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  • 1
    Electronic Resource
    Electronic Resource
    The anticyclonic eddies just south of jet stream (1952)
    Springer
    Meteorology and atmospheric physics 5 (1952), S. 1-4 
    Details
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die Bedeutung der hydrodynamischen Instabilität für die Bildung antizyklonaler Wirbel direkt südlich des westlichen Freistrahlstromes in mittleren Breiten wird dargelegt. Ferner macht der Verfasser auf seine früheren Untersuchungen von 1941 über dynamische Instabilität aufmerksam.
    Abstract: Résumé L'auteur montre l'importance de l'instabilité hydrodynamique pour la formation de tourbillons anticycloniques immédiatement au Sud du courant d'Ouest (jet stream) aux latitudes moyennes. Il rappelle ensuite ses précédentes recherches de 1941 sur l'instabilité dynamique.
    Notes: Summary The importance of the hydrodynamic instability for the formation of anticyclonic eddies just south of westerly jet stream in the middle latitudes is pointed out. Finally, the author would like to call attention for his earlier works on dynamic instability in 1941.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02247254
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  • 2
    Electronic Resource
    Electronic Resource
    Rossby-Haurwitz's equation for the conservation of vertical vorticity component in the baroclinic atmosphere (1950)
    Springer
    Pure and applied geophysics 18 (1950), S. 158-159 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary It is shown that the conservation equation of potential vorticity in the barotropic atmosphere $$\frac{d}{{dt}}\left( {\frac{{f + \zeta }}{{\Delta p}}} \right) = 0$$ holds good, even in the baroclinic atmosphere, if it is permissible to introduce the isentropic and mass-conservation approximations.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02000320
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  • 3
    Electronic Resource
    Electronic Resource
    Phugoid motion of whirlwinds in the atmosphere (1952)
    Springer
    Pure and applied geophysics 22 (1952), S. 171-173 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The movements of whirlwinds are discussed along the line of the phugoid theory, and it is concluded that the path of whirlwinds has the shape of a trochoid.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01989635
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  • 4
    Electronic Resource
    Electronic Resource
    Intrinsic equations of motion in dynamical meteorology (1951)
    Springer
    Pure and applied geophysics 20 (1951), S. 50-55 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Tangential and normal equations of horizontal motion along and normal to the characteristic lines (for example: stream lines, isobars, isotherms, etc.) are derived in general form. Then the later section of this paper is devoted to applications to natural coordinates and the coordinates chosen to lie parallel and normal to the isobars.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01996892
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  • 5
    Electronic Resource
    Electronic Resource
    The criterion of dynamic stability of zonal motion including the vertical shear (1951)
    Springer
    Pure and applied geophysics 20 (1951), S. 56-61 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Many writers treated on the problem of dynamic instability of westerly flow due to the excessive horizontal shear, and the present author discusses the corresponding dynamic instability due to the vertical shear. The critical vertical shear in indifferent stratification is given by the condition — the meridional component of absolute vorticity vanishes, — and is an approximate negative valueof 10−4 sec −1 in middle latitude. However the critical vertical shear in normal stable stratification is a fairly large negative value of 2 sec−1. It might be emphasized that the problem of this study differs fromRichardson's criterion of turbulence, for the present author discusses the condition under which the zonal flow is dynamically stable, whileRichardson expressed the condition under which the turbulence will decrease.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01996893
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  • 6
    Electronic Resource
    Electronic Resource
    Zonal wind-profile between the pole and the equator given by a single expression (1952)
    Springer
    Meteorology and atmospheric physics 5 (1952), S. 129-135 
    Details
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Der Mechanismus der Erhaltung der mittleren zonalen Zirkulation der Atmosphäre wird unter dem Gesichtspunkt der Übertragung und der Neubildung der Wirbelstärke (vorticity) durch atmosphärische Störungen diskutiert. Die zur Analyse benützte Methode ist ähnlich dem vonA. Ångström angegebenen Verfahren, das eine einfache Erklärung für die mittlere Temperaturverteilung über die Erdoberfläche bietet. Die mittleren jährlichen zonalen Winde werden über die ganze Erde durch einen einzigen Ausdruck wiedergegeben, während die vonRossby, Kasahara undKuo angegebenen zonalen Windverteilungen für die Polarregion und das Tropengebiet getrennt berechnet sind. Die hier berechnete allgemeine Tendenz der Breitenvariation der zonalen Winde stimmt mit den Beobachtungen recht gut überein.
    Abstract: Résumé On examine le mécanisme de l'entretien, de la circulation zonale moyenne de l'atmosphère du point de vue du transfert et de la régénération de la force tourbillonnaire (vorticity) par des perturbations atmosphériques. La méthode d'analyse utilisée est analogue au procédé indiqué parA. Ångström qui fournit une explication simple de la distribution moyenne de la température à la surface du globe. Une seule formule exprime les vents zonaux moyens annuels sur toute la terre, tandis que l'on calcule séparément les répartitions zonales des régions polaire et tropicale données parRossby, Kasahara etKuo. La tendance générale de variation des vents zonaux selon la latitude est en accord satisfaisant avec les faits observés.
    Notes: Abstract The mechanism of the maintenance of the mean zonal circulation of the atmosphere is discussed from the point of view of vorticity transfer and vorticity generation by atmospheric disturbance. The method of analysis used is quite similar with that given byA. Ångström which offers a simple explanation for the mean temperature distribution over the surface of the earth. The annual mean zonal winds over the earth are expressed in a single expression, whereas the zonal wind distribution given byRossby, Kasahara andKuo have all been given for the polar cap and the tropical region separately. The general trends of the latitude variation of the zonal winds computed here fit the observations quite well.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02246481
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  • 7
    Electronic Resource
    Electronic Resource
    Baroclinicy along some meridional cross sections through the atmosphere (1953)
    Springer
    Meteorology and atmospheric physics 6 (1953), S. 53-58 
    Details
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Im Hinblick auf die Bedeutung der Baroklinie für die Dynamik der allgemeinen Zirkulation der Atmosphäre werden die Intensitäten des Solenoidfeldes längs den vonHess angegebenen mittleren Meridionalschnitten durch die Atmosphäre wie auch die Barokline längsPalméns speziellem Meridionalschnitt berechnet, tabelliert und erläutert.
    Abstract: Résumé Vu l'importance du baroclinisme atmosphérique dans la dynamique de la circulation générale, on a calculé l'intensité du champ de solénoïdes le long des profils méridiens moyens établis parHess, ainsi que le long du profil méridien particulier donné parPalmén avec reproduction en tableaux et figures.
    Notes: Abstract In view of the importance of baroclinicy for the dynamics of the general circulation of the atmosphere, the intensity of solenoidal field alongHess' mean meridional cross sections through the atmosphere as well as the baroclinicy alongPalmén's individual meridional cross section through the atmosphere are computed, tabulated and illustrated.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02248851
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  • 8
    Electronic Resource
    Electronic Resource
    Fujiwhara on five centuries of freezing dates of Lake Suwa in the Central Japan (1954)
    Springer
    Theoretical and applied climatology 6 (1954), S. 152-166 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung Die Gefriertermine des Suwa-Sees in Mitteljapan werden als phänologische Indikatoren in chronologischer Reihe über mehr als fünf Jahrhunderte, vom Winter 1443/44 bis heute, mitgeteilt. Die letzten 2 1/2 Jahrhunderte sind durch späteres Zufrieren, also wärmere Winter charakterisiert, wenn sich auch deutliche Fluktuationen zwischen kalt und warm erkennen lassen. Außerdem wird auf Jahresringen der Bäume beruhendes Beweismaterial diskutiert.
    Abstract: Résumé L'auteur dispose en tableau chronologique les dates de gel du lac Suwa (Japon central) pour plus de 500 ans, soit depuis l'hiver 1443–44 jusqu'à aujourd'huit et qui peuvent servir d'indicateurs phénologiques. Les années des dernières 2 1/2 siècles sont caractérisées par des hivers plus chauds (gels plus tardifs), malgré des fluctuations définies de périodes chaudes et froides. Pour appuyer ces constations, l'auteur examine aussi les résultats obtenus par l'analyse des cernes des arbres.
    Notes: Summary As phenological indicators, the freezing dates of Lake Suwa in the Central Japan are tabulated in chronological order over more than five centuries since the winter 1443/44 up to the present. The years in the last 2 1/2 centuries have been characterized by warmer winter (i. e. later freezing), even though there is a definite sequence of fluctuation between cold and warm. Tree-rings analysis is also given for references.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02246747
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  • 9
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    Identification of errors in the electron density measurements of a tangential interferometer/polarimeter system during a tokamak discharge (2012)
    American Institute of Physics
    Details
    Publication Date: 2012-10-01
    Print ISSN: 0034-6748
    Electronic ISSN: 1089-7623
    Topics: Electrical Engineering, Measurement and Control Technology , Physics
    Published by American Institute of Physics
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  • 10
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    Observation of Quasi-Two-Dimensional Nonlinear Interactions in a Drift-Wave Streamer (2010)
    American Physical Society
    Details
    Publication Date: 2010-11-23
    Print ISSN: 0031-9007
    Electronic ISSN: 1079-7114
    Topics: Physics
    Published by American Physical Society
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