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  • Springer  (28,612)
  • Wiley-Blackwell  (6,063)
  • Oxford University Press  (1,722)
  • Cambridge University Press  (906)
  • 1980-1984
  • 1955-1959  (37,303)
  • 1959  (19,546)
  • 1958  (17,757)
Collection
Years
  • 1980-1984
  • 1955-1959  (37,303)
Year
  • 1
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 89-93 
    ISSN: 0950-5636
    Source: Cambridge Journals Digital Archives
    Topics: History , Natural Sciences in General
    Notes: The word “classification” is used here in its sense of “the result of classifying” rather than the action of so doing. Since the resulting classification has special reference to the subject-matter of science as a whole, it is natural to turn to the scientific literature of various periods for an indication of how this classification has been developed. For sake of comparison, reference may be made to one of the modern systems of library classification. In the Dewey Decimal System the numbers 550 to 559 are allotted to Geology and 560 to 569 to Palaeontology. By placing numbers to the right of the decimal point, further sub-divisions may be made, for example, 560·942 is classed as Palaeon-tology of England. Thus a number is available for every reasonable demand of classification. The present purpose is to trace the natural evolution of the various branches of science, in contrast to the mechanical process of providing a classification of scientific literature for ease of reference. An example may make this distinction clearer.
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  • 2
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 96-96 
    ISSN: 0950-5636
    Source: Cambridge Journals Digital Archives
    Topics: History , Natural Sciences in General
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  • 3
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 1-1 
    ISSN: 0950-5636
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  • 4
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 95-95 
    ISSN: 0950-5636
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    Topics: History , Natural Sciences in General
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  • 5
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 94-94 
    ISSN: 0950-5636
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    Topics: History , Natural Sciences in General
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  • 6
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 95-96 
    ISSN: 0950-5636
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  • 7
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    Cambridge : Cambridge University Press
    Bulletin of the British Society for the History of Science 2 (1958), S. 94-95 
    ISSN: 0950-5636
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    Topics: History , Natural Sciences in General
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  • 8
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    Bulletin of mathematical biology 20 (1958), S. 71-93 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract A somewhat different approach to the principle of biotopological mapping, discussed in previous publications, is given. The organism is considered as a set of properties, each of which is in its turn a set of numerous subproperties which are logically included in the corresponding properties. Topology is introduced by an appropriate definition of neighborhoods, and four postulates are stated which concern the mapping of the spaces corresponding to higher organisms on those of lower ones. A number of conclusions are drawn from the postulates. Some of them correspond to well-known facts. For example, in man and some higher organisms appropriate emotional stimuli should produce gastrointestinal or cardiovascular disturbances; or some microorganisms should produce substances harmful to other microorganisms (antibiotics). Some other conclusions are still awaiting verification. One of them is, for example, that there must exist unicellular organisms which produce antibodies to appropriate antigens.
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    Bulletin of mathematical biology 20 (1958), S. 25-32 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Zusammenfassung Für die Praxis der Pflanzenernährung ist es wichtig, zu wissen, in welcher Weise die Ertragsbildung von der Konzentration eines mineralischen Nährstoffes in der Umgebung der Pflanze abhängt. Da nur diejenigen Nährstoffmengen das physiologische Geschehen in der Pflanze unmittelbar zu beeinflussen vermögen, die sich in der Pflanze befinden, wird angenommen, dass das Wachstum zum Zeitpunktt, d.h. die Geschwindigkeit der Trockensubstanzzunahme zu diesem Zeitpunkt, eine Funktion der zur Zeitt in der Pflanze enthaltenen Nährstoffmenge ist. Diese Nährstoffmenge wird natürlich im Intervall vor dem Zeitpunktt aufgenommen. Deshalb und auch noch aus anderen Gründen hängt das Wachstum zur Zeitt davon ab, wie die in der Umgebung der Pflanze herrschende Konzentration des betrachteten Nährstoffes in demjenigen Zeitintervall verläuft, das sich von der Aussaat bis zum Zeitpunktt erstreckt. Die angegebene Annahme fürhrt zusammen mit einigen weiteren naheliegenden Annahmen zu einem Ansatz, der Ergebnisse liefert, die in verschiedener Hinsicht gut mit der Erfahrung übereinstimmen. Jedoch gibt es auch noch Widersprüche zwischen Theorie und Erfahrung. Durch weitere Ausgestaltung der Theorie lassen sich diese Widersprüche beseitigen. Es wird angeregt, Versuche durchzuführen, deren Resultate Hinweise für die weitere Ausgestaltung der Theorie liefern.
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    Bulletin of mathematical biology 20 (1958), S. 33-70 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract The dynamics of cell multiplication and differentiation in tissues in asteady state and the kinetics of isotope incorporation into the DNA have been theoretically analyzed. Equations have been derived, with the aid of which thegeneration time, thelife span, and the distribution or rate of death of the cells can be obtained if the tissue is in asteady state, i.e., if the number of cells is maintained constant by constant, equal rates of cell division and cell death and if the mean DNA content per cell is also constant. An equation has also been derived which gives thegeneration time in the case of logarithmic multiplication of cells. Two special cases have been analyzed: InCase 1, the isotope is considered as being introduced into the metabolic system at zero time only; inCase 2, the specific activity of the DNA precursor is considered as being maintained constant. The use of the method has been illustrated by an example in which thegeneration time and themean, themedian, and themode life span, as well as the curve of the rate of death of leukocytes in a patient with chronic leukemic granulocytic leukemia, have been obtained from the rate of P32 incorporation into the DNA. The merits and the limitations of the method are discussed.
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  • 11
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    Bulletin of mathematical biology 20 (1958), S. 95-95 
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
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  • 12
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    Bulletin of mathematical biology 21 (1959), S. 1-11 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract By means of the Laplace transform, the behavior of a simplified model of the cardiovascular system is mathematically formulated. This formulation allows mathematical expression of the periodicity of the cardiac output and the systemic response. With the cardiac output represented as half of a sine function cycle, the systolic aortic pressure becomes the sum of a sine term and exponential terms, while the sum of the exponential terms alone represents the diastolic pressure. The characteristics of the mathematical expressions for systole and diastole are analyzed, and some relationships of potentially practical value are derived. Variation in the parameters of the system yields mathematical results consistent with the expected physical ones.
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    Bulletin of mathematical biology 21 (1959), S. 19-32 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract A generalization of Landahl's approximation method (H. D. Landahl,Bull. Math. Biophysics,15, 49–61, 1953) for non-linear diffusion problems is suggested. The method is applied to sorption, desorption, and free diffusion problems involving concentration-dependent diffusion coefficients. With some limitations, the results compare favorably with those obtained by numerical methods.
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    Bulletin of mathematical biology 21 (1959), S. 33-60 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract Recently a theorem for representing current generators in a volume conductor by the superposition of a central dipole, quadrupole, octopole, etc., has been established by G. C. K. Yeh, J. Martinek, and H. de Beaumont (Bull. Math. Biophysics,20, 203–16, 1958). This theorem makes possible the representation of any discrete or line, surface- or volume-distributed current source by a unique model which can be determined for each given case by surface potential measurements and closed form analysis. In this paper the multipole representations of an eccentric dipole and an eccentric double-layer are obtained in terms of the various parameters of the assumed singularities, and the contributions to surface potentials due to each of the multipoles are compared. Certain numerical results corresponding to those of E. Frank (Amer. Heart J.,46, 364–78, 1953) are carried out and compared. Furthermore, the multipole representation of a partially damaged double-layer is also determined and compared with that of an undamaged one. It is concluded that within the range of parameters corresponding to human subjects the higher-order multipoles can contribute significantly to the surface potentials compared with the dipole.
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  • 15
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    Bulletin of mathematical biology 21 (1959), S. 97-100 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract In line with a recent suggestion by the author (Bull. Math. Biophysics,20, 267–73, September, 1958) that not only does the organism as a whole map on the primordial, but that each organ can also be thus mapped, it is shown that the previously introduced abstract spaces, which represent an organism, contain subspaces which map continuously on the space of the primordial. Several theorems about those subspaces are proven.
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  • 16
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    Bulletin of mathematical biology 21 (1959), S. 71-95 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract The DNA-protein coding problem is given a general algebraic formulation, the consequences of which are then explored by standard mathematical methods. To keep the treatment self-contained, the mathematical techniques to be used are explained in detail. It is demonstrated that there exista priori a countably infinite number of different abstract DNA-protein codes, thereby showing that inductive attempts to construct such a code will most likely be fruitless. A notion of ergodicity is then introduced, which imposes a number of restrictions on the admissible codes, and, in fact, these considerations enable us toderive a small portion of a code which, if our hypothesis of ergodicity is correct, must occur in nature. Finally, we discuss briefly the problem as to whether there can exist more than one DNA-protein code in nature.
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  • 17
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
    Notes: Abstract The present-day practices of electrocardiography and vectorardiography are based upon the theory that the surface potential differences can be assumed to be due to a single dipole inside the body. It is shown in this paper that a dipole cannot account for all the surface potentials due to realistic current generators, and hence the determination of the current generator from surface potential measurements based upon such a theory will lead to inconsistent representations of the heart for one and the same subject. To demonstrate this point two eccentric dipoles of different strengths and locations representing two muscle fibers are taken to be the current generator in a homogeneous spherical conductor. The exact surface potentials are then expressed by means of the “interior sphere theorem” of the authors. With these expressions the magnitude, direction, and location of the resultant dipole are determined by the method of D. Gabor and C. V. Nelson (J. App. Physics,25, 413–16, 1954). The surface potentials due to this resultant dipole are again exactly expressed by means of the “interior sphere theorem” and compared with those due to the eccentric dipoles assumed. It can be seen that the differences can be considerable. It is suggested that the multipole model of the authors (Bull. Math. Biophysics,20, 203–16, 1958) be used as a more accurate and the only unique representation of the heart.
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    Bulletin of mathematical biology 21 (1959), S. 101-106 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract In a preceding paper (Bull. Math. Biophysics 20, 71–93, 1958) the principle of biotopological mapping was formulated in terms of a continuous mapping of an abstract space, made from the set of biological properties which characterize the organism, by an appropriate definition of neighborhoods. In this paper it is shown that we may consider directly the mappings of the different sets of properties which characterize different organisms without taking recourse to abstract spaces. All the verificable conclusions made in the preceding paper remain valid. A serious difficulty mentioned previously is, however, avoided and the possibility of more general predictions is established.
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    Bulletin of mathematical biology 21 (1959), S. 107-107 
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
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    Bulletin of mathematical biology 21 (1959), S. 109-128 
    ISSN: 1522-9602
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Mathematics
    Notes: Abstract The general Theory of Categories is applied to the study of the (M, R)-systems previously defined. A set of axioms is provided which characterize “abstract (M, R)-systems”, defined in terms of the Theory of Categories. It is shown that the replication of the repair components of these systems may be accounted for in a natural way within this framework, thereby obviating the need for anad hoc postulation of a replication mechanism. A time-lag structure is introduced into these abstract (M, R)-systems. In order to apply this structure to a discussion of the “morphology” of these systems, it is necessary to make certain assumptions which relate the morphology to the time lags. By so doing, a system of abstract biology is in effect constructed. In particular, a formulation of a general Principle of Optimal Design is proposed for these systems. It is shown under what conditions the repair mechanism of the system will be localized into a spherical region, suggestive of the nuclear arrangements in cells. The possibility of placing an abstract (M, R)-system into optimal form in more than one way is then investigated, and a necessary and sufficient condition for this occurrence is obtained. Some further implications of the above assumptions are then discussed.
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    Bulletin of mathematical biology 21 (1959), S. 141-151 
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
    Notes: Abstract The transient stage of the random dispersal of logistic populations is investigated, using a Sturm-Liouville series leading to an infinite system of non-linear integral equations. These equations are then solved via a successive approximation scheme. R. A. Fisher's (steady-state) velocity of advance paradox is discussed. An illustrative example is worked to the second order of approximation.
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    Bulletin of mathematical biology 21 (1959), S. 153-159 
    ISSN: 1522-9602
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    Notes: Abstract An approximation method using a sine function is used to solve the second degree growth equation for the case in which an organism may simultaneously become dispersed throughout a uniform region. The resulting expression for a special case is compared with the expression obtained by R. Barakat (1959,Bull. Math. Biophysics,21, 141–51), giving the first two terms, by an iterative, procedure. The agreement is satisfactory.
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    Bulletin of mathematical biology 21 (1959), S. 129-140 
    ISSN: 1522-9602
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    Notes: Abstract Diffusion through a flat pore into a large open region is proportional to the linear dimension of the pore and not to its area. This was first explained by Brown and Escombe (1900) for a circular pore and is here generalized, by means of a dimensional argument, to include any type of regular opening. The problem is further generalized to include diffusion through pores of finite thickness, finite distance apart, and into finite regions. Since this problem cannot be solved exactly, an approximation method is introduced. Reasons for the credibility of the approximation are presented. It is then shown, by means of the approximation method, that the diffusive flow through a pore is equal to the total concentration difference divided by the resistance of the system. The resistance, in turn, is the sum of the resistances of all portions of the system, each of which is calculated. The result is compared with results which have been calculated exactly for limiting cases and found to agree very well. The results are then applied to a standard method of computing pore size in membranes, and it is shown that the correction factor is negligible.
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    Bulletin of mathematical biology 21 (1959), S. 161-183 
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
    Notes: Abstract V. S. Ivlev [Experimental Ecology of Nutrition of Fishes, 1955, Moscow (in Russia)] has shown that the food uptake by fishes during a fixed interval of time is an exponential function of the concentration of food. Ivlev's equation is derived here, and it is shown that it can hold only for non-stationary conditions, such as prevailed in Ivlev's experiments. For a stationary state, the rate of food uptake should tend asymptotically to a limiting value as the concentration increases, but the variation is not exponential. Different other aspects of the problem are investigated, and definite new experimental procedures suggested. The implications of Ivlev's findings on the effect of non-uniformity of food distribution upon the rate of food consumption are studied from a mathematical point of view. The conclusion is reached that whereas a fish does not, in the process of eating, move directly to an individual food particle which it perceives, it does move more or less directly to large aggregates of particles, if the latter are distributed nonuniformly.
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    Bulletin of mathematical biology 21 (1959), S. 185-193 
    ISSN: 1522-9602
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    Topics: Biology , Mathematics
    Notes: Abstract Some relational aspects of the property of self-reproduction of biological systems are studied. If in addition to the requirement of the property of self-reproduction we add also the requirement of adaptability of the organism to changing environment, this imposes certain conditions on the topology of the graphs which represent such systems. A further study of the relational properties of such systems seems to offer the possibility of deriving the principle of biological mapping from the requirement of self-reproduction and adaptability. An examination of the problem of the original formation of such self-reproducing systems in connection with the established fact of impossibility of spontaneous generation leads to the conclusion that an organism must inhibit such processes which, in the absence of organisms, would lead to spontaneous generation.
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    Bulletin of mathematical biology 21 (1959), S. 195-216 
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    Notes: Abstract In the human, the antagonistic, extensor-flexor system of the leg is an example of a common type of neurophysiological feedback system. After a brief introduction to the neuroanatomy and physiology of this feedback system, the paper formulates transfer functions from temporal response data available in the literature. A feedback stability analysis, based on the extension of Nyquist's stability criteria to multiple-loop systems and utilizing flow-graph techniques, demonstrates the stable behavior of the system. Expressions are given relating the sensitivity of the system to variations in muscle response and Golgi tendon organ (tension receptor) response. By considering the events taking place at synapses and end-plates during “isometric tension-small knee angle excursion” conditions as stationary stochastic processes, an external “noise” input to the system is given, whose spectrum is derived from the statistics of a shot-process representation of these events. The paper concludes with some correlations between the analytical results and clinical syndromes.
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    Bulletin of mathematical biology 21 (1959), S. 217-255 
    ISSN: 1522-9602
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    Notes: Abstract In this continuation of a previous report it is shown how the Volterra population dynamics, which underlies the statistical theory, can be based on a variational principle; how the dynamics can be generalized as regards both the behavior of total populations and migration phenomena; and how many directly observable data, such as amplitudes and frequencies of oscillation of a population, fit into the statistical theory and can test it. Such a test is carried out in some detail using the fox-catch data of Elton, with a clear indication that the theory is capable of comprehending the major statistical properties of population-time curves. A final section sketches an extension of the theory to cover secular variations of external conditions such as temperature of the environment.
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    Bulletin of mathematical biology 20 (1958), S. 1-23 
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    Notes: Abstract To account for some of the more important aspects of drug interaction we shall consider a model which can also account for certain general properties of the action of a single drug. A simple model in which there may be enzymatic detoxification of a drug is studied theoretically. The relation between time for appearance of an effect due to the drug and the size of the dose is found to contain the same parameters as the relation between the effectiveness of paired doses and the interval of time between doses. A similar situation holds when the drug is given at a constant rate. When two drugs are administered together, their effect will depend on the manner of interaction, how much of each drug is given, which is given first, and on the interval of time between each administration. A number of plausible types of interaction is considered theoretically in terms of the model, analytical expressions being given for a number of cases. The interaction may be synergistic or antagonistic. In the former case the potentiation may be more than or less than additive depending on the order of delivery and on the time between injections. Methods for the estimation of the parameters from data are discussed.
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    Bulletin of mathematical biology 21 (1959), S. 13-17 
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    Notes: Abstract This paper extends Leslie's vector and matrix treatment of populations. A simple matrix is given for species in which adult mortality and fertility are independent of age, but in which the juvenile mortality rate differs from the adult. The population vector can be changed into a population matrix. This should allow equations using functions of the size of the population to be developed. Genetic variables such as sex or other polymorphisms can be introduced, and the notation allows different systems of selection or non-random mating to be specified.
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    European journal of wildlife research 4 (1958), S. 48-56 
    ISSN: 1439-0574
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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    European journal of wildlife research 4 (1958), S. 93-99 
    ISSN: 1439-0574
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    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Description / Table of Contents: Summary The fortunate circumstance that the world of ancient Mesopotamia from the third up to the first millenium b. C. has preserved not only proofs of plastic art and reliefs, but also thousands of seal pictures, which often show animals, enables us to study the fauna of the ancient Orient much better than that of many other periods and territories. Especially about 2800, 2300, and 1300 b. C. people were very diligent with animal portraits, and naturally they chose in the first place to illustrate chase or chaseable animals. Starting with the lion the bear, wild oxen, wild sheep and goat, the oriental kinds of antelopes and stags up to the ostrich and the wild boar we find here almost complete documentary evidence of the animals to be hunted, which will be continued once more in the later Assyrian reliefs — here not treated. These testimonies are the more valuable because they are generally very animated and prove a surprising capacity of observation of these creatures.
    Abstract: Résumé C'est un fait heureux que du monde de l'ancienne Mésopotamie du troisième jusqu'au premier millénaire a. J.-C. nous sommes remis à coté des pièces justificatives de l'art plastique et de l'art du relief aussi des images de sceaux présentant très souvent des animaux, ce que nous donne la possibilité d'étudier de beaucoup mieux la faune de l'ancien Orient que celle de beaucoup d'autres époques et régions. C'est surtout vers le temps de 2800, 2300 et 1300 a. J.-C. qu'on soignait très bien le portrait d'animaux et ce n'est que trôp compréhensible que se sont surrout les représentations de chasse ou au moins des bêtes bonne à chasser qui y sont en vedette. Commancé par le lion en passant par l'ours au boeuf sauvage, le mouton et la chèvre sauvage, les espèces d'antilopes se trouvant en Asie antérieur, jusqu'au cerf, l'autruche et le sanglier; on y trouve une documentation presque complète sur tous les bêtes bonne à chasser; documentation qui sera encore continuée dans les reliefs de l'ancien Assyrie, quoique ces derniers ne soient pas traités dans cet ouvrage. Ces témoignages sont d'autant plus précieux, qu'ils font le plus souvent épreuve d'une grande vivacité et qu'ils accusent un talent d'observations étonnant chez leurs créateurs.
    Notes: Zusammenfassung Der glückliche Umstand, daß die Welt Altmesopotamiens vom 3. bis zum 1. Jahrtausend v. Chr. uns neben Belegen der Vollplastik und Reliefkunst Tausende von Siegelbildern aufbewahrt hat und auf diesen häufig Tiere abgebildet sind, ermöglicht es uns, die Fauna des Alten Orients weit besser studieren zu können als die vieler anderer Zeiten und Gebiete. Besonders um 2800, um 2300 und um 1300 v. Chr. hat man sich um Tierporträts sehr bemüht, und hierbei steht verständlicherweise das Jagdbild oder zum mindesten das jagdbare Wild im Vordergrund. Vom Löwen angefangen über Bär, Wildrind, Wildschaf und-ziege, die vorderasiatischen Antilopenarten und den Hirsch bis hin zum Strauß und das Wildschwein wird hier eine nahezu vollständige Beurkundung der jagdbaren Tiere geboten, die dann in den — hier nicht behandelten —spätassyrischen Reliefs noch einmal fortgesetzt wird. Diese Zeugnisse sind um so kostbarer, als sie meist von großer Lebendigkeit sind und eine erstaunliche Beobachtungsgabe ihrer Schöpfer beweisen.
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    Meteorology and atmospheric physics 10 (1958), S. 301-304 
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    Description / Table of Contents: Zusammenfassung Aus einer Untersuchung der aeronomischen Verhältnisse in der unteren Thermosphäre ergibt sich, daß das Maximum der Konzentration an atomarem Sauerstoff seinen Sitz in ungefähr 90 km Höhe hat und unabhängig ist von den Bedingungen des photochemischen Gleichgewichts. Eine solche Verteilung des atomaren Sauerstoffs gestattet einen Schluß auf die Beziehungen, die zwischen dem Transport der Sauerstoffatome und der Emission der Linie 5577 Å des Nachthimmelslichts sowie den niedrigen Temperaturen oberhalb der Mesopause bestehen.
    Abstract: Summary An aeronomic study of departures from photoequilibrium conditions in the lower thermosphere shows that the peak of atomic oxygen concentration occurs in the neighbourhood of 90 km. Its vertical distribution must be associated with the airglow emission at 5577 Å and the low temperatures above the mesopause.
    Notes: Résumé Une étude des conditions aéronomiques dans la thermosphère inférieure montre que le maximum de la concentration de l'oxygène atomique est situé aux environs de 90 km et ne dépend pas des conditions d'équilibre photochimique. Une telle distribution de l'oxygène atomique permet de souligner les relations existant entre le transport des atomes d'oxygène et l'émission de la raie 5577 Å du ciel nocturne et également les basses températures au-dessus de la mésopause.
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    Meteorology and atmospheric physics 10 (1958), S. 328-338 
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    Description / Table of Contents: Zusammenfassung Die auf die planetare Grenzschicht angewandten Bewegungsgleichungen werden für spezielle Verteilungen des Austauschkoeffizienten numerisch integriert. Beschleunigungen werden beibehalten, vertikale, und, in geringerem Maße, zeitliche Variationen des Austauschkoeffizienten angenommen. Die resultierenden Trägheitsschwingungen sind zwar im allgemeinen sehr beschränkt, zeigen jedoch gute Übereinstimmung mit den Beobachtungen. In einzelnen Fällen kann eine Drehung des Windvektors nicht nur im Uhrzeigersinn, sondern auch im Gegenuhrzeigersinn auftreten. Einige Lösungen stimmen gut, andere nicht mit den analytischen Lösungen für einen unbegrenzten Austauschkoeffizienten überein.
    Abstract: Résumé Les équations du mouvement appliquées à la couche limite planétaire sont intégrées pour des distributions particulières du coefficient d'échange turbulent. On tient compte des accélérations et on admet des variations verticales et, en moindre mesure, temporelles du coefficient d'échange. Les oscillations d'inertie qui en résultent sont, il est vrai, très limitées mais s'accordent bien avec les observations. Dans certains cas une rotation de la résultante du vecteur vent peut apparaître, non seulement dans le sens des aiguilles d'une montre, mais aussi en sens contraire. Quelques solutions concordent avec celles que l'on obtient en admettant un coefficient d'échange illimité, d'autres pas.
    Notes: Summary The equations of motion applied to the planetary boundary layer are numerically integrated for certain special eddy viscosity distributions. Accelerations are retained, eddy viscosity varied with height and, to a lesser extent, with time. The resulting inertial oscillations, although very limited in generality, show agreement with observations. Not only clockwise but also counterclockwise rotation of the end point of the wind vector can occur in some cases. Some solutions agree and others disagree with the analytical solutions for unbounded eddy viscosity.
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    Meteorology and atmospheric physics 10 (1958), S. 285-290 
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    Description / Table of Contents: Zusammenfassung Wenn man den Einfluß nicht-adiabatischer Vorgänge auf die atmosphärischen Prozesse berücksichtigen will, ist es unentbehrlich, die räumliche und zeitliche Verteilung der Strahlungsbilanz innerhalb der Atmosphäre und längs ihren Begrenzungen zu erkennen. Gleich wie für die synoptischen Daten müssen auch die auf die Strahlung bezüglichen Angaben repräsentativ sein.
    Abstract: Résumé Si l'on veut tenir compte des effets non-adiabatiques sur les processus atmosphériques, il est indispensable de connaître la répartition spatiotemporelle du bilan radiatif dans l'atmosphère et le long de ses frontières. Tout comme pour les données synoptiques, les données relatives au rayonnement doivent être représentatives des grandeurs météorologiques mesurées.
    Notes: Summary In order to be able to account for non-adiabatic effects on atmospheric processes, the space and time distributions of actual values of the radiation balance must be known in the atmosphere and at its boundaries. As for synoptic data, the representativeness of radiation data is an essential requirement.
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  • 97
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    Meteorology and atmospheric physics 10 (1958), S. 291-300 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Eine Methode, das jahreszeitliche Wärmebudget der Atmosphäre zu berechnen, hat auch der Wärmespericherung in den Ozeanen Rechnung zu tragen. Auf Grund von Wasserthermographenwerten und Ozeanoberflächentemperaturen wurden die dem Ozean zugeführten oder von ihm abgegebenen Wärmemengen monatsweise berechnet. Die im Ozean gespeicherte Wärme wurde dann mit der vonGabites aufgestellten Schätzung der durch Strahlung und durch die latente Wärme des Wasserdampfs zugeführten Wärmeenge verglichen und von dieser Vergleichung wurde auf die Erwärmung der Atmosphäre geschlossen. In mittleren Breiten liegt der Erwärmungszuwachs der Atmosphäre während des Großteils des Jahres bei Null, so daß sogar das Vorzeichen der Erwärmung zweifelhaft ist. Während des Großteils des Jahres erfährt die Atmosphäre dagegen in niederen Breiten einen Wärmezuwachs, in hohen Breiten einen Überschuß an Abkühlung. Diese Überschüsse werden durch Bewegungsvorgänge in der Atmosphäre und im Ozean verfrachtet.
    Abstract: Résumé Une méthode visant à calcular le bilan thermique annuel de l'atmosphère doit tenir compte de la chaleur mise en réserve dans les mers. Des mesures de température de l'eau de mer en profondeur et en surface permettent d'établir les quantités de chaleur fournies mensuellement à la mer ou enlevée à celle-ci. La chaleur accumulée fut alors comparée à celle qu'estimeGabites en considérant la chaleur fournie par rayonnement et par la chaleur latente de la vapeur d'eau; on en a tiré une conclusion relative au réchauffement de l'atmosphère. Aux latitudes moyennes, l'accroissement de chaleur de cette dernière est voisine de zéro la plus grande partie de l'année, de sorte que même le signe est douteux. Aux latitudes basses par contre l'atmosphère reçoit de la chaleur pendant la plus grande partie de l'année; elle en perd aux latitudes élevées. Ces gains et ces pertes s'équilibrent in globo par les mouvements de l'air et de l'eau.
    Notes: Summary One method of computing the seasonal heat budget of the atmosphere involves the seasonal heat storage in the oceans. On the basis of bathythermograph data and ocean surface temperatures, the heat added to, or released by the ocean was computed month by month. The heat stored in the ocean was then compared withGabites' estimate of the heat added by radiation and by means of the latent heat of water vapor. From this comparison, the heating of the atmosphere was approximated. In middle latitudes, the net heating of the atmosphere is close to zero during most of the year, so that even the sign of the atmospheric heating is in doubt there. During most of the year, the atmosphere undergoes net heating in low latitudes, and net cooling in high latitudes. The excess is removed by motions of the atmosphere and the ocean.
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  • 98
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    Meteorology and atmospheric physics 10 (1958), S. 339-349 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die vereinfachten Bewegungsgleichungen werden gelöst, um Scheitelbreiten für Trajektorienscharen der Luftbewegungen zu finden, die ausgehend von dem Ruhezustand unter Einwirkung eines konstanten meridionalen Druckgradienten polwärts gerichtet sind. Der allgemeine Fall wird diskutiert und es werden Berechnungen für den 20. westlichen Längengrad der Nordhemisphäre für Januar und Juli durchgeführt. Der resultierende Massentransport zeigt, daß im Januar in 32° N ein Konvergenzgürtel auftreten sollte. Dies stimmt gut überein mit der geographischen Breite der Achse des mittleren subtropischen Hochdruckgürtels zu dieser Jahreszeit. Schließlich wird die Form des klimatologischen Modells für niedere Breiten, das durch diese Berechnungen nahegelegt wird, diskutiert.
    Abstract: Résumé Résolution des équations simpflifiées du mouvement pour déterminer l'origine des faisceaux de trajectoires des courants aériens qui, partant du repos, sont dirigés vers le pôle sous l'effet d'un gradient constant de pression méridien. Discussion du cas général; calcul pour le 20e méridien Ouest de l'hémisphère Nord en janvier et en juillet. Le transport de masse résultant montre qu'il doit y avoir en janvier, a 32° de latitude Nord, une ceinture de convergence ce qui concorde bien avec la latitude de l'axe de la zone moyenne des hautes pressions subtropicales en cette saison. Forme du modèle climatologique aux basses latitudes suggéré par ces calculs.
    Notes: Summary The primitive equations of motion are solved to find peak latitudes of families of trajectories of air moving from low latitudes towards the pole from a state of rest under the action of a constant meridional pressure gradient. The general case is discussed first and then calculations are applied to the 20° West meridian in January and July for the Northern Hemisphere. The resulting mass transposition indicates that a belt of convergence should occur at about 32° N in January; this agrees well with the latitude of the axis of the mean sub-tropical high pressure belt at that time of year. The nature of the climatological model in low latitudes suggested by the calculation is then discussed.
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  • 99
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    Meteorology and atmospheric physics 10 (1958), S. 350-354 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Summary According to Sprung's formula for obtaining the relative humidity from psychrometer-readings, graphs have been produced. For simplifying the method of reading it has been tried to replace the two-dimensional arrangement by a simple slide rule; in this case the psychrometric formula should correspond to the equationR=100 f(t′)/f(t) (t=dry temperature,t′=wet bulb temperature), which is not fulfilled by Sprung's formula. Another formula is therefore here developed, leading to a satisfactory approximation, provided that the division of theR-scale be somewhat modified and differences be allowed up to 2 1/2%.
    Abstract: Résumé Pour déduire l'humidité relative des observations psychrométriques on emploie généralement la formule de Sprung ou des tableaux graphiques en diverses formes reposant sur celle-ci. Pour simplifier la procédure de lecture on a aussi essayé de remplacer ces représentations bi-dimensionelles par un simple curseur. Dans ce cas la formule psychrométrique devrait remplir la conditionR=100 f(t′)/f(t) (t=température sèche,t′=température mouillée), ce qui ne correspond pas à la formule de Sprung. Pour cette raison, on a développé une autre formule qui permet une approximation suffisante à condition que l'on corrige légèrement l'échelle pourR et qu'on admet des écartes jusqu'a 2 1/2%.
    Notes: Zusammenfassung Nach der zur Berechnung der relativen Feuchtigkeit aus Psychrometerablesungen aufgestellten Sprungschen Formel sind graphische Tafeln in verschiedenen Ausführungen hergestellt worden. Um das Ableseverfahren zu vereinfachen, ist auch versucht worden, diese zweidimensionalen Darstellungen durch einen einfachen Rechenschieber zu ersetzen; doch müßte in diesem Fall die Psychrometerformel die Bedingung erfüllenR=100 f(t′)/f(t) (t=Trockentemperatur,t′=Feuchttemperatur), was die Sprungsche Formel nicht tut. Es läßt sich nun eine andere Formel aufstellen, mit deren Hilfe man schon mit einer mäßigen Annäherung auskommt, wenn man die Skaleneinteilung fürR (bzw. logR) etwas korrigiert und Abweichungen bis zu 2 1/2% in Kauf nimmt.
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  • 100
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    Meteorology and atmospheric physics 10 (1958), S. 410-414 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Summary A radiation-turbulence model for the formation of high fog in the Vienna basin is described showing that stratus outside bad weather regions can be expected only on the margin of high-pressure areas with southeastern surface wind. This as well as other conclusions which can be used for forecasts are in perfect agreement with experience.
    Abstract: Résumé Description d'un schéma rayonnement/turbulence de la formation du brouillard élevé dans le bassin de Vienne s'appliquant aux couches de stratus des domaines de haute pression, en dehors des zones de mauvais temps, par vent du Sud-Est au sol. L'expérience vérifie ces conditions de formation et d'autres encore, importants pour la prévision.
    Notes: Zusammenfassung Es wird ein Strahlungs-Turbulenz-Modell der Hochnebelbildung im Wiener Becken beschrieben, das Stratusdecken außerhalb von Schlechtwettergebieten nur bei Hochdruckrandlagen mit südöstlicher Grundströmung erwarten läßt. Sowohl diese, als auch weitere, prognostisch verwertbare Folgerungen stehen mit der Erfahrung völlig im Einklang.
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