Strategies for Solving Addition Problems Using Modified Schema-Based Instruction in Students with Intellectual Disabilities

A study is presented on the strategies employed to solve additive change problems by three students with intellectual disabilities (two of them with autism spectrum disorder). The students followed a program involving modified schema-based instruction. The results show an improvement in the problem-solving skills of the three students, who achieved successful formal strategies associated with identifying the operation. We analyze the importance of adapting and/or emphasizing certain steps in the instruction process in order to tailor them to the difficulties of each student

Teaching students with mild intellectual disability to solve word problems using schema-based instruction

This study, which used a multiple baseline across participants design, examines the effectiveness of a modified schema-based instructional approach to improve the mathematical word problem solving performance of three students with mild intellectual disability, two of whom had an autism spectrum disorder. Following the intervention, the three students improved their performance when solving addition and subtraction change word problems; however, their performance was inconsistent on change word problems. The effects of the instruction were generalized to two-step addition and subtraction word problems for the three participants. Moreover, the results were generalized to an untrained setting and were maintained 8 weeks after the instruction. The implications of these findings for teaching problem-solving skills to students with intellectual disability are discussed.This work was supported by the Ministerio de Economía y Competitividad. Madrid. Spain. Projects EDU2017-84276-R, PID2019-105677RB-I0

Ocean dynamics shapes the structure and timing of Atlantic Equatorial Modes

A recent study has brought to light the co‐existence of two distinct Atlantic Equatorial Modes during negative phases of the Atlantic Multidecadal Variability: the Atlantic Niño and Horse‐Shoe (HS) mode. Nevertheless, the associated air‐sea interactions for HS mode have not been explored so far and the prevailing dynamic view of the Atlantic Niño has been questioned. Here, using a forced ocean model simulation, we find that for both modes, ocean dynamics is essential to explain the equatorial SST variations, while air‐sea fluxes control the off‐equatorial SST anomalies. Moreover, we demonstrate the key role played by ocean waves in shaping their distinct structure and timing. For the positive phase of both Atlantic Niño and HS, anomalous westerly winds trigger a set of equatorial downwelling Kelvin waves (KW) during spring‐summer. These dKWs deepen the thermocline, favouring the equatorial warming through vertical diffusion and horizontal advection. Remarkably, for the HS, an anomalous north‐equatorial wind stress curl excites an upwelling Rossby wave (RW), which propagates westward and is reflected at the western boundary becoming an equatorial upwelling KW. The uKW propagates to the east, activating the thermocline feedbacks responsible to cool the sea surface during summer months. This RW‐reflected mechanism acts as a negative feedback causing the early termination of the HS mode. Our results provide an improvement in the understanding of the TAV modes and emphasize the importance of ocean wave activity to modulate the equatorial SST variability. These findings could be very useful to improve the prediction of the Equatorial Modes

ENSO coupling to the equatorial Atlantic: analysis with an extended improved recharge oscillator model

© 2023 Crespo-Miguel, Polo, Mechoso, Rodríguez-Fonseca and Cao-García. Weacknowledge Javier Jarillo and Lander R. Crespo for their help during the early stages of manuscript writing. We acknowledge the World Climate Research Programme’s Working Group on Coupled Modeling, responsible for CMIP, and we thank the climate modeling groups for producing and making available their model output. This work was financially supported by 817578 TRIATLAS project of the Horizon 2020 Programme (EU) and RTI2018095802-B-I00 and PID2021-125806NB-I00 of Ministerio de Economía y Competitividad (Spain), Fondo Europeo de Desarrollo Regional (FEDER, EU), the European Union Seventh Framework Programme (EU-FP7/2007–2013) PREFACE (Grant Agreement No. 603521), the ERC STERCP project (grant 648982), the ARC Centre of Excellence in Climate Extremes (CE170100023) and the Spanish project (CGL201786415-R).Introduction: Observational and modeling studies have examined the interactions between El Niño-Southern Oscillation (ENSO) and the equatorial Atlantic variability as incorporated into the classical charge-recharge oscillator model of ENSO. These studies included the role of the Atlantic in the predictability of ENSO but assumed stationarity in the relationships, i.e., that models’ coefficients do not change overtime. Arecentworkbytheauthors has challenged the stationarity assumption in the ENSO framework but without considering the equatorial Atlantic influence on ENSO. Methods: The present paper addresses the changing relationship between ENSO and the Atlantic El Niño using an extended version of the recharge oscillator model. The classical two-variable model of ENSO is extended by adding a linear coupling on the SST anomalies in the equatorial Atlantic. The model’s coefficients are computed for different periods. This calculation is done using two methods tofitthemodel tothe data: (1) the traditional method (ReOsc), and (2) a novel method (ReOsc+) based on fitting the Fisher’s Z transform of the auto and cross-correlation functions. Results: Weshowthat, duringthe 20th century, the characteristic dampingrate of the SST and thermocline depth anomalies in the Pacific have decreased in time by a factor of 2 and 3, respectively. Moreover, the damping time of the ENSO fluctuations has doubled from 10 to 20 months, and the oscillation period of ENSO has decreased from 60-70 months before the 1960s to 50 months afterward. These two changes have contributed to enhancing ENSO amplitude. The results also show that correlations between ENSO and the Atlantic SST strengthened after the 70s and the way in which the impact of the equatorial Atlantic is added to the internal ENSO variability. Conclusions: The remote effects of the equatorial Atlantic on ENSO must be considered in studies of ENSO dynamics and predictability during specific time-periods. Our results provide further insight into the evolution of the ENSO dynamics anditscoupling to the equatorial Atlantic, as well as an improved tool to study the coupling of climatic and ecological variables.Depto. de Estructura de la Materia, Física Térmica y ElectrónicaDepto. de Física de la Tierra y AstrofísicaFac. de Ciencias FísicasTRUEHorizon 2020 Programme (EU)Ministerio de Economía y CompetitividadFondo Europeo de Desarrollo Regional (FEDER, EU)European Union Seventh Framework ProgrammeERC STERCP projectARC Centre of Excellence in Climate ExtremesSpanish projectpu

Estudio del océano superior del Pacífico Tropical y su relación con un forzamiento del Atlántico

Ponencia presentada en: XXXI Jornadas Científicas de la AME y el XI Encuentro Hispano Luso de Meteorología celebrado en Sevilla, del 1 al 3 de marzo de 2010

Análisis de la Influencia del Atlántico en la variabilidad interanual del Pacífico tropical

Ponencia presentada en: XXXII Jornadas Científicas de la AME y el XIII Encuentro Hispano Luso de Meteorología celebrado en Alcobendas (Madrid), del 28 al 30 de mayo de 2012

Impact of equatorial Atlantic variability on ENSO predictive skill

El Niño-Southern Oscillation (ENSO) is a key mode of climate variability with worldwide climate impacts. Recent studies have highlighted the impact of other tropical oceans on its variability. In particular, observations have demonstrated that summer Atlantic Niños (Niñas) favor the development of Pacific Niñas (Niños) the following winter, but it is unclear how well climate models capture this teleconnection and its role in defining the seasonal predictive skill of ENSO. Here we use an ensemble of seasonal forecast systems to demonstrate that a better representation of equatorial Atlantic variability in summer and its lagged teleconnection mechanism with the Pacific relates to enhanced predictive capacity of autumn/winter ENSO. An additional sensitivity study further shows that correcting SST variability in equatorial Atlantic improves different aspects of forecast skill in the Tropical Pacific, boosting ENSO skill. This study thus emphasizes that new efforts to improve the representation of equatorial Atlantic variability, a region with long standing systematic model biases, can foster predictive skill in the region, the Tropical Pacific and beyond, through the global impacts of ENSO

From Magma Source to Volcanic Sink Under Tagoro Volcano (El Hierro, Canary Islands): Petrologic, Geochemical and Physiographic Evolution of the 2011–2012 Submarine Eruption

Active volcanoes are key laboratories to carry out detailed research -and monitoring- about the history of magmas before, during and after eruptions. Tagoro, the submarine active volcano at El Hierro Island (Canary archipelago), is a highly favorable case to assess and monitor its daily ongoing behaviour, as well as to study the links between the processes of magma genesis occurring at depth and their derived eruptive events at the surface. In this interdisciplinary research we combine new results of classical petrology (petrography, geochemistry, and thermodynamics) on the volcanic products expelled by Tagoro during the 2011–2012 eruption, with a high-resolution (5 m grid) bathymetry model carried out during 2017, and recent data from magnetometry, to refine the current knowledge of this eruption. Our results mainly reveal (i) slight magma differentiation and mixing processes at c. 12 km depth during a continuous eruptive pulse; (ii) a similar magmatic evolution and residence times at depth between previous and 2011–2012 eruptions on the island; (iii) an insignificant interaction of external fluids with the magma at depth or within the ascent conduit; (iv) a present-day magnetometric anomaly under the Tagoro’s area; (v) a minimum volume estimate for the magma withdrawn from the plumbing system at depth.This research was possible thanks to: (i) the funds provided by the MINECO and FEDER through the project VULCANO I (CTM2012-36317) and the project VULCANA (Vulcana-IEO-2015-2017) funded by the Spanish Institute of Oceanography, both granted to E.F.-N., that provided the oceanographic instruments, cruise and samples; (ii) the funds provided by the MINECO and MEC grants (Spanish Government) to A.M.A.-V. through the programs EXPLORA-CIENCIA (CGL2014—61775-EXP; MINECO), José Castillejo (CAS14-00189; MEC), and Programa Propio mod. 1B—2019 (USAL). J.M. is supported by EC Grant EVE (DG ECHO H2020 826292). A.P S is grateful for his PhD grant “Programa Propio III Universidad de Salamanca, cofounded by Banco de Santander”. H.A. is a Serra Húnter Lecturer Professor at the University of Barcelona. A-V specially thanks all the colleagues and friends who made possible this research starting from the ones designing the oceanographic campaigns, to those sharing their work on the vessel’s deck and acoustic lab, or carrying out geochemical analysis, as well as the undergraduate and graduate students involved in the research (some developing their master and graduate theses at USAL, e.g. I.N. and N.G., respectively). We also thank the careful and in-depth reviews by D. González García, an anonymous reviewer and editor. This research is also part of the PTI VOLCAN research initiatives.Peer reviewe