995 resultados para 190-1175
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Contient : 1° « Le Truant », ou « Le secret parlement de l'homme contemplatif à son ame », de « JEHAN JARSON » ; 2° « Livre de Contemplation », du même, formant la deuxième partie du Truant ; 3° « Devotions ordonnez par Frere BONAVENTURE », recueil de trente-huit pièces dévotes traduites ou imitées de St Bonaventure ; 4° « Le Livre de SENEQUE qui parle des quatre vertus principaulz », traduction française de « JEHAN TROUSSEAU » ; 5° « Ung petit Traitié de moralité de philozophie » ; 6° Instruction pour entendre la messe
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Servicios registrales
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El presente trabajo de grado tiene como propósito evidenciar los cambios que se generaron en las dinámicas sociales de los residentes y comerciantes del barrio San Bernardo, cuando se decidió declarar este territorio idóneo para el Tratamiento de Renovación Urbana como resultado de una serie de especulaciones originadas por parte de la comunidad debido a la incertidumbre generada por la presencia de las entidades distritales en este barrio de Bogotá.
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Incluye índices, en el primero se citan los temas de cada una de las ciencias sobre los que se incluyen experiencias, indicando la página inicial del tema. El segundo índice hace referencia a todas las experiencias en el mismo orden en el que aparecen en el libro. El último es un índice general de búsqueda alfabética
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Flow and turbulence above urban terrain is more complex than above rural terrain, due to the different momentum and heat transfer characteristics that are affected by the presence of buildings (e.g. pressure variations around buildings). The applicability of similarity theory (as developed over rural terrain) is tested using observations of flow from a sonic anemometer located at 190.3 m height in London, U.K. using about 6500 h of data. Turbulence statistics—dimensionless wind speed and temperature, standard deviations and correlation coefficients for momentum and heat transfer—were analysed in three ways. First, turbulence statistics were plotted as a function only of a local stability parameter z/Λ (where Λ is the local Obukhov length and z is the height above ground); the σ_i/u_* values (i = u, v, w) for neutral conditions are 2.3, 1.85 and 1.35 respectively, similar to canonical values. Second, analysis of urban mixed-layer formulations during daytime convective conditions over London was undertaken, showing that atmospheric turbulence at high altitude over large cities might not behave dissimilarly from that over rural terrain. Third, correlation coefficients for heat and momentum were analyzed with respect to local stability. The results give confidence in using the framework of local similarity for turbulence measured over London, and perhaps other cities. However, the following caveats for our data are worth noting: (i) the terrain is reasonably flat, (ii) building heights vary little over a large area, and (iii) the sensor height is above the mean roughness sublayer depth.
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Many clouds important to the Earth’s energy balance contain small amounts of liquid water, yet despite many improvements, large differences in retrievals of their liquid water amount and particle size still must be resolved.
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The robustness of the parameterized gravity wave response to an imposed radiative perturbation in the middle atmosphere is examined. When momentum is conserved and for reasonable gravity wave drag parameters, the response to a polar cooling induces polar downwelling above the region of the imposed cooling, with consequent adiabatic warming. This response is robust to changes in the gravity wave source spectrum, background flow, gravity wave breaking criterion, and model lid height. When momentum is not conserved, either in the formulation or in the implementation of the gravity wave drag parameterization, the response becomes sensitive to the above-mentioned factors—in particular to the model lid height. The spurious response resulting from nonconservation is found to be nonnegligible in terms of the total gravity wave drag–induced downwelling.
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Radar refractivity retrievals can capture near-surface humidity changes, but noisy phase changes of the ground clutter returns limit the accuracy for both klystron- and magnetron-based systems. Observations with a C-band (5.6 cm) magnetron weather radar indicate that the correction for phase changes introduced by local oscillator frequency changes leads to refractivity errors no larger than 0.25 N units: equivalent to a relative humidity change of only 0.25% at 20°C. Requested stable local oscillator (STALO) frequency changes were accurate to 0.002 ppm based on laboratory measurements. More serious are the random phase change errors introduced when targets are not at the range-gate center and there are changes in the transmitter frequency (ΔfTx) or the refractivity (ΔN). Observations at C band with a 2-μs pulse show an additional 66° of phase change noise for a ΔfTx of 190 kHz (34 ppm); this allows the effect due to ΔN to be predicted. Even at S band with klystron transmitters, significant phase change noise should occur when a large ΔN develops relative to the reference period [e.g., ~55° when ΔN = 60 for the Next Generation Weather Radar (NEXRAD) radars]. At shorter wavelengths (e.g., C and X band) and with magnetron transmitters in particular, refractivity retrievals relative to an earlier reference period are even more difficult, and operational retrievals may be restricted to changes over shorter (e.g., hourly) periods of time. Target location errors can be reduced by using a shorter pulse or identified by a new technique making alternate measurements at two closely spaced frequencies, which could even be achieved with a dual–pulse repetition frequency (PRF) operation of a magnetron transmitter.
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The Confederate Veterans Association Catawba Camp No. 278 Records consist mainly of minutes, but also included are lists of members, newspaper clippings and resolutions of the Association which was organized in 1893 and based in Rock Hill, SC. The collection consists entirely of photocopies.
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Good morning! There's a lot of information I want to share with you in a short amount of time, so I'm going to get right to it.