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  • 1980-1984  (11)
  • 1970-1974  (10)
  • 1960-1964  (21)
  • 1
    Electronic Resource
    Electronic Resource
    METEOROLOGICAL EFFECTS OF REJECTED HEAT (1980)
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 338 (1980), S. 0 
    Details
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1749-6632.1980.tb17150.x
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  • 2
    Electronic Resource
    Electronic Resource
    In memoriam professor Frederick Sargent II 1920–1980 (1980)
    Springer
    International journal of biometeorology 24 (1980), S. 277-278 
    Details
    ISSN: 1432-1254
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02250568
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  • 3
    Electronic Resource
    Electronic Resource
    Book reviews (1962)
    Springer
    International journal of biometeorology 5 (1962), S. 101-102 
    Details
    ISSN: 1432-1254
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02186060
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  • 4
    Electronic Resource
    Electronic Resource
    Variations in the global water budget (1983)
    Springer
    Boundary layer meteorology 27 (1983), S. 413-413 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02033749
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  • 5
    Electronic Resource
    Electronic Resource
    Note on rapid pulsations of temperature lapse rate (1970)
    Springer
    Boundary layer meteorology 1 (1970), S. 61-63 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Pulsations of the lapse rate between 1 and 5 m were recorded on a sunny day over a field of tall weeds (z 0 ≈ 6 cm) and over a parking lot (z 0 ≈ 0.1 cm). The frequency distributions of values recorded every 2 sec in a 20 min span were nearly identical in the two environments. Values ranged from inversions of 0.75 °C to lapses of 1.75 °C. There was a tendency for a wider range of fluctuations in short time intervals in the weeds than over the smoother parking lot. The data suggest that these very short-periodic fluctuations were dynamically induced.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00193904
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  • 6
    Electronic Resource
    Electronic Resource
    Book review (1973)
    Springer
    Boundary layer meteorology 3 (1973), S. 522-524 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01034991
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  • 7
    Electronic Resource
    Electronic Resource
    Micrometeorological observations in an area of urban growth (1972)
    Springer
    Boundary layer meteorology 2 (1972), S. 365-370 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Stationary and mobile surveys of micrometeorological changes in the new town of Columbia, Maryland have been made since late 1967. These show the development, intensification, and expansion of an urban heat island. This phenomenon is principally attributable to the altered heat flux into and out of the soil caused by the change in surface characteristics. About half of the observed change of relative humidity can be assigned to decreased evapotranspiration as a result of replacing vegetation by stone and asphalt.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02184776
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  • 8
    Electronic Resource
    Electronic Resource
    A note on bedroom bioclimate (1962)
    Springer
    Theoretical and applied climatology 12 (1962), S. 159-163 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung Es wird über eine dreimonatige Meßreihe in der Übergangszeit zwischen Frühling und Sommer in einem Schlafzimmer im Gebeit von Washington, D. C., berichtet. Solange Zentralheizung nötig war und die Fenster geschlossen blieben, war das Zimmerklima von den Außenverhältnissen ganz unabhängig. In der späteren Jahreszeit nahm bei offenem Fenster die Innentemperatur nachts im Mittel um 1,6° C ab und die Feuchte um 6% zu. Mit fortschreitender Erwärmung wurden die Abendbedingungen teilweise unbehaglich und in mehreren Fällen überschritten sie die Schwülegrenze. Mit Hilfe eines Ventilators ließen sich jedoch Werte der Abkühlungsgröße und der behaglichkeitsziffer im Bereich des Angenehmen wiederherstellen.
    Abstract: Résumé On rapporte ici sur les mesures effectuées durant 3 mois de l'entresaison printemps-été dans une chambre à coucher des environs de Washington, D.C. Le climat de la dite chambre a été absolument indépendant des conditions extérieures tant que le chauffage central fut nécessaire et que les fenêtres sont restées fermées. Plus tard, et par fenêtre ouverte, la température intérieure a diminué de 1,6°C en moyenne durant la nuit, alors que l'humidité relative augmentait de 6%. Avec l'arrivée des chaleurs estivales, les conditions y furent parfois désagréables et la limite du climat dit “lourd” fut franchie quelquefois. Cependant, la valeur du pouvoir réfrigérant et du chiffre de confort purent être ramenés dans la zone de confort par un ventilateur.
    Notes: Summary A three-month survey of bedroom climate in the transition season from spring to summer in the Washington, D. C., area is presented. It showed nearly complete independence from outdoor conditions during the period when central heating was needed and windos were closed. Later in the season, with open windows, nocturnal temperature drop indoors averaged about 1.6° C, while humidity increased about 6%. As the season progressed evening conditions approached discomfort and exceeded the limit of sultriness several times. But with mechanical ventilation cooling powers and comfort numbers in the optimal zone could be re-established.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02317959
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  • 9
    Electronic Resource
    Electronic Resource
    Some patterns of rainfall in the North-Central U.S.A. (1960)
    Springer
    Theoretical and applied climatology 10 (1960), S. 165-174 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung Wöchentliche Werte der Niederschlagswahrschein-lichkeit in der nördlichen Mittelzone der Vereinigten Staaten zeigen bevorzugte Regenperioden zu Anfang der Monate April und Juni. Trockene Wochen sind am häufigsten im Spätoktober, Mitte November, Mitte Dezember und zur Jahreswende. Eine nordwärts gerichtete Wanderung der Regentendenz im Frühling und Frühsommer wird mit einer gleichzeitigen Verschiebung des jet stream in Zusammenhang gebracht. Eine mögliche Beziehung dieser Witterungsfälle zu den “Singularitäten” in anderen Gegenden und zuBowens Regenstatistik wird erörtert, doch sind gesicherte Beziehungen nicht feststellbar.
    Abstract: Résumé Des valeurs hebdomadaires de la probabilité de pluie dans la zone moyenne septentrionale des Etats-Unis mettent en évidence des périodes pluvieuses particulièrement fréquentes au début des mois d'avril et de juin. Des semaines sèches apparaissent le plus souvent à la fin d'octobre, au milieu de novembre et de décembre et vers le Nouvel-An. Un déplacement vers le Nord de la tendance pluvieuse au printemps et au début de l'été peut être mis en parallèle avec un déplacement simultané du jet stream. On ne peut pas déceler de relations sûres entre ces cas de pluviosité et les singularités dans d'autres régions, pas plus qu'avec la statistique pluvieuse deBowen.
    Notes: Summary Weekly statistics of rainfall occurrence in the North-Central United States show certain preferences for precipitation in early April and early June. Dry spells are most common in late October, Mid-November, Mid-December and at the end of the year. A northward migration of the rainy condition in spring and early summer is linked with a comparable motion of the jet stream. The possible connection of these spells with “singularities” elsewhere andBowen's rain statistics is discussed but no firm relations can be established.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02246562
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  • 10
    Electronic Resource
    Electronic Resource
    Variable solar emissions, the “Maunder Minimum” and climatic temperature fluctuations (1980)
    Springer
    Theoretical and applied climatology 28 (1980), S. 181-191 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung Erst jetzt ausgewertete Tagebücher lassen erkennen, daß eine Reihe von Sonnenflecken- und Nordlichtbeobachtungen während des sog. „Maunder Minimums” der Sonnenaktivität unbekannt geblieben sind. Nun zeigt sich, daß der grundsätzliche solare Rhythmus aufrecht geblieben war. Eine Rekonstruktion der Nordhemisphärentemperaturen zurück bis 1579 ergibt, da\, auf die Nordhemisphäre bezogen, das „Maunder Minimum” nicht besonders kalt war. Die kältesten Jahrzehnte waren vor (1600 bis 1619) und besonders nach (1800 bis 1819) dem „Maunder Minimum”. Die Varianzspektrumanalyse zeigt, daß die Sonnenfleckenrhythmen nur wenig zur Gesamtvarianz der Temperatur beitragen.
    Notes: Summary Unexploited diary sources show that a number of sunspot and auroral observations during the so-called “Maunder Minimum” of solar activity have escaped attention. There is good evidence that the basic solar rhythms were maintained. A reconstruction of northern hemisphere temperatures back to 1579 showed that, on a hemispheric basis, the “Maunder Minimum” was not particularly cold. The coldest decades were before (1600–1619) and particularly after (1800–1819) the “Maunder Minimum”. Spectral analysis shows that the sunspot rhythms contribute only little to the total variance.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02245350
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