948 resultados para Santa Barbara, California.
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EXTRACT (SEE PDF FOR FULL ABSTRACT): Recently, paleoceanographers have been challenged to produce reliable proxies of climate variables that can be incorporated into climate models. In developing proxies using time series of annual radiolarian species fluxes from Santa Barbara Basin, we identify groups of species associated with years of extreme sea surface temperatures and sea level heights.
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EXTRACT (SEE PDF FOR FULL ABSTRACT): A varve chronology with annual resolution (AD 1117-1992) has been developed recently for Santa Barbara Basin. Varve thickness and water content show an exponential trend consistent with expected patterns in the presence of sediment compaction over time. Annual varve thickness was decomposed into orthogonal components using singular spectrum analysis (SSA) to identify and retrieve inter-decadal oscillations. ... This suggests a connection with global-scale decadal cycles identified in the subtropical Pacific gyre circulation and, possibly, with solar-driven phenomena. The near-1600 AD event coincides with (a) a similarly sudden change of state in nearby Santa Monica Basin that triggered the onset of anoxic conditions and the preservation of laminated sediments, (b) an extreme drought over the American Southwest, (c) a transformation of the age structure in a number of forest populations throughout Arizona and New Mexico. Total organic carbon burial flux in Santa Barbara Basin varves also shows a marked change after AD 1600. A possible climatic link is proposed that involves pathways for moisture transport in the Southwest at decadal and longer time scales.
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It is discovered that SBA-15 (santa barbara amorphous) can provide the favorable microenvironments and optimal direct electron-transfer tunnels (DETT) of immobilizing cytochrome c (Cyt c) by the preferred orientation on it. A high-redox potential (254 mV vs. Ag/AgCl) was obtained on glassy carbon (GC) electrode modified by immobilizing Cyt c on rod-like SBA-15. With ultraviolet-visible (UV-vis), circular dichroism (CD), FTIR and cyclic voltammetry, it was demonstrated that immobilization made Cyt c exhibits stable and ideal electrochemical characteristics while the biological activity of immobilized Cyt c is retained as usual.
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Padget, Martin, 'Women in the West', In: 'The Making of the American West: People and Perspectives', (Santa Barbara, CA: ABC-Clio), pp.239-258, 2007 RAE2008
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Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Hidráulica
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F. 1-12v. Calendrier en français, à l’encre rouge et noire, où l’on remarque des formes dialectales picardes et plusieurs saints du Nord : « sainte Audegonde » (30 janvier) ; « le Candelier » (2 févr.) ; « ste Gertrude » (17 mars) ; « saint Quentin » (2 mai) ; « saint Ernoulx » [ep. Suessonensis] (16 août) ; « saint Bertin » (5 septembre) ; « saint Lambert » (17 septembre) ; « saint Franchois » (4 oct.) ; « saint Gillain » [mart. in Hannonia] (16 oct., Ghislain); « le jour st Estievene » (26 déc., rouge). Une deuxième main très cursive ajouté d’autres saints, dont « s. Amand » (6 févr.) ; « s. Waleri » (1er avril) ; « s. Fuscien » [mart. Ambianensis] (27 juin et 10 déc.) ; « s. Firmin » [mart. Ambianensis] (25 septembre) ; « s. Bavon » (1er oct.). F. 13v-17v. « ... hore sancte Crucis». F. 18v-22v. « ... hore de sancto Spiritu ».F. 23v-85. « ... hore beate marie virginis secundum usum romanum ». F. 86v-94v. Office de la Vierge, selon les temps de l’année. « ... officum beate Marie virginis quod dicitur per totum adventum ad vesperas ».F.95-115. « ... septem psalmi penitentiales cum suis litaniis et precibus ». A noter « ... sancte Lamberte... sancte Rumolde [ep. Mechlinensis]... sancte Fursee [ab. Latiniacensis] ... sancte Amande... sancte Vedaste, sancte Bavo... sancte Philiberte... santa Ursula... sancta Brigida... sancta Aldegondis, sancta Gertrudis... ».F.116v-152v. « ... vigilie mortuorum » office des morts à l’usage de Sarum-Normandie-Metz ; cf. K. Ottosen, Responsories..., p. 242 (116v-151). — « Octo versus beati Bernardi ». « Illumina oculos meos ne umquam obdormiam... » ; cf. Leroquais, Livres d’heures, I, XXX-XXXI (151-152v).F.153-158v. « Initium sancti evvangelii secundum Johannem... secundum Lucam... secundum Matheum... secundum Marcum ».F. 158v-166. Suffrages aux saints : « Memoria de santo Johanne Baptista... ; devota oratio... » ; — « ... de sancto Adriano » ; — « ... de sancto Sebastiano » ; — « ... de sancto Anthonio » ; — « ... de sancto Quintino » ; — « ... de sancto Nicholae » ; — « ... de sancto Andrea » ; — « ... de sancto Fiacro ».F.166v-174v. Prières à la Vierge. « ... devotissima oratio ad beatem virginem Mariam ». « O intemerata... O Johannes... » (éd. Wilmart, Auteurs spirituels, 488-490) (166v-169v). — « Alia oratio ad beatam virginem Mariam ». « Obsecro te.... » (éd. Leroquais, Livres d’heures, II, 346-347) (169v-174). Les deux prières sont rédigées à la forme masculine. — « Laus Marie virginis ». « Salve regina... » (Analecta Hymnica, L, 318-319, n° 245) (174-174v). F. 175-184v. Suffrages aux saintes : « ... de santa Barbara » ; — « ... de sancta Margareta » ; — « ... de sancta Katerina » ; — « ... de sancta Maria Magdelena » ; — « ... de sancta Appolonia » ; — « ... de sancta Venicie [Venice, forme dérivée de Véronique] » « Veni sponsa Christi... Versus. Diffusa est gratia... Oratio. Exaudi nos Deus ut sicut de beate Venicie festivitate gaudemus, ita pie devotionis erudiamur. Per.... » ; sur le culte de sainte Véronique/Venice, en particulier à Paris, voir Gr. A. RUNNALS, Le mystère de sainte Venice, Exeter, 1980 (Textes littéraires) (175-180v). — Prières diverses : « ... quinque gaudia de beata virgine Maria » « Gaude Virgo mater Christi... » (éd. Leroquais, Livres d’heures, I, XXVI-XXVII) (180v-182). — « Oratio devota ad Jesum Christum ». « Ave domine Jhesu Christe verbum patris » (éd. Wilmart, Auteurs spirituels, 412 [III]) (182-183). — « Oratio devota que dicitur ad elevationem Domini ». « Ave verum corpus Domini nostri... » (éd. Szövérffy, Die Annalen , II, 298-299) (183-184). — « Memore de saint Miquiel », en latin (184-184v).
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La política exterior China es una consecuencia de la globalización que puede ser aprovechada por países en vías de desarrollo a través de lazos comerciales se pueden construir relaciones de cooperación, como estrategia que permita afianzar relaciones
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Introducción: En la literatura, han aparecido reportes de neoplasia escamosa de superficie ocular (NESO) asociado con pterigio en un mismo paciente. Sin embargo, Colombia no cuenta con una estadística para ninguna de estas patologías. Objetivos: Determinar la frecuencia de NESO en pterigios resecados, en la Fundación Oftalmológica Nacional. Identificar factores de riesgo y características clínicas que predispongan a su aparición. Metodología: Estudio descriptivo de corte transversal. Se realizó una clasificación prequirúrgica y estudio histopatológico de los pterigios resecados en 93 pacientes, para confirmar su coexistencia con NESO. Se efectuó un análisis de frecuencias para datos demográficos y factores de riesgo asociados su aparición. Resultados: La frecuencia de NESO asociado a pterigio fue 7,07%. De estos, 28,5% identificados como sospechosos en la evaluación preoperatoria. La mayoría se presentaron en mujeres (71,4%), las ocupaciones con mayor frecuencia: labores domésticas (42,8%) y el comercio (28.5%). La exposición a derivados del petróleo y tabaquismo fue del 14,28%. No se presentaron casos asociados a infección por VIH. No hubo diferencias estadísticamente significativas sobre la presencia de NESO al comparar los casos en edad (p=0,8), procedencia (p=0,6) tabaquismo (p=0,4), leucoplaquia (p=1,0), queratinización (p=0,137), o vasos amputados (p=0,137). Conclusiones: De los pacientes con diagnóstico histopatológico de NESO, un porcentaje mínimo es sospechado clínicamente. Además se encontró este diagnóstico en pacientes más jóvenes que lo reportado en la literatura. Se recomienda realizar estudios con mayor número de pacientes para una mejor identificación de factores de riesgo. Palabras clave:
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Atmospheric downwelling longwave radiation is an important component of the terrestrial energy budget; since it is strongly related with the greenhouse effect, it remarkably affects the climate. In this study, I evaluate the estimation of the downwelling longwave irradiance at the terrestrial surface for cloudless and overcast conditions using a one-dimensional radiative transfer model (RTM), specifically the Santa Barbara DISORT Atmospheric Radiative Transfer (SBDART). The calculations performed by using this model were compared with pyrgeometer measurements at three different European places: Girona (NE of the Iberian Peninsula), Payerne (in the East of Switzerland), and Heselbach (in the Black Forest, Germany). Several studies of sensitivity based on the radiative transfer model have shown that special attention on the input of temperature and water content profiles must be held for cloudless sky conditions; for overcast conditions, similar sensitivity studies have shown that, besides the atmospheric profiles, the cloud base height is very relevant, at least for optically thick clouds. Also, the estimation of DLR in places where radiosoundings are not available is explored, either by using the atmospheric profiles spatially interpolated from the gridded analysis data provided by European Centre of Medium-Range Weather Forecast (ECMWF), or by applying a real radiosounding of a nearby site. Calculations have been compared with measurements at all sites. During cloudless sky conditions, when radiosoundings were available, calculations show differences with measurements of -2.7 ± 3.4 Wm-2 (Payerne). While no in situ radiosoundings are available, differences between modeling and measurements were about 0.3 ± 9.4 Wm-2 (Girona). During overcast sky conditions, when in situ radiosoundings and cloud properties (derived from an algorithm that uses spectral infrared and microwave ground based measurements) were available (Black Forest), calculations show differences with measurements of -0.28 ± 2.52 Wm2. When using atmospheric profiles from the ECMWF and fixed values of liquid water path and droplet effective radius (Girona) calculations show differences with measurements of 4.0 ± 2.5 Wm2. For all analyzed sky conditions, it has been confirmed that estimations from radiative transfer modeling are remarkably better than those obtained by simple parameterizations of atmospheric emissivity.