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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: 2022-05-26
    Description: Author Posting. © American Meteorological Society, 2010. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Climate 23 (2010): 3249-3281, doi:10.1175/2010JCLI3343.1.
    Description: Ocean–atmosphere interaction over the Northern Hemisphere western boundary current (WBC) regions (i.e., the Gulf Stream, Kuroshio, Oyashio, and their extensions) is reviewed with an emphasis on their role in basin-scale climate variability. SST anomalies exhibit considerable variance on interannual to decadal time scales in these regions. Low-frequency SST variability is primarily driven by basin-scale wind stress curl variability via the oceanic Rossby wave adjustment of the gyre-scale circulation that modulates the latitude and strength of the WBC-related oceanic fronts. Rectification of the variability by mesoscale eddies, reemergence of the anomalies from the preceding winter, and tropical remote forcing also play important roles in driving and maintaining the low-frequency variability in these regions. In the Gulf Stream region, interaction with the deep western boundary current also likely influences the low-frequency variability. Surface heat fluxes damp the low-frequency SST anomalies over the WBC regions; thus, heat fluxes originate with heat anomalies in the ocean and have the potential to drive the overlying atmospheric circulation. While recent observational studies demonstrate a local atmospheric boundary layer response to WBC changes, the latter’s influence on the large-scale atmospheric circulation is still unclear. Nevertheless, heat and moisture fluxes from the WBCs into the atmosphere influence the mean state of the atmospheric circulation, including anchoring the latitude of the storm tracks to the WBCs. Furthermore, many climate models suggest that the large-scale atmospheric response to SST anomalies driven by ocean dynamics in WBC regions can be important in generating decadal climate variability. As a step toward bridging climate model results and observations, the degree of realism of the WBC in current climate model simulations is assessed. Finally, outstanding issues concerning ocean–atmosphere interaction in WBC regions and its impact on climate variability are discussed.
    Description: Funding for LT was provided by the NASA-sponsored Ocean Surface Topography Science Team, under Contract 1267196 with the University of Washington, administered by the Jet Propulsion Laboratory. HN was supported in part by the Grant-in-Aid 18204044 by the Japan Society for Promotion for Science (JSPS) and the Global Environment Research Fund (S-5) of the Japanese Ministry of Environment. YK was supported by the Kerr Endowed Fund and Penzance Endowed Fund.
    Keywords: Currents ; Sea surface temperature ; Anomalies ; Large-scale motions ; Oceanic mixed layer ; Northern Hemisphere
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature Climate Change 2 (2012): 161-166, doi:10.1038/nclimate1353.
    Description: Subtropical western boundary currents are warm, fast flowing currents that form on the western side of ocean basins. They carry warm tropical water to the mid-latitudes and vent large amounts of heat and moisture to the atmosphere along their paths, affecting atmospheric jet streams and mid-latitude storms, as well as ocean carbon uptake. The possibility that these highly energetic and nonlinear currents might change under greenhouse gas forcing has raised significant concerns, but detecting such changes is challenging owing to limited observations. Here, using reconstructed sea surface temperature datasets and newly developed century-long ocean and atmosphere reanalysis products, we find that the post-1900 surface ocean warming rate over the path of these currents is two to three times faster than the global mean surface ocean warming rate. The accelerated warming is associated with a synchronous poleward shift and/or intensification of global subtropical western boundary currents in conjunction with a systematic change in winds over both hemispheres. This enhanced warming may reduce ocean's ability to absorb anthropogenic carbon dioxide over these regions. However, uncertainties in detection and attribution of these warming trends remain, pointing to a need for a long-term monitoring network of the global western boundary currents and their extensions.
    Description: This work is supported by China National Key Basic Research Project (2007CB411800) and National Natural Science Foundation Projects (40788002, 40921004). WC is supported by the Australian Climate Change Science program and the Southeast Australia Climate Initiative. HN is supported in part by the Japanese Ministry of Education, Culture, Sports, Science and Technology through Grant-in-Aid for Scientific Research on Innovative Areas #2205 and by the Japanese Ministry of Environment through Global Environment Research Fund (S-5). MJM is supported by NOAA’s Climate Program Office.
    Description: 2012-07-29
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 5
    Publication Date: 2023-02-16
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Yamamoto, A., Nonaka, M., Martineau, P., Yamazaki, A., Kwon, Y.-O., Nakamura, H., & Taguchi, B. Oceanic moisture sources contributing to wintertime Euro-Atlantic blocking. Weather and Climate Dynamics, 2(3), (2021): 819–840, https://doi.org/10.5194/wcd-2-819-2021.
    Description: Although conventionally attributed to dry dynamics, increasing evidence points to a key role of moist dynamics in the formation and maintenance of blocking events. The source of moisture crucial for these processes, however, remains elusive. In this study, we identify the moisture sources responsible for latent heating associated with the wintertime Euro-Atlantic blocking events detected over 31 years (1979–2010). To this end, we track atmospheric particles backward in time from the blocking centres for a period of 10 d using an offline Lagrangian dispersion model applied to atmospheric reanalysis data. The analysis reveals that 28 %–55 % of particles gain heat and moisture from the ocean over the course of 10 d, with higher percentages for the lower altitudes from which particles are released. Via large-scale ascent, these moist particles transport low-potential-vorticity (PV) air of low-altitude, low-latitude origins into the upper troposphere, where the amplitude of blocking is the most prominent, in agreement with previous studies. The PV of these moist particles remains significantly lower compared to their dry counterparts throughout the course of 10 d, preferentially constituting blocking cores. Further analysis reveals that approximately two-thirds of the moist particles source their moisture locally from the Atlantic, while the remaining one-third of moist particles source it from the Pacific. There is also a small fraction of moist particles that take up moisture from both the Pacific and Atlantic basins, which undergo a large-scale uplift over the Atlantic using moisture picked up over both basins. The Gulf Stream and Kuroshio and their extensions as well as the eastern Pacific northeast of Hawaii not only provide heat and moisture to moist particles but also act as “springboards” for their large-scale, cross-isentropic ascent, where its extent strongly depends on the humidity content at the time of the ascent. While the particles of Atlantic origin swiftly ascend just before their arrival at blocking, those of Pacific origin begin their ascent a few days earlier, after which they carry low-PV air in the upper troposphere while undergoing radiative cooling just as dry particles. A previous study identified a blocking maintenance mechanism, whereby low-PV air is selectively absorbed into blocking systems to prolong blocking lifetime. As they used an isentropic trajectory analysis, this mechanism was regarded as a dry process. We found that these moist particles that are fuelled over the Pacific can also act to maintain blocks in the same manner, revealing that what appears to be a blocking maintenance mechanism governed by dry dynamics alone can, in fact, be of moist origin.
    Description: This research has been supported by the Japan Society for the Promotion of Science (JSPS) (grant nos. JP19H05701, JP19H05702, JP19H05703, JP19H05704 on Innovative Areas 6102, and JP20H01970), the Japan Science and Technology Agency through Belmont Forum CRA “InterDec” and COI-NEXT (grant no. JPMJPF2013), the Japanese Ministry of Environment through the Environment Research and Technology Development Fund (grant no. JPMEERF20192004), the Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT) through the Arctic Challenge for Sustainability (ArCS and ARCS II; grant nos. JPMXD1300000000 and JPMXD1420318865) programmes, the Japanese Ministry of Environment through the Environment Research and Technology Development Fund (grant no. 2-1904), the US NSF Climate & Large Scale Dynamics Program (grant no. AGS-2040073), and the US DOE CESD Regional and Gloabal Model Analysis programme (grant no. DE-SC0019492). Patrick Martineau was partly supported by Grant-in-Aid for JSPS Research Fellows.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Now that the mouse and human genome sequences are complete, biologists need systematic approaches to determine the function of each gene. A powerful way to discover gene function is to determine the consequence of mutations in living organisms. Large-scale production of mouse mutations with the ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Development genes and evolution 205 (1996), S. 300-310 
    ISSN: 1432-041X
    Keywords: Xenopus laevis HGF gene promoter ; CAT fusion gene ; Temporally and spatially controlled expression ; Silencer elements ; Mesoderm induction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Previously, we isolated Xenopus HGF (hepatocyte growth factor) cDNA and showed in Xenopus embryos that expression of this gene starts at the late gastrula stage mainly in the ventral mesoderm, and furthermore that the expression is induced in animal cap by activin A and bFGF (basic fibroblast growth factor). Here we have cloned the Xenopus HGF gene, covering a 14 kb 5′-upstream region and a 0.2 kb 5′-coding region. Within about 0.5 kb of the 5′-flanking region, the Xenopus HGF gene contained a TATA-like element AATGAAA, one putative NF-1 binding site, two NF-IL-6 binding motif sequences, one putative TGF-β-dependent inhibitory element (TIE) and one AP-1 binding site. A recombinant circular plasmid consisting of a 1.7 kb HGF promoter region and the bacterial chloramphenicol acetyltransferase (CAT) gene was first expressed at the late gastrula stage in the ventral mesoderm, as was the endogenous HGF gene. The expression of the fusion gene was induced in animal cap cells by activin A and bFGF although induction by the latter was not so strong. Using a series of 5′-deletion constructs introduced into animal caps, silencer elements, which seem to be essential for the gene's regionally correct expression, and the element responsible for induction by activin were found. The results show that the HGF gene promoter isolated here contains elements which may endow the gene with the regulative function for its temporally and spatially regulated expression, although the element necessary for induction by bFGF seems to be missing.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2019-09-23
    Description: Subtropical western boundary currents are warm, fast-flowing currents that form on the western side of ocean basins. They carry warm tropical water to the mid-latitudes and vent large amounts of heat and moisture to the atmosphere along their paths, affecting atmospheric jet streams and mid-latitude storms, as well as ocean carbon uptake1, 2, 3, 4. The possibility that these highly energetic currents might change under greenhouse-gas forcing has raised significant concerns5, 6, 7, but detecting such changes is challenging owing to limited observations. Here, using reconstructed sea surface temperature datasets and century-long ocean and atmosphere reanalysis products, we find that the post-1900 surface ocean warming rate over the path of these currents is two to three times faster than the global mean surface ocean warming rate. The accelerated warming is associated with a synchronous poleward shift and/or intensification of global subtropical western boundary currents in conjunction with a systematic change in winds over both hemispheres. This enhanced warming may reduce the ability of the oceans to absorb anthropogenic carbon dioxide over these regions. However, uncertainties in detection and attribution of these warming trends remain, pointing to a need for a long-term monitoring network of the global western boundary currents and their extensions.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 9
    Publication Date: 2022-01-31
    Description: The individual impact of North Atlantic and Pacific Ocean Western Boundary Currents (OWBCs) on the tropospheric circulation has recently been studied in depth. However, their simultaneous role in shaping the hemisphere-scale wintertime troposphere/stratosphere-coupled circulation and its variability have not been considered. Through semi-idealized Atmospheric General-Circulation-Model experiments, we show that the North Atlantic and Pacific OWBCs jointly maintain and shape the wintertime hemispheric circulation and its leading mode of variability Northern Annular Mode (NAM). The OWBCs energize baroclinic waves that reinforce quasi-annular hemispheric structure in the tropospheric eddy-driven jetstreams and NAM variability. Without the OWBCs, the wintertime NAM variability is much weaker and its impact on the continental and maritime surface climate is largely insignificant. Atmospheric energy redistribution caused by the OWBCs acts to damp the near-surface atmospheric baroclinicity and compensates the associated oceanic meridional energy transport. Furthermore, the OWBCs substantially weaken the wintertime stratospheric polar vortex by enhancing the upward planetary wave propagation, and thereby affecting both stratospheric and tropospheric NAM-annularity. Whereas the overall impact of the extra-tropical OWBCs on the stratosphere results mainly from the Pacific, the impact on the troposphere results from both the Pacific and Atlantic OWBCs.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 10
    Publication Date: 2016-07-31
    Description: Gynecologic cancer is one of the most common malignant diseases in working-age women. This study investigated whether several characteristics influence return to work after treatment of gynecologic cancer.
    Electronic ISSN: 1471-2407
    Topics: Medicine
    Published by BioMed Central
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