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  • 1
    ISSN: 1520-510X
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Analytical chemistry 47 (1975), S. 1880-1880 
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Journal of agricultural and food chemistry 14 (1966), S. 307-311 
    ISSN: 1520-5118
    Source: ACS Legacy Archives
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 4
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    Boston, Mass., etc. : Periodicals Archive Online (PAO)
    The North American Review. 136 (1883:Jan./June) 467 
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  • 5
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Charge-ordering is an important phenomenon in conducting metal oxides: it leads to metal–insulator transitions in manganite perovskites (which show ‘colossal’ magnetoresistances), and the Verwey transition in magnetite (in which the material becomes insulating at low ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Acta crystallographica 30 (1974), S. 2267-2269 
    ISSN: 1600-5740
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
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    Unknown
    London, etc. : Periodicals Archive Online (PAO)
    Slavonic and East European review. 21:1 (1943:Mar.) 188 
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    International journal of biometeorology 15 (1971), S. 41-54 
    ISSN: 1432-1254
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die Untersuchung befasst sich mit den mikroklimatischen Unterschieden von gepflasterten und Grasflächen-Zonen der Stadt und Vorstadt von Cincinnatti,Ohio, anhand der Daten von Feucht- und Trockentemperatur, Strahlungswärme und Luftbewegung. Daraus wurden berechnet: die Effektive Temperatur und die korrigierte Effektive Temperatur, die Nass-Globe-Temperatur, der Discomfort-Index und der Relative-Strain-Index. Die Werte wurden untersucht in Hinsicht auf die Gesundheit und Behaglichkeit der Stadtbewohner im Vergleich mit den Vorstadtbewohnern. Am Nachmittag waren Grasflächen angenehmer als gepflasterte Flächen, am Abend war es umgekehrt. Dieser Stadt-Vorort Unterschied zeigt auf, dass der Wärmeüberschuss in der Stadt die direkte Ursache der Hitze-Todesfälle während extremer Hitzeperioden sein kann. Die wohlüberlegte Verteilung von Grünflächen und die Verwendung von Baumaterialien mit geringer Wärmeleitung und Wärmespeicherung und höheren Albedos werden zur Abschwächung des städtischen Wärmeüberschusses vorgeschlagen.
    Abstract: Resume On étudie ici les différences micrométéorologiques entre les zones pavées et engazonnées de Cincinnati, Ohio, USA, et cela aussi bien dans la villemême que dans les faubourgs. Pour cela, on a mesuré la température des thermomètres sec et mouillé, la chaleur radiante et la vitesse du vent. On en tire la température effective, la température effective corrigée, la température du thermomètre mouillé, l'indice dinconfort et l'indice de contrainte relative. On interprête ces chiffres au vu de l'état de santé et de confort des habitants du centre urbain lui-même par rapport à ceux des banlieusards. L'après-midi, les zones engazonnées sont plus agréables que celles qui sont pavées. Le soir, les faubourgs présentent un confort plus important que la ville. Les différences constatées entre la ville et sa banlieue montrent que les excès thermiques de la première sont directement responsables de la mortalité par coups de chaleur pendant les périodes de chaud prononcé. Pour améliorer les conditions de vie, c'est-à-dire diminuer les excès thermiques, on propose une répartition équilibrée de zones vertes et l'usage de matériaux de construction ayant de faibles conductivité et capacité thermiques ainsi qu'un albédo élevé.
    Notes: Abstract The study gives the microenvironmental contrasts between paved and grass surfaces, in both urban and suburban areas of Cincinnati, Ohio. Wetand dry-bulb temperatures, radiant heat, and air velocity measurements are presented. Thermal indices such as effective temperature, corrected effective temperature, wet-bulb globe temperature, discomfort index, and relative strain index are calculated from these measurements. The data are interpreted with respect to the health and comfort of urban inhabitants relative to adjacent suburban inhabitants. During the afternoon, the grass sites were more comfortable than paved sites. During the evening, the suburban area was significantly more comfortable than the urban area. The urban-suburban differences indicate that the urban thermal excess may be a direct factor in heat deaths during periods of extreme heat. Careful spacing of green areas, and the use of building materials with lower heat conductivity and heat storage properties and higher albedoes are suggested to ameliorate the urban temperature excess.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 25 (1983), S. 171-191 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Sensible heat flux data obtained from the U.S. Environmental Protection Agency's Regional Air Pollution Study in St. Louis, Missouri are presented and discussed. Large spatial variations exist in heat flux on both a land-use scale and the urban scale. Arguments based upon empirical data and sampling theory show that estimates of heat flux representative of an upwind fetch l x require a minimum observation height proportional to z 3/4. The influence of advection on the magnitude of the heat flux is also explored for both the urban and sub-urban or land-use scales. The data clearly indicate that advection can strongly modulate and even dominate the vertical heat flux above surfaces in areas which maintain large horizontal temperature gradients. The advection contribution is positive for cold air advection and negative for warm air advection, and may result from either the urban heat island or land-use mesoscale features. The depth of advective influence is directly proportional to the horizontal scale of the phenomenon and inversely proportional to horizontal temperature gradient.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Boundary layer meteorology 38 (1987), S. 249-272 
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The spatial variation of the nocturnal urban boundary-layer structure is described and the time variation of the mixing height, and the nocturnal inversion top and strength after sunrise is presented for urban sites located upwind, downwind, and near the center of the heat island, and at an upwind rural site. Observations were derived from high resolution temperature profiles obtained by a helicopter during 35 intensive morning experiments in St. Louis, Missouri. The nocturnal urban boundary layer increased in depth from the upwind edge of the urban area. Far downwind, in suburban and rural areas, a remnant of the urban boundary layer existed between a stable surface-based layer and an upper inversion that resembled the upwind rural inversion. The mixing height (base of the inversion) evolved in a parabolic manner after sunrise at the urban locations. A rise in the inversion top after sunrise at the urban locations is believed to be due to low-level convergence which caused the entire inversion layer to be lifted. Due to large horizontal temperature gradients associated with the urban heat island, cold air advection tended to counteract the urban-induced lifting effect by inhibiting mixing-height growth at urban locations upwind of the heat-island center. Advection also caused the maximum height and fastest growth rate of the urban mixed layer to be shifted downwind of the urban area with time. However, mean mixing-height growth rates at various urban locations did not differ significantly. The rural mixing-height growth rate was about twice as large as urban values for up to 3 hr after sunrise. Spatial differences in the mixing height became small near the time of inversion dissipation, which appeared to occur at about the same time at all locations.
    Type of Medium: Electronic Resource
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