Chicana, Indian and Sudanese Perspectives of Teaching in the Academy: Three Levels of Experience in the Teaching-Learning and Social Environment

“Women of color from any culture or country face additional barriers in predominantly white institutions. This panel presents perspectives and experiences of three women from three cultures and three different levels of academia—a Chicana Latino visiting professor, a graduate teaching assistant from India, and a Sudanese graduate research assistant.”

Impact of biannual rossby waves on the Indian Ocean Dipole

Topex/Poseidon sea surface height anomalies during 1993-2002 are decomposed using 2-D finite impulse response filters which showed biannual Rossby waves (BRWs) in the equatorial Indian Ocean (peak at 1.5 degrees S) and in the southern tropical Indian Ocean (peak at 10.5 degrees S) during Indian Ocean Dipole (IOD) years. Anomalous downwelling BRWs in the equatorial Indian Ocean triggered by the wind stress curl-induced Ekman pumping near the eastern boundary started propagating westward from the eastern boundary in July/August 1993 and 1996, i.e., more than one year prior to the formation of the IOD events of 1994 and 1997 respectively. These strong downwelling signals reach the western equatorial Indian Ocean during the peak dipole time.

Can Indian Ocean SST anomalies influence South American rainfall?

In this study we examine the impact of Indian Ocean sea surface temperature (SST) variability on South American circulation using observations and a suite of numerical experiments forced by a combination of Indian and Pacific SST anomalies. Previous studies have shown that the Indian Ocean Dipole (IOD) mode can affect climate over remote regions across the globe, including over South America. Here we show that such a link exists not only with the IOD, but also with the Indian Ocean basin-wide warming (IOBW). The IOBW, a response to El Nino events, tends to reinforce the South American anomalous circulation in March-to-May associated with the warm events in the Pacific. This leads to increased rainfall in the La Plata basin and decreased rainfall over the northern regions of the continent. In addition, the IOBW is suggested to be an important factor for modulating the persistence of dry conditions over northeastern South America during austral autumn. The link between the IOBW and South American climate occurs via alterations of the Walker circulation pattern and through a mid-latitude wave-train teleconnection.

A new local variety of Crepidomanes minutum (Hymenophyllaceae) in the Mascarene Archipelago (Indian Ocean) and a new record for Mauritius

Crepidomanes minutum (Hymenophyllaceae) is here identified and recorded from Mauritius for the first time. The Mauritian specimens, in addition to those of La Reunion observed at low to middle elevations, are easily distinguished from populations observed outside the Mascarene Archipelago by their dwarfed size and rarity of the stipe proliferation that usually characterizes this species. We thus describe a new variety in this species for the Mascarene Islands.

Wind-driven cross-equatorial flow in the Indian ocean

Máster en Oceanografía

Changes of the surface cell of the Atlantic and Indian Meridional overturning circulations

Premio Extraordinario de Doctorado. Rama de Ciencias.

The role of public opinions on recent Spanish emigration

[ES]Presentación de un informe sobre el debate social reflejado en los medios de comunicación españoles sobre el nuevo fenómeno de la emigración de jóvenes españoles al extranjero y su relación con la crisis económica internacional.

Changes of the surface cell of the Atlantic and Indian Meridional Overturning Circulations

Programa de doctorado en Oceanografía.

Magma injections and destabilization of basaltic volcanoes: a numerical study. Application to La Reunion (Indian ocean, France) and Stromboli (Tyrrhenian sea, Italy)

Most basaltic volcanoes are affected by recurrent lateral instabilities during their evolution. Numerous factors have been shown to be involved in the process of flank destabilization occurring over long periods of time or by instantaneous failures. However, the role of these factors on the mechanical behaviour and stability of volcanic edifices is poorly-constrained as lateral failure usually results from the combined effects of several parameters. Our study focuses on the morphological and structural comparison of two end-member basaltic systems, La Reunion (Indian ocean, France) and Stromboli (southern Tyrrhenian sea, Italy). We showed that despite major differences on their volumes and geodynamic settings, both systems present some similarities as they are characterized by an intense intrusive activity along well-developed rift zones and recurrent phenomena of flank collapse during their evolution. Among the factors of instability, the examples of la Reunion and Stromboli evidence the major contribution of intrusive complexes to volcano growth and destruction as attested by field observations and the monitoring of these active volcanoes. Classical models consider the relationship between vertical intrusions of magma and flank movements along a preexisting sliding surface. A set of published and new field data from Piton des Neiges volcano (La Reunion) allowed us to recognize the role of subhorizontal intrusions in the process of flank instability and to characterize the geometry of both subvertical and subhorizontal intrusions within basaltic edifices. This study compares the results of numerical modelling of the displacements associated with high-angle and low-angle intrusions within basaltic volcanoes. We use a Mixed Boundary Element Method to investigate the mechanical response of an edifice to the injection of magmatic intrusions in different stress fields. Our results indicate that the anisotropy of the stress field favours the slip along the intrusions due to cointrusive shear stress, generating flank-scale displacements of the edifice, especially in the case of subhorizontal intrusions, capable of triggering large-scale flank collapses on basaltic volcanoes. Applications of our theoretical results to real cases of flank displacements on basaltic volcanoes (such as the 2007 eruptive crisis at La Reunion and Stromboli) revealed that the previous model of subvertical intrusions-related collapse is a likely mechanism affecting small-scale steeply-sloping basaltic volcanoes like Stromboli. Furthermore, our field study combined to modelling results confirms the importance of shallow-dipping intrusions in the morpho-structural evolution of large gently-sloping basaltic volcanoes like Piton de la Fournaise, Etna and Kilauea, with particular regards to flank instability, which can cause catastrophic tsunamis.

Emigration als Herausforderung für Prozesse der Einbindung und Ablösung in Kindheit und Jugend: Eine Studie zu Identitätskonstruktionen von aus dem nationalsozialistischen Deutschland emigrierten Kindern und Jugendlichen

Ziel der vorliegenden Arbeit war die Untersuchung der Bedeutung des lebensgeschichtlichen Ereignisses (erzwungener) Emigration aus Deutschland zur Zeit des Nationalsozialismus für die Identitätsentwicklung von Kindern und Jugendlichen. Anhand der objektiv hermeneutischen Analyse und Interpretation lebensgeschichtlicher Interviews, objektiver Daten sowie z.T. weiterer (auto-)biographischer Materialien dreier Personen, die als Kinder in die USA emigrierten, wurde vor allem der Frage nachgegangen, welche Zusammenhänge herstellbar sind zwischen entwicklungsmäßig gewissermaßen ‚vorprogrammierten‘ Krisen der Bindung und Ablösung im Sozialisationsprozess und dem Ereignis Emigration als fallübergreifend vorliegender Besonderheit im Sinne eines potentiell traumatischen Krisenereignisses. Das zentrale Interesse bestand in der Rekonstruktion unterschiedlicher biographisch wirksamer Habitus der Krisenbewältigung. In heuristischer Absicht wurde dabei einerseits angeknüpft an das soziologisch strukturtheoretische Modell Ulrich Oevermanns von Sozialisation als Prozess der Krisenbewältigung, andererseits an Robert Kegans entwicklungspsychologisches Konzept der Entwicklung des Selbst in einbindenden Kulturen. Im Zuge der Fallrekonstruktionen ließen sich erstens von Fall zu Fall unterschiedliche Perspektiven auf die Erfahrung der Emigration herausarbeiten sowie zweitens jeweils spezifische Haltungen im Umgang mit (wie bewusst auch immer als solche wahrgenommenen) Entscheidungskrisen der Lebensgestaltung, also eine je eigene Form des Umgangs mit der für die menschliche Lebenspraxis konstitutiven widersprüchlichen Einheit von Entscheidungszwang und Begründungsverpflichtung. Die Ergebnisse verweisen zum einen auf den großen Einfluss familialer Sozialisation auf die Entwicklung, zeigen zum anderen aber auch die Bedeutsamkeit kultureller Einbindungsmöglichkeiten über die Lebensspanne auf. Sie bieten damit eine empirische Fundierung der Synthese des Oevermannschen und des Keganschen Modells.

Prokaryotic community structure in ultra-slow spreading Southwest Indian Ridge.

The Southwest Indian Ridge segment that extends between 10° and 16° E has the slowest spreading rate of any other oceanic ridge (about 8.4 mm/year). In 2013 during the expedition ANTXXIX/8 seismology, geology, microbiology, heat flow analyses were carried out. Here, no hydrothermal plumes or black smoker systems were found but the results of the survey allowed to identify areas with peculiar characteristics: Area 1 with higher heat flux bsf; Area 2 where in 2002 the presence of hydrothermal emissions was hypothesized (Bach et al., 2002); Area 3 with anomalies of methane, ammonium, sulphide and dissolved inorganic carbon in pore water sediment profiles, and recovery of fauna vents. All these aspects suggest the presence of a hydrothermal circulation. Using Illumina 16S gene tag, statistical tools and phylogenetic trees, I provided a biological proof of the presence of hydrothermal circulation in this ridge segment. At Area 3, alpha and beta diversity indexes showed similarities with those described for venting microbial communities and about 40-70% of the dominant microbial community was found phylogenetically related to clones isolated hydrothermal-driven environments. Although the majority of chemosynthetic environment related taxa were not classified like autotrophic prokaryotes, some of them are key taxa in support of the presence of hydrothermal circulation, since they are partners of consortia or mediate specific reaction typically described for hydrothermal and seep environments, or are specialized organisms in exploiting labile organic substrates. Concluding, these results are remarkable because support the importance of ultra slow spreading ridge systems in contributing to global geochemical cycles and larval dispersion of vent fauna.