De la fidelidad a la revolución: el proceso de la independencia de la antigua provincia de Guayaquil, 1809-1820 (Estudios)

Este articulo analiza las transformaciones políticas e ideológicas que tuvieron lugar en Guayaquil entre 1809 y 1820, período en el que la ciudad transitó de un marcado fidelismo hacia la autonomía e independencia. Se estudian las disputas entre los grupos de poder local y las reacciones del cabildo a las sucesivas coyunturas peninsulares y regionales. El ensayo muestra la relación entre las tensiones sociales internas y la dinámica, hasta ahora desconocida, de las diferentes elecciones ocurridas entre 1809 y 1813, as¡ como el impacto local de la vigencia y posterior supresión de la constitución gatidatana. El estudio concluye con una reconsideración de la independencia guayaquileña de 1820.

Habiendo roto el freno de la obediencia: participación indígena en la insurgencia de Quito, 1809-1812 (Estudios)

El artículo analiza un ámbito de la participación de los indígenas en la coyuntura de quiebre del régimen monárquico producida en Quito ante las noticias de la invasión napoleónica y la abdicación del trono español en favor de José Bonaparte. El trabajo investiga si los indígenas de Quito fueron fundamentalmente indiferentes ante la proclamación de autonomía de la primera junta quiteña en 1809 o si tuvieron alguna propuesta específica durante el período de mayor convulsión y movilización entre 1810 y 1812. De otro lado, explora las actitudes de la élite y la plebe en el período. El trabajo pone atención en el ambiente de temor que la movilización popular suscitó luego de los abusos y la cruenta represión cometidas por las tropas limeñas acantonadas en Quito, en 1810.

Los orígenes de la Revolución de Quito en 1809 (Debates)

La Revolución de Quito de 1809 no fue un movimiento por la independencia. Lejos de ello, se trató de una reacción local ante la crisis de la monarquía española. A lo largo del siglo XVIII, el Reino de Quito experimentó un declive económico, político y jurídico. Supeditado a las capitales de dos virreinatos –Lima y Santa Fe–, Quito buscaba el estatus de una capitanía general independiente con el fin de liberarse del dominio de Nueva Granada y Perú. Convencido de que España estaba perdida y de que los españoles en Quito traicionarían al reino y aceptarían el gobierno francés, un grupo de quiteños tomó el control del gobierno y puso en práctica un programa que garantizara la autonomía y que promoviera sus intereses económicos. No obstante, otras provincias del reino, cuyos intereses se vieron amenazados, se opusieron a Quito y unieron fuerzas con los virreyes de Perú y Nueva Granada para extinguir el levantamiento que duró unos tres meses.

The Influence of Body Condition on the Stopover Ecology of Least Sandpipers in the Lower Mississippi Alluvial Valley during Fall Migration

Many shorebirds are long-distance migrants and depend on the energy gained at stopover sites to complete migration. Competing hypotheses have described strategies used by migrating birds; the energy-selection hypothesis predicts that shorebirds attempt to maximize energy gained at stopover sites, whereas the time-selection hypothesis predicts that shorebirds attempt to minimize time spent at stopover sites. The energy- and time-selection hypotheses both predict that birds in better condition will depart sites sooner. However, numerous studies of stopover duration have found little support for this prediction, leading to the suggestion that migrating birds operate under energy and time constraints for only a small portion of the migratory season. During fall migration 2002, we tested the prediction that birds in better condition depart stopover sites sooner by examining the relationship between stopover duration and body condition for migrating Least Sandpipers (Calidris minutilla) at three stopover sites in the Lower Mississippi Alluvial Valley. We also tested the assumption made by the Lower Mississippi Alluvial Valley Migratory Bird Science Team that shorebirds stay in the Mississippi Valley for 10 d. The assumption of 10 d was used to estimate the amount of habitat required by shorebirds in the Mississippi Valley during fall migration; a period longer than 10 d would increase the estimate of the amount habitat required. We used multiple-day constancy models of apparent survival and program MARK to estimate stopover duration for 293 individually color-marked and resighted Least Sandpipers. We found that a four-day constancy interval and a site x quadratic time trend interaction term best modeled apparent survival. We found only weak support for body condition as a factor explaining length of stopover duration, which is consistent with findings from similar work. Stopover duration estimates were 4.1 d (95% CI = 2.8–6.1) for adult Least Sandpipers at Bald Knob National Wildlife Refuge, Arkansas, 6.5 d (95% CI = 4.9–8.7) for adult and 6.1 d (95% CI =4.2–9.1) for juvenile Least Sandpipers at Yazoo National Wildlife Refuge, Mississippi, and 6.9 d (95% CI = 5.5–8.7) for juvenile Least Sandpipers at Morgan Brake National Wildlife Refuge, Mississippi. Based on our estimates of stopover duration and the assumption made by the Lower Mississippi Alluvial Valley Migratory Bird Science Team, there is sufficient habitat in the lower Mississippi Valley to support shorebirds during fall migration.

The fall speeds of sub-100 mu m ice crystals

Estimates for the sedimentation rate of realistic ice crystals at sizes smaller than 100 µm are presented. These calculations, which exploit new results for the capacitance of ice crystals, are compared with laboratory studies and found to be in good agreement. The results highlight a weakness in contemporary ice particle fall speed parametrizations for very small crystals, which can lead to sedimentation rates being overestimated by a factor of two. The theoretical approach applied here may also be useful for calculating the sedimentation rate and mobility of non-spherical aerosol particles.

The rise and fall of open solar flux during the current grand solar maximum

We use geomagnetic activity data to study the rise and fall over the past century of the solar wind flow speed VSW, the interplanetary magnetic field strength B, and the open solar flux FS. Our estimates include allowance for the kinematic effect of longitudinal structure in the solar wind flow speed. As well as solar cycle variations, all three parameters show a long-term rise during the first half of the 20th century followed by peaks around 1955 and 1986 and then a recent decline. Cosmogenic isotope data reveal that this constitutes a grand maximum of solar activity which began in 1920, using the definition that such grand maxima are when 25-year averages of the heliospheric modulation potential exceeds 600 MV. Extrapolating the linear declines seen in all three parameters since 1985, yields predictions that the grand maximum will end in the years 2013, 2014, or 2027 using VSW, FS, or B, respectively. These estimates are consistent with predictions based on the probability distribution of the durations of past grand solar maxima seen in cosmogenic isotope data. The data contradict any suggestions of a floor to the open solar flux: we show that the solar minimum open solar flux, kinematically corrected to allow for the excess flux effect, has halved over the past two solar cycles.