure ; temperature ; salinity ; Argo ; profiling ; floats
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 2022-07-15
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Roemmich, D., Talley, L., Zilberman, N., Osborne, E., Johnson, K., Barbero, L., Bittig, H., Briggs, N., Fassbender, A., Johnson, G., King, B., McDonagh, E., Purkey, S., Riser, S., Suga, T., Takeshita, Y., Thierry, V., & Wijffels, S. The technological, scientific, and sociological revolution of global subsurface ocean observing. Oceanography, 34(4), (2021): 2-8, https://doi.org/10.5670/oceanog.2021.supplement.02-02.
    Description: The complementary partnership of the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP; https://www.go-ship.org/) and the Argo Program (https://argo.ucsd.edu) has been instrumental in providing sustained subsurface observations of the global ocean for over two decades. Since the late twentieth century, new clues into the ocean’s role in Earth’s climate system have revealed a need for sustained global ocean observations (e.g., Gould et al., 2013; Schmitt, 2018) and stimulated revolutionary technology advances needed to address the societal mandate. Together, the international GO-SHIP and Argo Program responded to this need, providing insight into the mean state and variability of the physics, biology, and chemistry of the ocean that led to advancements in fundamental science and monitoring of the state of Earth's climate.
    Description: The authors gratefully acknowledge support from their respective Argo and GO-SHIP national programs or national agencies, which have made these programs possible.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 7
    Publication Date: 2022-01-31
    Description: The Argo Program has been implemented and sustained for almost two decades, as a global array of about 4000 profiling floats. Argo provides continuous observations of ocean temperature and salinity versus pressure, from the sea surface to 2000 dbar. The successful installation of the Argo array and its innovative data management system arose opportunistically from the combination of great scientific need and technological innovation. Through the data system, Argo provides fundamental physical observations with broad societally-valuable applications, built on the cost-efficient and robust technologies of autonomous profiling floats. Following recent advances in platform and sensor technologies, even greater opportunity exists now than 20 years ago to (i) improve Argo's global coverage and value beyond the original design, (ii) extend Argo to span the full ocean depth, (iii) add biogeochemical sensors for improved understanding of oceanic cycles of carbon, nutrients, and ecosystems, and (iv) consider experimental sensors that might be included in the future, for example to document the spatial and temporal patterns of ocean mixing. For Core Argo and each of these enhancements, the past, present, and future progression along a path from experimental deployments to regional pilot arrays to global implementation is described. The objective is to create a fully global, top-to-bottom, dynamically complete, and multidisciplinary Argo Program that will integrate seamlessly with satellite and with other in situ elements of the Global Ocean Observing System (Legler et al., 2015). The integrated system will deliver operational reanalysis and forecasting capability, and assessment of the state and variability of the climate system with respect to physical, biogeochemical, and ecosystems parameters. It will enable basic research of unprecedented breadth and magnitude, and a wealth of ocean-education and outreach opportunities.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 8
    Publication Date: 2024-02-07
    Description: The Earth climate system is out of energy balance, and heat has accumulated continuously over the past decades, warming the ocean, the land, the cryosphere, and the atmosphere. According to the Sixth Assessment Report by Working Group I of the Intergovernmental Panel on Climate Change, this planetary warming over multiple decades is human-driven and results in unprecedented and committed changes to the Earth system, with adverse impacts for ecosystems and human systems. The Earth heat inventory provides a measure of the Earth energy imbalance (EEI) and allows for quantifying how much heat has accumulated in the Earth system, as well as where the heat is stored. Here we show that the Earth system has continued to accumulate heat, with 381±61 ZJ accumulated from 1971 to 2020. This is equivalent to a heating rate (i.e., the EEI) of 0.48±0.1 W m−2. The majority, about 89 %, of this heat is stored in the ocean, followed by about 6 % on land, 1 % in the atmosphere, and about 4 % available for melting the cryosphere. Over the most recent period (2006–2020), the EEI amounts to 0.76±0.2 W m−2. The Earth energy imbalance is the most fundamental global climate indicator that the scientific community and the public can use as the measure of how well the world is doing in the task of bringing anthropogenic climate change under control. Moreover, this indicator is highly complementary to other established ones like global mean surface temperature as it represents a robust measure of the rate of climate change and its future commitment. We call for an implementation of the Earth energy imbalance into the Paris Agreement's Global Stocktake based on best available science. The Earth heat inventory in this study, updated from von Schuckmann et al. (2020), is underpinned by worldwide multidisciplinary collaboration and demonstrates the critical importance of concerted international efforts for climate change monitoring and community-based recommendations and we also call for urgently needed actions for enabling continuity, archiving, rescuing, and calibrating efforts to assure improved and long-term monitoring capacity of the global climate observing system. The data for the Earth heat inventory are publicly available, and more details are provided in Table 4.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    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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  • 10
    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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