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  • 1
    Call number: AWI A5-97-0059 ; MOP 17854
    Type of Medium: Monograph available for loan
    Pages: IX, 1334 S.
    Edition: 2nd print.
    Language: English
    Note: Table of Contents: COMPOSITION OF THE ATMOSPHERE. - The Composition of Atmospheric Air / by E. Glueckauf. - RADIATION. - Solar Radiant Energy and Its Modification by the Earth and Its Atmosphere / by Sigmund Fritz. - Long-Wave Radiation / by Fritz Möller. - Actinometric Measurements / by Anders Ångström. - METEOROLOGICAL OPTICS - General Meteorological Optics / by Hans Neuberger. - Polarization of Skylight / by Zdeněk Sekera. - Visibility in Meteorology / by W. E. Knowles Middleton. - ATMOSPHERIC ELECTRICITY. - Universal Aspects of Atmospheric Electricity / by O. H. Gish. - Ions in the Atmosphere / by G. R. Wait and W. D. Parkinson. - Precipitation Electricity / by Ross Gunn. - The Lightning Discharge / by J. H. Hagenguth. - Instruments and Methods for the Measurement of Atmospheric Electricity / by H. Israël. - Radioactivity of the Atmosphere / by H. Israël. - CLOUD PHYSICS. - On the Physics of Clouds and Precipitation / by Henry G. Houghton. - Nuclei of Atmospheric Condensation / by Christian Junge. - The Physics of Ice Clouds and Mixed Clouds / by F. H. Ludlam. - Thermodynamics of Clouds / by Fritz Möller. - The Formation of Ice Crystals / by Ukichiro Nakaya. - Snow and Its Relationship to Experimental Meteorology / by Vincent J. Schaefer. - Relation of Artificial Cloud-Modification to the Production of Precipitation / by Richard D. Coons and Ross Gunn. - THE UPPER ATMOSPHERE. - General Aspects of Upper Atmospheric Physics / by S. K. Mitra. - Photochemical Processes in the Upper Atmosphere and Resultant Composition / by Sidney Chapman. - Ozone in the Atmosphere by F. W. Paul Götz. - Radiative Temperature Changes in the Ozone Layer / by Richard A. Craig. - Temperatures and Pressures in the Upper Atmosphere / by Homer E. Newell, Jr. - Water Vapour in the Upper Air / by G. M. B. Dobson and A. W. Brewer. - Diffusion in the Upper Atmosphere / by Heinz Lettau. - The Ionosphere / by S. L. Seaton. - Night-Sky Radiations from the Upper Atmosphere / by E. O. Hulburt. - Aurorae and Magnetic Storms / by L. Harang. - Meteors as Probes of the Upper Atmosphere / by Fred L. Whipple. - Sound Propagation in the Atmosphere / by B. Gutenberg. - COSMICAL METEOROLOGY. - Solar Energy Variations As a Possible Cause of Anomalous Weather Changes / by Richard A. Craig and H. C. Willett. - The Atmospheres of the Other Planets / by S. L. Hess and H. A. Panofsky. - DYNAMICS OF THE ATMOSPHERE. - The Perturbation Equations in Meteorology / by B. Haurwitz. - The Solution of Nonlinear Meteorological Problems by the Method of Characteristics / by John C. Freeman. - Hydrodynamic Instability / by Jacques M. Van Mieghem. - Stability Properties of Large-Scale Atmospheric Disturbances / by R. Fjørtoft. - The Quantitative Theory of Cyclone Development / by E. T. Eady. - Dynamic Forecasting by Numerical Process / by J. G. Charney. - Energy Equations / by James E. Miller. - Atmospheric Turbulence and Diffusion / by O. G. Sutton. - Atmospheric Tides and Oscillations / by Sydney Chapman. - Application of the Thermodynamics of Open Systems to Meteorology / by Jacques M. Van Mieghem. - THE GENERAL CIRCULATION. - The Physical Basis for the General Circulation / by Victor P. Starr. - Observational Studies of General Circulation Patterns / by Jerome Namias and Philip F. Clapp. - Applications of Energy Principles to the General Circulation / by Victor P. Starr. - MECHANICS OF PRESSURE SYSTEMS. - Extratropical Cyclones / by J. Bjerknes. - The Aerology of Extratropical Disturbances / by E. Palmén. - Anticyclones / by H. Wexler. - Mechanism of Pressure Change / by James M. Austin. - Large-Scale Vertical Velocity and Divergence / by H. A. Panofsky. - The Instability Line / by J. R. Fulks. - LOCAL CIRCULATIONS. - Local Winds / by Friedrich Defant. - Tornadoes and Related Phenomena / by Edward M. Brooks. - Thunderstorms / by Horace R. Byers. - Cumulus Convection and Entrainment / by James M. Austin. - OBSERVATIONS AND ANALYSIS. - World Weather Network / by Athelstan F. Spilhaus. - Models and Techniques of Synoptic Representation / by John C. Bellamy. - Meteorological Analysis in the Middle Latitudes / by V. J. Oliver and M. B. Oliver. - WEATHER FORECASTING. - The Forecast Problem / by H. C. Willett. - Short-Range Weather Forecasting / by Gordon E. Dunn. - A Procedure of Short-Range Weather Forecasting / by Robert C. Bundgaard. - Objective Weather Forecasting / by R. A. Allen and E. M. Vernon. - General Aspects of Extended-Range Forecasting / by Jerome Namias. - Extended-Range Weather Forecasting / by Franz Baur. - Extended-Range Forecasting by Weather Types / by Robert D. Elliott. - Verification of Weather Forecasts / by Glenn W. Brier and Roger A. Allen. - Application of Statistical Methods to Weather Forecasting / by George P. Wadsworth. - TROPICAL METEOROLOGY. - Tropical Meteorology / by C. E. Palmer. - Equatorial Meteorology / by A. Grimes. - Tropical Cyclones / by Gordon E. Dunn. - Aerology of Tropical Storms / by Herbert Riehl. - POLAR METEOROLOGY. - Antarctic Atmospheric Circulation / by Arnold Court. - Arctic Meteorology / by Herbert G. Dorsey, Jr. - Some Climatological Problems of the Arctic and Sub-Arctic / by F. Kenneth Hare. - CLIMATOLOGY. - Climate - The Synthesis of Weather / by C. S. Durst. - Applied Climatology / by Helmut E. Landsberg and Woodrow C. Jacobs. - Microclimatology / by Rudolf Geiger. - Geological and Historical Aspects of Climatic Change / by C. E. P. Brooks. - Climatic Implications of Glacier Research / by Richard Foster Flint. - Tree-Ring Indices of Rainfall, Temperature, and River Flow / by Edmund Schulman. - HYDROMETEOROLOGY. - Hydrometeorology in the United States / by Robert D. Fletcher. - The Hydrologic Cycle and Its Relation to Meteorology - River Forecasting / by Ray K. Linsley. - MARINE METEOROLOGY. - Large-Scale Aspects of Energy Transformation over the Oceans / by Woodrow C. Jacobs. - Evaporation from the Oceans / by H. U. Sverdrup. - Forecasting Ocean Waves / by W. H. Munk and R. S. Arthur. - Ocean Waves as a Meteorological Tool / by W. H. Munk. - BIOLOGICAL AND CHEMICAL METEOROLOGY. - Aerobiology / by Woodrow C. Jacobs. - Physical Aspects of Human Bioclimatology / by Konrad J. K. Buettner. - Some Problems of Atmospheric Chemistry / by H. Cauer. - ATMOSPHERIC POLLUTION. - Atmospheric Pollution / by E. Wendell Hewson. - CLOUDS, FOG, AND AIRCRAFT ICING. - The Classification of Cloud Forms / by Wallace E. Howell. - The Use of Clouds in Forecasting / by Charles F. Brooks. - Fog / by Joseph J. George. - Physical and Operational Aspects of Aircraft Icing / by Lewis A. Rodert. - Meteorological Aspects of Aircraft Icing / by William Lewis. - METEOROLOGICAL INSTRUMENTS. - Instruments and Techniques for Meteorological Measurements / by Michael Ference, Jr. - Aircraft Meteorological Instruments / by Alan C. Bemis. - LABORATORY INVESTIGATIONS. - Experimental Analogies to Atmospheric Motions / by Dave Fultz. - Model Techniques in Meteorological Research / by Hunter Rouse. - Experimental Cloud Formation / by Sir David Brunt. - RADIOMETEOROLOGY. - Radar Storm Observation / by Myron G. H. Ligda. - Theory and Observation of Radar Storm Detection / by Raymond Wexler. - Meteorological Aspects of Propagation Problems / by H. G. Booker. - Sferics / by R. C. Wanta. - MICROSEISMS. - Observations and Theory of Microseisms / by B. Gutenberg. - Practical Application of Microseisms to Forecasting / by James B. Macelwane, S. J. CORRIGENDA. - INDEX.
    Location: AWI Reading room
    Location: MOP - must be ordered
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 48 (1947), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Planetary and Space Science 5 (1961), S. 92-98 
    ISSN: 0032-0633
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Planetary and Space Science 5 (1961), S. 196-201 
    ISSN: 0032-0633
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 44 (1943), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 213 (1967), S. 9-13 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Lunar tides in the oceans are familiar and easy to observe. Lunar tides in the atmosphere also exist, although their recognition is more ...
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 77 (1969), S. 122-150 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The global distribution of the lunar barometric tideL 2 is investigated by spherical harmonic analysis, based on 104 stations for the annual mean, and on 85 stations for the three seasons. The main wave ofL 2 is the one with wave number 2, but for a detailed study of the irregularities of the global distribution ofL 2, waves with other wave numbers have also to be considered. Even the main wave ofL 2 is asymmetric to the equator with the two lunar-daily pressure maxima occurring earlier in the Southern than in the Northern Hemisphere. The amplitudes at the same distances from the equator are greater in the Southern than in the Northern Hemisphere. These hemispheric differences are most pronounced during the D season. As found in earlier investigations the phase consiant ofL 2 is always greater during the J season than during the D season. But the amplitudes are greatest during the J season only north of 30oS. Farther south the amplitude maximum occurs during the D season.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 102 (1973), S. 193-222 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The global distributions of the annual and seasonal means of the diurnal (S 1) and semidiurnal (S 2) surface pressure oscillations are investigated by spherical harmonic analysis. The main waves are,S 1 1 (with wave number 1) forS 1 andS 2 2 forS 2.S 1 1 is much less predominant among the waves ofS 1 thanS 2 2 among those ofS 2. As in the case of the lunar semidiurnal barometric tideL 2 the pressure maxima occur earlier in the Southern than in the Northern Hemisphere. In the case ofS 2 the standing waveS 2 0 and the waveS 2 3 are also of interest besidesS 2 2. Although the present analysis extends only from 60°N to 60°S, whileS 2 0 is largest at polar latitudes, its results show thatS 2 0 should be smaller at high southerly than at high northerly latitudes, as has been observed. Thus this observed asymmetrical distribution ofS 2 0 may be due to causes outside the polar regions rather than to their geographical differences. The best approximation to the observed distribution ofS 2 0 is obtained by including a mode representing an oscillation independent of longitude and latitude indicating a small semidiurnal variation of the mean global surface presure, which is an unlikely result on physical grounds. The seasonal variation ofS 1 1 expressed in percent of the annual mean is smaller than that ofS 2 2, and both are less than the unexplained seasonal variation ofL 2 2. The main wavesS 1 1 andS 2 2 are expressed not only by associated Legendre functions, but also by Hough functions.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 4 (1951), S. 73-86 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Es ist häufig beobachtet worden, daß zwei tropische Zyklonen sich entgegen dem Uhrzeigersinne umeinander bewegen. Eine theoretische Erklärung dieser Bewegung kann gegeben werden auf Grund der Annahme, daß sich jedes Zyklonenzentrum unter dem Einfluß des Windfeldes der anderen Zyklone bewegt; auf Grund dieser Theorie läßt sich die Rotationsgeschwindigkeit des Zyklonenpaares berechnen. An Hand von neun Fällen mit genügend zuverlässigem und vollständigem Beobachtungsmaterial wird gezeigt, daß gute Übereinstimmung zwischen Theorie und Beobachtung besteht.
    Abstract: Résumé On a souvent observé que deux cyclones tropicaux se meuvent l'un par rapport à l'autre dans le sens inverse des aiguilles d'une montre. On peut expliquer le fait en admettant que chaque centre cyclonique se déplace sous l'influence du champ de vent de l'autre. Grâce à cette hypothèse on peut calculer la vitesse de rotation de la paire de cyclones. Neuf exemples richement documentés montrent un bon accord entre la théorie et l'observation.
    Notes: Summary When two tropical cyclones are present simultaneously in the same region they show as a rule a counterclockwise rotation around each other. A theoretical explanation of this motion is given. The theory permits the computation of the rate of rotation. A discussion of nine examples with sufficiently reliable and complete observational data gives a satisfactory agreement between theoretical and observed rates of rotation.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 10 (1957), S. 29-42 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Für sechzehn Stationen in hohen Breiten sind die Amplituden und Phasen der halbtägigen Luftdruckwelle berechnet worden, und die Resultate wurden verwendet, um ein Bild über die geographischen und jahreszeitlichen Variationen dieser Oszillation in hohen Breiten zu erhalten. An den meisten Stationen hat die Amplitude ein Maximum während der Äquinoktien und ein Minimum im Sommer. Für die Phase wurde keine ausgeprägte jahreszeitliche Schwankung gefunden; allerdings scheint es, daß an Stationen nördlich von 70° N Breite das Maximum am spätesten im Sommer und am frühesten im Winter eintritt. Für die geographische Verteilung des Jahresmittels der stehenden halbtägigen Luftdruckschwankung in hohen Breiten wird eine einfache Formel gegeben.
    Abstract: Résumé On a calculé les amplitudes et les phases de l'onde barométrique semi-diurne pour 16 stations de hautes latitudes. Avec les résultats de ces calculs, on obtient des indications sur les variations géographiques et saisonnières de cette oscillation aux latitudes élevées. A la plupart des stations, l'amplitude montre un maximum pendant les équinoxes et un minimum en été; on n'a pas décelé de variation saisonnière marquée de la phase; pourtant il semble qu'aux stations situées au nord de 70° de latitude nord, le maximum apparaît au plus tard en été et au plus tôt en hiver. On donne une formule simple pour la distribution géographique de la moyenne annuelle de l'oscillation barométrique semi-diurne stationnaire aux hautes latitudes.
    Notes: Abstract The amplitudes and phases of the semidiurnal pressure wave have been computed for sixteen high-latitude stations. The data were analyzed to obtain a picture of the geographical and seasonal variations of this oscillation at high latitudes. At most of the stations the seasonal variation of the amplitude was found to have a maximum during the equinoxes and a minimum in the summer. No definite seasonal variation was found for the phase, although a tendency was found at stations above 70° N for the latest phase to occur in summer and an earliest phase to occur in winter. A simple expression is given for the geographical distribution of the annual mean of the standing semidiurnal oscillation at high latitudes.
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