Works matching La Niña
Results: 4555
ABUNDANCIA DE Amblyrhynchus cristatus EN EL NIÑO (97-98) Y LA NIÑA (01-02) EN SANTA CRUZ, GALÁPAGOS.
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- Ecologia Aplicada, 2004, v. 3, n. 1/2, p. 87
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Análisis del comportamiento de la precipitación en el municipio de Buenaventura (Valle del Cauca, Colombia) en condiciones de desarrollo de los fenómenos El Niño y La Niña.
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- Cuadernos de Geografia: Revista Colombiana de Geografía, 2014, v. 23, n. 1, p. 165
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COINCIDENCIAS ENTRE EL NIÑO, LA NIÑA Y LA PRECIPITACIÓN EN LAS CUENCAS ACAPONETA Y CANDELARIA, MÉXICO.
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- Hemispheric & Polar Studies Journal / Revista Estudios Hemisféricos y Polares, 2018, v. 9, n. 1, p. 39
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Modelo para el Control de Inundaciones durante el Fenómeno De "La Niña" Utilizando un Embalse Hidroeléctrico.
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- Información Tecnológica, 2015, v. 26, n. 2, p. 89, doi. 10.4067/S0718-07642015000200011
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Análisis estadístico de las precipitaciones en la cuenca del río de Bogotá (Colombia) incluyendo las variables del fenómeno El Niño y La Niña.
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- Revista Espacios, 2020, v. 41, n. 38, p. 125
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LA NIÑA DE PLATA: A HISTÓRIA DE DONA MARIA DE PADILHA E DOM PEDRO I POR LOPE DE VEGA.
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- Revista Alea: Estudos Neolatinos, 2024, v. 26, n. 1, p. 1, doi. 10.1590/1517-106X/2024e62125
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Characterization of El Niño, La Niña, and normal conditions through planktonic foraminifera (2006-2007) in the southeastern Pacific.
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- Ciencias Marinas, 2013, v. 39, n. 3, p. 253, doi. 10.7773/cm.v39i3.2177
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“La niña horrible” entre la apoteosis teatral y la subversión heteropatriarcal.
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- Revista Laboratorio, 2023, n. 28, p. 1, doi. 10.32995/rl282023303
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Evolução mensal da cota fluviométrica do Rio Xingu em Altamira-PA associada aos eventos El Niño e La Niña.
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- Revista Ciência e Natura, 2015, v. 37, p. 104, doi. 10.5902/2179460X16223
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A most-recognized principle to define El Niño and La Niña years based on the K-line diagram technique.
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- International Journal of Climatology, 2015, v. 35, n. 10, p. 2777, doi. 10.1002/joc.4171
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Juvenile chinook salmon ( Oncorhynchus tshawytscha) growth on the central California coast during the 1998 El Niño and 1999 La Niña.
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- Fisheries Oceanography, 2005, v. 14, n. 5, p. 321, doi. 10.1111/j.1365-2419.2005.00338.x
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Why Eastern Africa was not dry during the 2020 short rainy season despite La Niña and a negative Indian Ocean Dipole: Interplay between the Madden-Julian Oscillation and La Niña in modulating short rain.
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- Theoretical & Applied Climatology, 2023, v. 153, n. 3/4, p. 1191, doi. 10.1007/s00704-023-04519-9
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Spatial classification of La Niña events.
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- Izvestiya, Atmospheric & Oceanic Physics, 2017, v. 53, n. 1, p. 111, doi. 10.1134/S0001433817010133
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Impacts of Tropical Indian and Atlantic Ocean Warming on the Occurrence of the 2017/2018 La Niña.
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- Geophysical Research Letters, 2019, v. 46, n. 6, p. 3435, doi. 10.1029/2019GL082280
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Thermodynamic processes prolong triple La Niña events in a hybrid coupled ocean-atmosphere model.
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- Climate Dynamics, 2025, v. 63, n. 2, p. 1, doi. 10.1007/s00382-024-07564-w
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Thermodynamic processes prolong triple La Niña events in a hybrid coupled ocean-atmosphere model.
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- Climate Dynamics, 2025, v. 63, n. 1, p. 1, doi. 10.1007/s00382-024-07564-w
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Roles of tropical-Pacific interannual–interdecadal variability in forming the super long La Niña events.
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- Climate Dynamics, 2024, v. 62, n. 9, p. 9117, doi. 10.1007/s00382-024-07381-1
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Positive feedback between the negative phase of interannual component of the Pacific Decadal Oscillation and La Niña.
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- Climate Dynamics, 2024, v. 62, n. 8, p. 8319, doi. 10.1007/s00382-024-07346-4
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The asymmetry of air-sea coupled strength between the first-year and second-year La Niña events.
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- Climate Dynamics, 2024, v. 62, n. 7, p. 6951, doi. 10.1007/s00382-024-07259-2
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How the central-western equatorial Pacific easterly wind in early 2022 affects the third-year La Niña occurrence.
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- Climate Dynamics, 2024, v. 62, n. 5, p. 3047, doi. 10.1007/s00382-023-07050-9
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Effects of Indian Ocean Dipole initialization on the forecasting of La Niña 1 year in advance.
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- Climate Dynamics, 2023, v. 61, n. 9/10, p. 4661, doi. 10.1007/s00382-023-06816-5
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Causes of positive precipitation anomalies in South China during La Niña winters.
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- Climate Dynamics, 2023, v. 61, n. 7/8, p. 3343, doi. 10.1007/s00382-023-06738-2
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Extreme precipitation driven by the rapid tropical Atlantic warming and the second developing La Niña over the Yangtze–Huaihe River Basin in August 2021.
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- Climate Dynamics, 2023, v. 61, n. 5/6, p. 2581, doi. 10.1007/s00382-023-06683-0
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Combined effects of La Niña events and Arctic tropospheric warming on the winter North Pacific storm track.
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- Climate Dynamics, 2023, v. 60, n. 5/6, p. 1351, doi. 10.1007/s00382-022-06389-9
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Long-lived cold blobs in the Northeast Pacific linked with the tropical La Niña.
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- Climate Dynamics, 2021, v. 57, n. 1/2, p. 223, doi. 10.1007/s00382-021-05706-y
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Impacts of different types of El Niño and La Niña on northern tropical Atlantic sea surface temperature.
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- Climate Dynamics, 2020, v. 54, n. 9/10, p. 4147, doi. 10.1007/s00382-020-05220-7
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Change of El Niño and La Niña amplitude asymmetry around 1980.
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- Climate Dynamics, 2020, v. 54, n. 3/4, p. 1351, doi. 10.1007/s00382-019-05062-y
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Northeast monsoon rainfall variability over the southern Peninsular India associated with multiyear La Niña events.
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- Climate Dynamics, 2019, v. 53, n. 9/10, p. 6265, doi. 10.1007/s00382-019-04927-6
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Frequency of extreme El Niño and La Niña events under global warming.
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- Climate Dynamics, 2019, v. 53, n. 9/10, p. 5799, doi. 10.1007/s00382-019-04902-1
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Mechanism for asymmetric atmospheric responses in the western North Pacific to El Niño and La Niña.
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- Climate Dynamics, 2019, v. 53, n. 7/8, p. 3957, doi. 10.1007/s00382-019-04767-4
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Season-dependent predictability and error growth dynamics for La Niña predictions.
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- Climate Dynamics, 2019, v. 53, n. 1/2, p. 1063, doi. 10.1007/s00382-019-04631-5
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Signature of La Niña in interannual variations of the East India Coastal Current during spring.
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- Climate Dynamics, 2019, v. 53, n. 1/2, p. 551, doi. 10.1007/s00382-018-4601-9
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A "La Niña-like" state occurring in the second year after large tropical volcanic eruptions during the past 1500 years.
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- Climate Dynamics, 2019, v. 52, n. 12, p. 7495, doi. 10.1007/s00382-018-4163-x
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Role of ocean heat content in boosting post-monsoon tropical storms over Bay of Bengal during La-Niña events.
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- Climate Dynamics, 2019, v. 52, n. 12, p. 7225, doi. 10.1007/s00382-016-3428-5
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Impact of multiyear La Niña events on the South and East Asian summer monsoon rainfall in observations and CMIP5 models.
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- Climate Dynamics, 2019, v. 52, n. 11, p. 6989, doi. 10.1007/s00382-018-4561-0
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Spatial variation of different rain systems during El Niño and La Niña periods over India and adjoining ocean.
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- Climate Dynamics, 2018, v. 50, n. 9/10, p. 3671, doi. 10.1007/s00382-017-3833-4
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Spatiotemporal change of intraseasonal oscillation intensity over the tropical Indo-Pacific Ocean associated with El Niño and La Niña events.
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- Climate Dynamics, 2018, v. 50, n. 3/4, p. 1221, doi. 10.1007/s00382-017-3675-0
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Asymmetry in summertime atmospheric circulation anomalies over the northwest Pacific during decaying phase of El Niño and La Niña.
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- Climate Dynamics, 2017, v. 49, n. 5/6, p. 2007, doi. 10.1007/s00382-016-3432-9
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Roles of tropical SST anomalies in modulating the western north Pacific anomalous cyclone during strong La Niña decaying years.
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- Climate Dynamics, 2017, v. 49, n. 1/2, p. 633, doi. 10.1007/s00382-016-3364-4
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The roles of atmospheric wind and entrained water temperature (T) in the second-year cooling of the 2010-12 La Niña event.
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- Climate Dynamics, 2017, v. 48, n. 1/2, p. 597, doi. 10.1007/s00382-016-3097-4
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Interaction of the recent 50 year SST trend and La Niña 2010: amplification of the Southern Annular Mode and Australian springtime rainfall.
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- Climate Dynamics, 2016, v. 47, n. 7/8, p. 2273, doi. 10.1007/s00382-015-2963-9
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Relative importance of tropical SST anomalies in maintaining the Western North Pacific anomalous anticyclone during El Niño to La Niña transition years.
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- Climate Dynamics, 2016, v. 46, n. 3/4, p. 1027, doi. 10.1007/s00382-015-2630-1
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Role of intraseasonal oscillation in asymmetric impacts of El Niño and La Niña on the rainfall over southern China in boreal winter.
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- Climate Dynamics, 2015, v. 45, n. 3/4, p. 559, doi. 10.1007/s00382-014-2207-4
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La Niña diversity and Northwest Indian Ocean Rim teleconnections.
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- Climate Dynamics, 2014, v. 43, n. 9/10, p. 2707, doi. 10.1007/s00382-014-2083-y
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The regional forcing of Northern hemisphere drought during recent warm tropical west Pacific Ocean La Niña events.
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- Climate Dynamics, 2014, v. 42, n. 11/12, p. 3289, doi. 10.1007/s00382-013-1799-4
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Perceptions of El Niño-Southern Oscillation (ENSO) and La Niña Shape Fishers' Adaptive Capacity and Resilience.
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- Social Sciences (2076-0760), 2024, v. 13, n. 7, p. 356, doi. 10.3390/socsci13070356
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Shifts in Growing Season of Tropical Deciduous Forests as Driven by El Niño and La Niña during 2001–2016.
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- Forests (19994907), 2018, v. 9, n. 8, p. 448, doi. 10.3390/f9080448
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Forecasting El Niño/La Niña and Their Types Using Neural Networks.
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- Russian Meteorology & Hydrology, 2020, v. 45, n. 11, p. 806, doi. 10.3103/S1068373920110084
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New rurality and the experience of place: the small rural locality of La Niña, Buenos Aires, Argentina.
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- GeoJournal, 2018, v. 83, n. 6, p. 1301, doi. 10.1007/s10708-017-9834-3
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Why Does Extreme Precipitation Occur in Borneo During Both El Niño and La Niña Winters?
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- Journal of Geophysical Research. Atmospheres, 2024, v. 129, n. 10, p. 1, doi. 10.1029/2023JD040415
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