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88 results for “El Niño”
Programa "Juego, coopero y aprendo" para el desarrollo psicomotor de niños de 3 años de una I.E. del Callao
<p>La matriz de datos incluye las siguientes variables: Alumno, Género, Edad, Coordinación, Lenguaje, Motricidad y 16 casos.</p>
Programa de cuentos pictográficos para incrementar el lenguaje oral en niños(as) de 3 años de una institución educativa del Callao
<p>La matriz de datos contiene las siguientes variables: Lenguaje oral, Programa de cuentos pictográficos, Pre-test, Forma, Contenido, Uso.</p>
Programa de cuentos pictográficos para incrementar el lenguaje oral en niños(as) de 3 años de una institución educativa del Callao
<p>La matriz de datos contiene las siguientes variables: Lenguaje oral, Programa de cuentos pictográficos, Pre-test, Forma, Contenido, Uso y 17 casos.</p>
Biogeochemical responses to different El Niño events in the equatorial Pacific: A case study of 1997-98 and 2015-16 El Niños
<p>Model output used in Biogeochemical responses to different El Niño events in the equatorial Pacific: A case study of 1997-98 and 2015-16 El Niños</p>
Data for "Strong El Niño events lead to robust multi-year ENSO predictability"
<p>The full raw data, intermediate steps, and final results for all three experiments used in Lenssen et al. (202X), "Strong El Niño events lead to robust multi-year ENSO predictability," as submitted to GRL. Each zip file contains the raw data, intermediate steps, and final results for model analog forecast issued to predict that model or observational record. All data has been gridded to a common 2x2 grid using nco following the include `mygrid_2x2` file.</p><p>Archived codebase for this data available at <a href="https://zenodo.org/doi/10.5281/zenodo.10045615">https://zenodo.org/doi/10.5281/zenodo.10045615</a><br>Live codebase at <a href="https://github.com/nlenssen/LongLeadENSO/">https://github.com/nlenssen/LongLeadENSO/</a></p>
The model data of Potential Impact of Spring Thermal Forcing over the Tibetan Plateau on the Following Winter El Niño–Southern Oscillation
<p>This is the model data of "Potential Impact of Spring Thermal Forcing over the Tibetan Plateau on the Following Winter El Niño–Southern Oscillation". The data includes the last 20 years data of control run (CTRL), the 20 years data of TP–T experiment, and the wave activity flux difference between ensemble means of TP–T and CTRL. 2D is two dimensions. 3D is three dimensions.</p>
Different biogeochemical responses to the 1997-98 and 2015-16 El Niño events in the equatorial Pacific: Did PDO play a role?
<p>This dataset contains model outputs simulated by a basin-scale model (OGCM-DEEC V1.4). It is supplementary of the paper "Different biogeochemical responses to the 1997-98 and 2015-16 El Niño events in the equatorial Pacific: Did PDO play a role?". Please let me know if you need any more information</p>
San José y el niño
San José y el niño, Estancia Jesuítica "La Candelaria". Córdoba, Argentina. Source: Objaverse 1.0 / Sketchfab
Los premios para niños y Jóvenes el canon no académico
<p>Los datos forman parte del proyecto de investigación «El canon literario no académico: construcción, características, responsables, selección y recepción en los epitextos públicos virtuales» PID2019-10587RB-I00. Proyectos de I+D+i en el marco de los Programas Estatales generación de conocimiento y fortalecimiento científico y tecnológico del sistema de I+D+i Orientada a los Retos de la Sociedad. Ministerio de Ciencia e Innovación de España. Convocatoria 2019. </p> <p>DATOS COMUNICADOS EN: </p> <div> Baldaquí-Escandell, Josep Maria; García-Rodríguez, Araceli; Gómez-Díaz, Raquel; Lluch, Gemma; Sanz Tejeda, Aránzazu (2024): “Premios, biblioteca y booksinfluenceros como constructores del canon no académico. El caso de la LIJ”. Salamanca: Publicaciones de la Universidad de Salamanca. </div> <p>García Rodríguez, Araceli; Gómez-Díaz, Raquel (2022). Children’s and young adults’ literature awards in Spain: Analysis and characterization. <em>History of Education & Children’s Literature.</em> XVII, n. 2, pp. 355-376</p> <div>Gómez-Díaz, Raquel y García-Rodríguez, Araceli (2024). Los premios como configuradores de un canon literario infantil y juvenil. <em>Ocnos</em>, 23(1). https://doi.org/10.18239/ocnos_2024.23.1.452 </div> <div> </div> <div>Lluch, Gemma (dir.), García Rodríguez, Araceli, Gómez Díaz, Raquel, Escandell, Dari, Sanz-Tejeda, Aranzazu, Esteve, Ana, Francés, M. Àngels (2024): LOS LIBROS QUE LEEMOS; QUIÉN, CÓMO Y DÓNDE SE DECIDE. La construcción del canon no académico. Editorial Tirant lo blanc. </div>
Coupling and de-coupling of the El Niño Southern Oscillation to the supply of larval fishes to benthic populations in the Hawaiian Islands
<p>Several recent high intensity ENSO events have caused strong negative impacts on the adult phases of foundational species in coral reef ecosystems, but comparatively little is known about how climatic variables related to recent ENSOs are impacting the supply of larvae to benthic populations. In marine fishes and invertebrates, reproductive adults and planktonic larvae are generally more sensitive to environmental variability than older, non-reproductive adults. Further, the transport of larvae in ocean currents may also be strongly ENSO dependent. The interactions between the dynamics of larval survivorship and larval transport could lead to population bottlenecks as stronger ENSO events become more common. We tested the predictions of this hypothesis around the Main Hawaiian Islands (MHI) by constructing a correlation matrix of physical and biological time series variables that spanned 11 years (2007 – 2017) and multiple ENSO events. Our correlation matrix included four types of variables: i. published ENSO indices, ii. satellite-derived sea surface temperature (SST) and chlorophyll variables, iii. abundance and diversity of larval fishes sampled during the late winter spawning season off Oahu, and iv. abundance and diversity of coral reef fish recruits sampled on the western shore of the Big Island of Hawaii. We found that the abundance and diversity of larval fishes was negatively correlated with the Multivariate El Niño Index (MEI), and that larval variables were positively correlated with measures of fall recruitment (September & November), but not correlated with spring-summer recruitment (May & July). In the MHI, SST variables were not correlated with the MEI, but two successive El Niño events of 2014-15 and 2015-2016 were characterized by SST maxima approaching 30 °C. Two large pulses of benthic recruitment occurred in the 2009 and 2014 recruitment seasons, with > 8000 recruits observed by divers over the summer and fall months. Both events were characterized by either neutral or negative MEI indices measured during the preceding winter months. These patterns suggest that La Niña and the neutral phases of the ENSO cycle are generally favorable for adult reproduction and larval development in the spring and summer, while El Niño phases may limit recruitment in the late summer and fall. We hypothesize that episodic recruitment during non-El Niño phases is related to favorable survivorship and transport dynamics that are associated with the formation of pairs of anticyclonic and cyclonic eddies on the leeward sides (western shores) of the Main Hawaiian Islands.</p>
El Niño Enhances Exposure to Humid Heat Extremes with Regionally Varying Impacts during Eastern vs Central Pacific Events
<p><span>Humid heat extremes, characterized by high wet bulb temperature (Tw), pose significant health risks. While strong El Niño events are known to affect the frequency of extreme Tw days, the distinct impacts of Central Pacific (CP) and Eastern Pacific (EP) El Niño events remain understudied. Using a 12-member CMIP6 ensemble at discrete global warming targets (+1.5˚C, 2˚C, 3˚C, 4˚C), this study shows progressively enhanced humid heat exposure during EP events primarily in Mainland Southeast Asia, while South Asia experiences regionally opposing effects from EP and CP events. EP and CP events expose distinct, regionally varying areas to dangerous Tw, yet both significantly amplify population and area exposure to humid heat extremes at all global warming levels. This amplification surpasses the impact of an additional degree of global warming, highlighting El Niño’s compounding effect on heat stress threats across warmer climates.</span> <br><a name="_msocom_1"></a></p>
Data for "Strong linkage of El Niño-Southern Oscillation to the polar cold air mass in the Northern Hemisphere"
<p>This repository archives codes for analysis and plot presented in Abdillah et al. (2018): "Strong linkage of El Niño-Southern Oscillation to the polar cold air mass in the Northern Hemisphere". The codes are written in GrADS, Octave, and NCL format. </p> <p>The repository also includes a Fortran package for isentropic polar cold air mass diagnosis as in Iwasaki et al. (2014). The package was specifically created by Dr. Y. Kanno.</p> <p>Reference:</p> <p>Abdillah, M. R., Kanno, Y., Iwasaki, T. (2018). Strong linkage of El Niño‐Southern Oscillation to the polar cold air mass in the Northern Hemisphere. <em>Geophysical Research Letters, in press. </em>https://doi.org/10.1029/2018GL077612</p> <p>Iwasaki, T., Shoji, T., Kanno, Y., Sawada, M., Ujiie, M., & Takaya, K. (2014). Isentropic Analysis of Polar Cold Airmass Streams in the Northern Hemispheric Winter. <em>Journal of the Atmospheric Sciences</em>, <em>71</em>(6), 2230–2243. https://doi.org/10.1175/JAS-D-13-058.1</p>
Simulated coordinated impacts of the previous autumn NAO and winter El Niño on the winter aerosol concentrations over eastern China
<p>The simulated aerosol concentrations and the model input meteorology fields (SLP and wind at 850 hPa) , as well as the data description files are listed.</p>
Data from : "The massive 2016 marine heatwave in the Southwest Pacific: an "El Niño - Madden-Julian Oscillation" compound event"
<p>File : PD-JRA-v1-c6_TMLtrend_1993-2022.nc</p> <p>Daily mixed layer temperature budget between 1993 and 2022 from a NEMO simulation.</p> <p>Data were extracted over the Southwest Pacific region [142.5°E-222.5°E;45°S;1°N].</p> <p>These data were used in Dutheil et al., (2024) The massive 2016 marine heatwave in the Southwest Pacific: an “El Niño - Madden-Julian Oscillation” compound event</p>
The 2023 global warming spike was driven by El Niño/Southern Oscillation (Data)
<p>GFDL FLOR and CM2.1 surface temperature datasets used in:<br>Raghuraman et al., 2024, Atmospheric Chemistry and Physics,<br>"The 2023 global warming spike was driven by El Niño/Southern Oscillation"</p> <p>Point of Contact: Shiv Priyam Raghuraman, sraghur2@illinois.edu</p> <p>All other model data files used in paper can be downloaded from their respective websites (see paper's "Data availability" section).</p>
CESM experiments for intraseasonal oscillation intensity changes in El Niño and La Niña developing summers
<p> Experiments are conducted using version 5.2 of Community Atmospheric Model (CAM-5.2; https://www.cesm.ucar.edu/models/cesm1.1/cam/). CAM is the atmosphere component of Community Earth System Model (CESM) developed by the National Center for Atmospheric Research (NCAR). The model resolution used in this study is f19_g16, with f19 finite volume grid (1.9º latitude by 2.5º longitude) for the atmosphere and land components combined with the gx1v6 displaced pole grid (approximately 1º) for the ocean and ice components.</p> <p> Four sets of numerical experiments are performed in this study:</p> <ol> <li>Full SST forcing simulation (full-SST run): The CAM is forced by global monthly OI SST and integrated from January 1982 to December 2020.</li> <li>Climatological SST forcing simulation (CLM-SST run): The CAM is integrated for 30 years forced by global climatological mean monthly SST obtained from OI SST data for the period of January 1982 to December 2020.</li> <li>Tropical central-eastern Pacific SST forcing simulation (CEP-SST run): The SST forcing field is composed of two parts: total monthly SST in the domain of 15°S-15°N and 160°E-80°W and climatological mean monthly SST in the other regions. The CAM is integrated from January 1982 to December 2020.</li> <li>Sensitivity experiments of tropical central-eastern Pacific SST anomalies during ENSO events: Composite SST anomalies in El Niño and La Niña events in the region of 15°S-15°N and 160°E-80°W and the above SST anomaly fields multiplied by -1 are added to climatological mean monthly SST from May to December. Climatological mean monthly SST is used in the other regions and months. The CAM is integrated for 30 years in these experiments. These experiments are referred to as EPEL, EPLA, EPEL-reverse and EPLA-reverse, respectively.</li> </ol>
Fig. 1 in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil
Fig. 1. Study area in middle rio Negro basin (a) and detail of the sampling sites (b).
Fig. 2 in Spatial and temporal variation of benthic fish assemblages during the extreme drought of 1997-98 (El Niño) in the middle rio Negro, Amazonia, Brazil
Fig. 2. River level during annual flood cycles. Large arrows denote dates of sampling expeditions.
Supporting data for: Oceanic and atmospheric drivers of post-El-Niño chlorophyll rebound in the equatorial Pacific
<p>The GFDL ESM2M, ESM4.1, ESM4.1-static simulation data used for ENSO related chlorophyll and iron analysis in the study are available in this repository. </p> <p>Please contact <a href="mailto:hyung-gyu.lim@noaa.gov">hyung-gyu.lim@noaa.gov</a> for further questions.. </p> <p>The project on "Oceanic and atmospheric drivers of post-El-Niño chlorophyll rebound in the equatorial Pacific" is implemented based on below dataset that is submitted to Geophysical Research Letters at September 2021</p> <p>regridded by 1 degree horizontal resolution for the tropical Pacific region [120E-60W, 20N-20S]</p> <p>ESM2M : chl, temp, fed, no3 for 1001-1100 years</p> <p>ESM4.1: chl, thetao, dfe, no3, od550dust, dep_dry_fed, dep_wet_fed for 501-650 years</p> <p>ESM4.1-static: chlos, dfeos, tos for 501-650 years</p> <p>The tar file in this submission holds the above data. </p>
Potential Impact of Winter–Spring North Atlantic Tripole SSTAs on the Following Autumn–Winter El Niño–Southern Oscillation: Bridging Role of the Tibetan Plateau
<p>This is the key model data of "Potential Impact of Winter–Spring North Atlantic Tripole SSTAs on the Following Autumn–Winter El Niño–Southern Oscillation: Bridging Role of the Tibetan Plateau". The data includes the last 25 years data of the CTRL experiment, and 25 years data of the CTRL_NTP experiment, the NA_ST experiment, and the NA_ST_NTP experiment, respectively. "2D" is two-dimensional variables , "3D" is three-dimensional variables, and "pottmp" is ocean potential temperature.</p>
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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