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Cover title.

Adventures and Misfortunes in Macondo: Rehabilitation of the Cienaga Grande

We describe trajectories of selected ecological indicators used as performance measures to evaluate the success of a mangrove rehabilitation project in the Ciénaga Grande de Santa Marta (CGSM) Delta-Lagoon complex, Colombia, as result of freshwater diversions initiated in 1995. There is a significant reduction in soil and water column salinity in all sampling stations following the hydraulic reconnection of the Clarín and Aguas Negras channels to the Magdalena River. Soil intersticial water salinity (depth: 0.5 m) (7 stations) and water column salinity (0.5 m) (10 stations) values declined significantly (soil <30 g kg-1; water <10 g kg-1) from 1994 to 2000. During 1994 soil interstitial water salinity ranged from 40 g kg-1 (Rinconada) to 100 g kg-1 (KM 13), while water column salinity fluctuated between 25-35 g kg-1 for most of the sampling stations. This salinity reduction increased mangrove forest regeneration promoting a net gain of 99 km2 from 1995 to 1999. The high precipitation recorded in 1995 and 1999 caused by El Niño-La Niña (ENSO), coinciding with the channels rehabilitation, influenced rapid mangrove regeneration. The lack of economic investment in the maintenance of the diversion structures from 2001 to 2004 caused a salinity increase affecting negatively already restored vegetation. A sustainable effort from the international community and the Colombian government is needed to maintain the strategic social and economic benefits reached until 2000 in the CGSM region.

Discharge measurements and storm event chemistry at the San Francisco River station (Planta) in 2007-2008

To improve our knowledge of the influence of land-use on solute behaviour and export rates in neotropical montane catchments we investigated total organic carbon (TOC), Ca, Mg, Na, K, NO3 and SO4 concentrations during April 2007-May 2008 at different flow conditions and over time in six forested and pasture-dominated headwaters (0.7-76 km2) in Ecuador. NO3 and SO4 concentrations decreased during the study period, with a continual decrease in NO3 and an abrupt decrease in February 2008 for SO4. We attribute this to changing weather regimes connected to a weakening La Niña event. Stream Na concentration decreased in all catchments, and Mg and Ca concentration decreased in all but the forested catchments during storm flow. Under all land-uses TOC increased at high flows. The differences in solute behaviour during storm flow might be attributed to largely shallow subsurface and surface flow paths in pasture streams on the one hand, and a predominant origin of storm flow from the organic layer in the forested streams on the other hand. Nutrient export rates in the forested streams were comparable to the values found in literature for tropical streams. They amounted to 6-8 kg/ha/y for Ca, 7-8 kg/ha/y for K, 4-5 kg/ha/y for Mg, 11-14 kg/ha/y for Na, 19-22 kg/ha/y for NO3 (i.e. 4.3-5.0 kg/ha/y NO3-N) and 17 kg/ha/y for SO4. Our data contradict the assumption that nutrient export increases with the loss of forest cover. For NO3 we observed a positive correlation of export value and percentage forest cover.

Dinâmica das configurações de formação e inibição das chuvas no Rio Grande do Norte: caracterização hidroclimática do estado

This study aimed to evaluate the influence of the main meteorological mechanisms trainers and inhibitors of precipitation, and the interactions between different scales of operation, the spatial and temporal variability of the annual cycle of precipitation in the Rio Grande do Norte. Além disso, considerando as circunstâncias locais e regionais, criando assim uma base científica para apoiar ações futuras na gestão da demanda de água no Estado. Database from monthly precipitation of 45 years, ranging between 1963 and 2007, data provided by EMPARN. The methodology used to achieve the results was initially composed of descriptive statistical analysis of historical data to prove the stability of the series, were applied after, geostatistics tool for plotting maps of the variables, within the geostatistical we opted for by Kriging interpolation method because it was the method that showed the best results and minor errors. Among the results, we highlight the annual cycle of rainfall the State which is influenced by meteorological mechanisms of different spatial and temporal scales, where the main mechanisms cycle modulators are the Conference Intertropical Zone (ITCZ) acting since midFebruary to mid May throughout the state, waves Leste (OL), Lines of instability (LI), breeze systems and orographic rainfall acting mainly in the Coastal strip between February and July. Along with vortice of high levels (VCANs), Complex Mesoscale Convective (CCMs) and orographic rain in any region of the state mainly in spring and summer. In terms of larger scale phenomena stood out El Niño and La Niña, ENSO in the tropical Pacific basin. In La Niña episodes usually occur normal or rainy years, as upon the occurrence of prolonged periods of drought are influenced by EL NIÑO. In the Atlantic Ocean the standard Dipole also affects the intensity of the rainfall cycle in State. The cycle of rains in Rio Grande do Norte is divided into two periods, one comprising the regions West, Central and the Western Portion of the Wasteland Potiguar mesoregions of west Chapada Borborema, causing rains from midFebruary to mid-May and a second period of cycle, between February-July, where rains occur in mesoregions East and of the Wasteland, located upwind of the Chapada Borborema, both interspersed with dry periods without occurrence of significant rainfall and transition periods of rainy - dry and dry-rainy where isolated rainfall occur. Approximately 82% of the rainfall stations of the state which corresponds to 83.4% of the total area of Rio Grande do Norte, do not record annual volumes above 900 mm. Because the water supply of the State be maintained by small reservoirs already are in an advanced state of eutrophication, when the rains occur, act to wash and replace the water in the reservoirs, improving the quality of these, reducing the eutrophication process. When rain they do not significantly occur or after long periods of shortages, the process of eutrophication and deterioration of water in dams increased significantly. Through knowledge of the behavior of the annual cycle of rainfall can have an intimate knowledge of how it may be the tendency of rainy or prone to shortages following period, mainly observing the trends of larger scale phenomena

A criança com paralisia cerebral na educação infantil: um olhar sobre a prática docente

La inclusión de los niños con discapacidad en la educación infantil, además de ser un tema poco planteado en la comunidad científica, es un reto actual en lo que se refiere a la práctica docente. Basándose en este aspecto, nuestro objetivo en esta investigación realizada, que resultó en la elaboración de este trabajo, fue analizar cómo se procesa la práctica docente con vistas a la inclusión escolar de un niño con parálisis cerebral, en un Centro Municipal de Educación Infantil (CMEI), en la ciudad de Natal / RN. Más específicamente, buscamos: reflexionar sobre la práctica de la profesora responsable por la clase, en lo que se refiere al desarrollo del niño con parálisis cerebral; analizar las interacciones entre educador y niño con parálisis cerebral; observar la práctica docente en la perspectiva de favorecer la interacción entre el niño con parálisis cerebral y otros niños. Para ello, realizamos una pesquisa exploratoria, cualitativa, y así que optamos por el método del Estudio de Caso. Utilizamos como procedimientos metodológicos el análisis documental, la investigación bibliográfica, la entrevista semiestructurada, la observación y la filmación de escenas relacionadas a la práctica docente. Los sujetos de la investigación fueron la profesora y el niño con parálisis cerebral. Los datos construidos durante la investigación señalaron el hecho de que la práctica de la profesora no estaba encaminada a las necesidades específicas de la alumna con parálisis cerebral, todavía, se desarrollaba de una manera similar para todos los niños en la clase. La presencia de limitaciones significativas para la inclusión de la niña con parálisis cerebral en la educación infantil puede ser considerado como el resultado de la ausencia de una adecuada preparación docente, tanto en el nivel de la formación inicial, cuanto de una formación continua y también la escasez de directrices para el maestro, en proceso; directrices estas acerca de la educación de los niños con parálisis cerebral, lo que hacía imposible a la profesora contribuir de manera efectiva a su mayor desarrollo cognitivo y social.

Um estudo sobre a variabilidade do vento no nordeste do Brasil através de métodos estatísticos e via modelos dinâmicos de meso e micro escala

The objective of this study was to determine the seasonal and interannual variability and calculate the trends of wind speed in NEB and then validate the mesoscale numerical model for after engage with the microscale numerical model in order to get the wind resource at some locations in the NEB. For this we use two data sets of wind speed (weather stations and anemometric towers) and two dynamic models; one of mesoscale and another of microscale. We use statistical tools to evaluate and validate the data obtained. The simulations of the dynamic mesoscale model were made using data assimilation methods (Newtonian Relaxation and Kalman filter). The main results show: (i) Five homogeneous groups of wind speed in the NEB with higher values in winter and spring and with lower in summer and fall; (ii) The interannual variability of the wind speed in some groups stood out with higher values; (iii) The large-scale circulation modified by the El Niño and La Niña intensified wind speed for the groups with higher values; (iv) The trend analysis showed more significant negative values for G3, G4 and G5 in all seasons and in the annual average; (v) The performance of dynamic mesoscale model showed smaller errors in the locations Paracuru and São João and major errors were observed in Triunfo; (vi) Application of the Kalman filter significantly reduce the systematic errors shown in the simulations of the dynamic mesoscale model; (vii) The wind resource indicate that Paracuru and Triunfo are favorable areas for the generation of energy, and the coupling technique after validation showed better results for Paracuru. We conclude that the objective was achieved, making it possible to identify trends in homogeneous groups of wind behavior, and to evaluate the quality of both simulations with the dynamic model of mesoscale and microscale to answer questions as necessary before planning research projects in Wind-Energy area in the NEB

(Appendix A) Radiolarian abundance in ODP Hole 202-1241A

A quantitative radiolarian study at Ocean Drilling Program Site 1241 in the eastern tropical Pacific enables us to reconstruct paleoceanographic changes that occurred since the latest middle Miocene. Today, this site is located just under the Eastern Pacific Warm Pool (EPWP). Based on the abundance variations of radiolarian characteristic species which are indicators of upwelling and thermocline changes, it is suggested that three notable changes occurred at 10.6, 9.8, and 4.2 Ma in the region. Four distinct periods of oceanographic conditions bounded by these notable changes were characterized on the basis of the following: (1) stratified seawater (12.0 to 10.6 Ma); (2) a shallowing of the thermocline and an increasing of upwelling (10.6 to 9.8 Ma); (3) significant inflow of warm water to the eastern tropical Pacific caused by an intensified Northern Equatorial Countercurrent (NECC), resulting in the formation of EPWP (9.8 to 4.2 Ma); and (4) the reduction of the EPWP and the NECC, and an increase in upwelling (4.2 to 0 Ma). The timing of these paleoceanographic events indicated the strong relations with the opening and closing of the Indonesian and Central American (Panama) Seaways. The reduction of the EPWP (this study) and the deepening of the thermocline in western Pacific at about 4.2 Ma (Cannariato and Ravelo, 1997; Chaisson and Ravelo, 2000) indicated a change from a state resembling El Niño in the late Miocene and the early Pliocene time to a state resembling La Niña by the late Pliocene

(Table 2) Seasonal flux data and percentages of major bulk components of total flux at the mesotrophic sediment trap site CB from 1988 - 2012

A more than two-decadal sediment trap record from the Eastern Boundary Upwelling Ecosystem (EBUE) off Cape Blanc, Mauritania, is analysed with respect to deep ocean mass fluxes, flux components and their variability on seasonal to decadal timescales. The total mass flux revealed interannual fluctuations which were superimposed by fluctuations on decadal timescales. High winter fluxes of biogenic silica (BSi), used as a measure of marine production (mostly by diatoms) largely correspond to a positive North Atlantic Oscillation (NAO) index (December-March). However, this relationship is weak. The highest positive BSi anomaly was in winter 2004-2005 when the NAO was in a neutral state. More episodic BSi sedimentation events occurred in several summer seasons between 2001 and 2005, when the previous winter NAO was neutral or even negative. We suggest that distinct dust outbreaks and deposition in the surface ocean in winter and occasionally in summer/autumn enhanced particle sedimentation and carbon export on short timescales via the ballasting effect. Episodic perturbations of the marine carbon cycle by dust outbreaks (e.g. in 2005) might have weakened the relationships between fluxes and large-scale climatic oscillations. As phytoplankton biomass is high throughout the year, any dry (in winter) or wet (in summer) deposition of fine-grained dust particles is assumed to enhance the efficiency of the biological pump by incorporating dust into dense and fast settling organic-rich aggregates. A good correspondence between BSi and dust fluxes was observed for the dusty year 2005, following a period of rather dry conditions in the Sahara/Sahel region. Large changes of all bulk fluxes occurred during the strongest El Niño-Southern Oscillation (ENSO) in 1997-1999 where low fluxes were obtained for almost 1 year during the warm El Niño and high fluxes in the following cold La Niña phase. For decadal timescales, Bakun (1990) suggested an intensification of coastal upwelling due to increased winds (''Bakun upwelling intensification hypothesis''; Cropper et al., 2014) and global climate change. We did not observe an increase of any flux component off Cape Blanc during the past 2 and a half decades which might support this. Furthermore, fluxes of mineral dust did not show any positive or negative trends over time which might suggest enhanced desertification or ''Saharan greening'' during the last few decades.

"Amor de don Perlimplín con Belisa en su jardín": una obra teatral satírica

El componente satírico es una constante en el teatro de Federico García Lorca, en el que coexisten, en mayor o menor medida, dependiendo de la obra en cuestión, lo cómico y lo serio, ambas vertientes intrínsecas a la sátira. Dicha combinación, así como el innegable aspecto crítico, inherente a la obra lorquiana, identifican a este autor con la figura del satírico. García Lorca lleva a cabo su crítica sirviéndose del humor, que oscila entre lo puramente jocoso y el humor negro, y se manifiesta mediante el empleo de técnicas tradicionales de la sátira, con idéntico propósito al del satírico: degradar a su objeto de ataque suscitando sonrisa o repulsa. Este artículo analiza en clave de sátira Amor de don Perlimplín con Belisa en su jardín, identificando el objeto de ataque de la sátira lorquiana en esta obra y las técnicas satíricas empleadas por su autor.

El Índice Térmico Costero Peruano (ITCP)

El Ecosistema de Afloramiento Peruano (EAP) es una de las zonas marinas con mayor productividad pesquera en el mundo y por su ubicación geográfica, es afectada por procesos físicos remotos, principalmente por la variabilidad climática interanual proveniente del océano Pacifico Ecuatorial, cuya señal dominante es El Niño y la Oscilación Sur (ENOS). Con el fin de evaluar los efectos de ENOS frente al Perú, se desarrolló el Índice Térmico Costero Peruano (ITCP) que representa el 87,7% de la variación total de las anomalías de la temperatura superficial del mar del EAP. Se analizó el periodo 1982-2014, detectándose 12 periodos con condiciones cálidas y 16 con condiciones frías. El ITCP tuvo una tendencia lineal, un componente de bajas frecuencias y un componente de ruido, con 1,5%, 94,5 % y 4 % de contribución a la varianza total, respectivamente. El ITCP presenta ventajas respecto a otros índices climáticos de la costa peruana, porque comprende el área representativa del Ecosistema de Afloramiento Peruano y porque captura la señal del afloramiento costero así como de los efectos térmicos de El Niño y La Niña.

Impactos multifactoriales del cambio climático en Nicaragua y estrategias de adaptación

En Nicaragua, el cambio climático está asociado al fenómeno de El Niño y La Niña, que en situaciones extremas tienen efectos económicos, sociales y ambientales fatales. El fenómeno de El Niño es una condición anómala en la temperatura del océano pacifico tropical del este. Ocurre cuando el agua del océano pacifico ecuatorial se hace más caliente que el promedio (1°C - 3°C).Cuando esto sucede, la atmosfera encima del océano también reacciona. Ese cambio de temperatura afecta la circulación del viento reduciendo considerablemente las lluvias(Cruz Roja Nicaragüense, 2014). Este calentamiento de las aguas sucede cada dos o siete años y puede durar entre 12 y 18 meses. Según los cambios en el clima así se comporta ElNiño y puede ser clasificado como débil o moderado, pero también como fuerte o muy fuerte, en estos últimos casos provocando sequías extremas. Cuando estas aguas se enfrían sucede lo contrario, llueve mucho y hay inundaciones, y se le llama La Niña. Los huracanes más destructivos ocurren en periodos de La Niña, observados en el océano atlántico, Mar Caribe y Golfo de México. Estos favorecen epidemias transmitidas por el mosquito Aedes aegyti, como el dengue, la malaria y recientemente el Chikungunya, así como la leptospirosis (enfermedad bacteriana que se trasmite por consumo de agua y alimentos contaminados con orina de roedores), deslizamientos de tierra, pérdidas humanas, pérdidas de la infraestructura social y productiva, tanto pública como privada (escuelas, caminos,carreteras, puentes, viviendas, cercados, corrales, etc.).En síntesis, fenómenos extremos de El Niño o La Niña provocan un fuerte deterioro de los medios de vida de la población de las zonas afectadas, que dependen de los recursos agua, suelo, bosque y del clima.

Fenómeno del Niño historia y perspectivas

Ecuador se ubica en zona de riesgo para la llegada del Fenómeno del Niño, por lo que es necesario estar informados sobre este tema y diferenciar que es la Corriente del Niño (corriente cálida del Pacífico Sudamericano) y el Niño-Oscilación del Sur (patrón climático en el que se producen oscilaciones de la temperatura en dos fases: el Fenómeno del Niño y La Niña). En los años 1997-1998 este fenómeno afectó el 60% del total de la población, con un impacto muy alto en la salud de la ciudadanía, así como en la propiedad pública privada y en diversos ecosistemas. Ante la amenaza en el periodo 2015-2016, la Secretaría de Gestión de Riesgos (SGR) planificó tres etapas de acción: Preparación, Respuesta y Rehabilitación. Luego de la revisión los autores recomiendan entre otras cosas: brindar información oportuna sobre los cambios meteorológicos, informar sobre los planes de contingencia, garantizar la seguridad alimentaria y el acceso al agua; y fortalecer la atención integral que proveen los Servicios de Salud

Climate variability of the last 1000 years in the NW Pacific: high resolution, multi-biomarker records from Lake Toyoni

The East Asian Monsoon (EAM) is an active component of the global climate system and has a profound social and economic impact in East Asia and its surrounding countries. Its impact on regional hydrological processes may influence society through industrial water supplies, food productivity and energy use. In order to predict future rates of climate change, reliable and accurate reconstructions of regional temperature and rainfall are required from all over the world to test climate models and better predict future climate variability. Hokkaido is a region which has limited palaeo-climate data and is sensitive to climate change. Instrumental data show that the climate in Hokkaido is influenced by the East Asian Monsoon (EAM), however, instrumental data is limited to the past ~150 years. Therefore down-core climate reconstructions, prior to instrumental records, are required to provide a better understanding of the long-term behaviour of the climate drivers (e.g. the EAM, Westerlies, and teleconnections) in this region. The present study develops multi-proxy reconstructions to determine past climatic and hydrologic variability in Japan over the past 1000 years and aid in understanding the effects of the EAM and the Westerlies independently and interactively. A 250-cm long sediment core from Lake Toyoni, Hokkaido was retrieved to investigate terrestrial and aquatic input, lake temperature and hydrological changes over the past 1000-years within Lake Toyoni and its catchment using X-Ray Fluorescence (XRF) data, alkenone palaeothermometry, the molecular and hydrogen isotopic composition of higher plant waxes (δD(HPW)). Here, we conducted the first survey for alkenone biomarkers in eight lakes in the Hokkaido, Japan. We detected the occurrence of alkenones within the sediments of Lake Toyoni. We present the first lacustrine alkenone record from Japan, including genetic analysis of the alkenone producer. C37 alkenone concentrations in surface sediments are 18µg C37 g−1 of dry sediment and the dominant alkenone is C37:4. 18S rDNA analysis revealed the presence of a single alkenone producer in Lake Toyoni and thus a single calibration is used for reconstructing lake temperature based on alkenone unsaturation patterns. Temperature reconstructions over the past 1000 years suggest that lake water temperatures varies between 8 and 19°C which is in line with water temperature changes observed in the modern Lake Toyoni. The alkenone-based temperature reconstruction provides evidence for the variability of the EAM over the past 1000 years. The δD(HPW) suggest that the large fluctuations (∼40‰) represent changes in temperature and source precipitation in this region, which is ultimately controlled by the EAM system and therefore a proxy for the EAM system. In order to complement the biomarker reconstructions, the XRF data strengthen the lake temperature and hydrological reconstructions by providing information on past productivity, which is controlled by the East Asian Summer monsoon (EASM) and wind input into Lake Toyoni, which is controlled by the East Asian Winter Monsoon (EAWM) and the Westerlies. By combining the data generated from XRF, alkenone palaeothermometry and the δD(HPW) reconstructions, we provide valuable information on the EAM and the Westerlies, including; the timing of intensification and weakening, the teleconnections influencing them and the relationship between them. During the Medieval Warm Period (MWP), we find that the EASM dominated and the EAWM was suppressed, whereas, during the Little Ice Age (LIA), the influence of the EAWM dominated with time periods of increased EASM and Westerlies intensification. The El Niño Southern Oscillation (ENSO) significantly influenced the EAM; a strong EASM occurred during El Niño conditions and a strong EAWM occurred during La Niña. The North Atlantic Oscillation, on the other hand, was a key driver of the Westerlies intensification; strengthening of the Westerlies during a positive NAO phase and weakening of the Westerlies during a negative NAO phase. A key finding from this study is that our data support an anti-phase relationship between the EASM and the EAWM (e.g. the intensification of the EASM and weakening of the EAWM and vice versa) and that the EAWM and the Westerlies vary independently from each other, rather than coincide as previously suggested in other studies.

Educational Inclusion in the Regular Classroom: an Asperger Syndrome Case

The following paper resulted from the final research project conducted for my Master’s Degree in Teacher Training for Teachers of Primary Education (1st – 6th grade of the Basic General Education). This research project was conducted under the supervision of the Rural Education Division of the Center for Research and Teaching in Education (CIDE-UNA, Spanish acronym), in coordination with the Central America Educational and Cultural Coordination (CECC). The research is qualitative with an interpretative approach. Our main objective was to analyze the process of inclusive education in the regular classroom for a person with Asperger’s Syndrome, defined as a type of social impairment. The case study method was used in this research, as it allows a deeper study. A girl was chosen from a public school in an urban area of San José, Costa Rica. Three techniques were used to obtain information: interviews, questionnaires and documentation (personal file, behavior record, and psychological assessment) related to the girl with Asperger. The triangulation of sources was used as a method of analysis. The conclusion of the project was that regular schools may have children miss-diagnosed with Asperger’s Syndrome, and that our schools are still far from achieving inclusive education, but efforts are being made to achieve it. For a more opportune intervention, some recommendations based on this study were provided to the family and the school of the girl with Asperger.