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Journal articles on the topic 'Modoki El Niño'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Hsu, Po-Chun, Chung-Ru Ho, Shin-Jye Liang, and Nan-Jung Kuo. "Impacts of Two Types of El Niño and La Niña Events on Typhoon Activity." Advances in Meteorology 2013 (2013): 1–8. http://dx.doi.org/10.1155/2013/632470.

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The HadISST (Hadley Centre Sea Ice and Sea Surface Temperature) dataset is used to define the years of El Niño, El Niño Modoki, and La Niña events and to find out the impacts of these events on typhoon activity. The results show that the formation positions of typhoon are farther eastward moving in El Niño years than in La Niña years and much further eastward in El Niño Modoki years. The lifetime and the distance of movement are longer, and the intensity of typhoons is stronger in El Niño and in El Niño Modoki years than in La Niña years. The Accumulated Cyclone Energy of typhoon is highly cor

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2

Taschetto, Andréa S., and Matthew H. England. "El Niño Modoki Impacts on Australian Rainfall." Journal of Climate 22, no. 11 (2009): 3167–74. http://dx.doi.org/10.1175/2008jcli2589.1.

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Abstract This study investigates interseasonal and interevent variations in the impact of El Niño on Australian rainfall using available observations from the postsatellite era. Of particular interest is the difference in impact between classical El Niño events wherein peak sea surface temperature (SST) anomalies appear in the eastern Pacific and the recently termed El Niño “Modoki” events that are characterized by distinct warm SST anomalies in the central Pacific and weaker cold anomalies in the west and east of the basin. A clear interseasonal and interevent difference is apparent, with the

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3

Wang, Chunzai, and Xin Wang. "Classifying El Niño Modoki I and II by Different Impacts on Rainfall in Southern China and Typhoon Tracks." Journal of Climate 26, no. 4 (2013): 1322–38. http://dx.doi.org/10.1175/jcli-d-12-00107.1.

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Abstract Based on their opposite influences on rainfall in southern China during boreal fall, this paper classifies El Niño Modoki into two groups: El Niño Modoki I and II, which show different origins and patterns of SST anomalies. The warm SST anomalies originate in the equatorial central Pacific and subtropical northeastern Pacific for El Niño Modoki I and II, respectively. Thus, El Niño Modoki I shows a symmetric SST anomaly distribution about the equator with the maximum warming in the equatorial central Pacific, whereas El Niño Modoki II displays an asymmetric distribution with the warm

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4

Xie, F., J. Li, W. Tian, J. Feng, and Y. Huo. "Signals of El Niño Modoki in the tropical tropopause layer and stratosphere." Atmospheric Chemistry and Physics 12, no. 11 (2012): 5259–73. http://dx.doi.org/10.5194/acp-12-5259-2012.

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Abstract. The effects of El Niño Modoki events on the tropical tropopause layer (TTL) and on the stratosphere were investigated using European Center for Medium Range Weather Forecasting (ECMWF) reanalysis data, oceanic El Niño indices, and general climate model outputs. El Niño Modoki events tend to depress convective activities in the western and eastern Pacific but enhance convective activities in the central and northern Pacific. Consequently, during El Niño Modoki events, negative water vapor anomalies occur in the western and eastern Pacific upper troposphere, whereas there are positive

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5

Li, Gen, Baohua Ren, Chengyun Yang, and Jianqiu Zheng. "Indices of El Niño and El Niño Modoki: An improved El Niño Modoki index." Advances in Atmospheric Sciences 27, no. 5 (2010): 1210–20. http://dx.doi.org/10.1007/s00376-010-9173-5.

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6

Sobaeva, D. A. "THE INFLUENCE OF THE LOCALIZATION OF POSITIVE SURFACE TEMPERATURE ANOMALIES IN THE EQUATORIAL PACIFIC OCEAN ON THE PROPAGATION OF WAVE ACTIVITY FROM THE TROPOSPHERE TO THE STRATOSPHERE IN MODEL EXPERIMENTS." Journal of Oceanological Research 52, no. 4 (2024): 224–42. https://doi.org/10.29006/1564-2291.jor-2024.52(4).11.

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During an El Niño event an area of intense convection is formed above the area of positive sea surface temperature (SST) anomalies in the equatorial Pacific Ocean. This leads to the formation of a Rossby wave, which propagates from low to high latitudes and can lead to changes in largescale atmospheric circulation in mid-latitudes and, as a consequence, to a change in the vertical wave activity flow from the troposphere to the stratosphere. In recent decades, a new type of El Niño – El Niño Modoki – has been increasingly observed. During El Niño Modoki positive SST anomalies are observed in th

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7

Xie, F., J. Li, W. Tian, and J. Feng. "Signals of El Niño Modoki in the tropical tropopause layer and stratosphere." Atmospheric Chemistry and Physics Discussions 12, no. 2 (2012): 3619–53. http://dx.doi.org/10.5194/acpd-12-3619-2012.

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Abstract. The effects of El Niño Modoki events on the tropical tropopause layer (TTL) and on the stratosphere were investigated using European Center for Medium Range Weather Forecasting (ECMWF) reanalysis data, satellite observations from the Aura satellite Microwave Limb Sounder (MLS), oceanic El Niño indices, and general climate model outputs. El Niño Modoki events tend to depress convective activities in the western and eastern Pacific but enhance convective activities in the central and northern Pacific. Consequently, during Modoki events, negative water vapor anomalies occur in the weste

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8

Lin, Chen-Chih, Yi-Jiun Liou, and Shih-Jen Huang. "Impacts of Two-Type ENSO on Rainfall over Taiwan." Advances in Meteorology 2015 (2015): 1–7. http://dx.doi.org/10.1155/2015/658347.

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Impacts of two-type ENSO (El Niño/Southern Oscillation), canonical ENSO and ENSO Modoki, on rainfall over Taiwan are investigated by the monthly mean rainfall data accessed from Taiwan Central Weather Bureau. The periods of the two-type ENSO are distinguished by Niño 3.4 index and ENSO Modoki index (EMI). The rainfall data in variously geographical regions are analyzed with the values of Niño 3.4 and EMI by correlation method. Results show that the seasonal rainfalls over Taiwan are different depending on the effects of two-type ENSO. In canonical El Niño episode, the rainfall increases in win

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9

Tan, Wei, Xin Wang, Weiqiang Wang, Chunzai Wang, and Juncheng Zuo. "Different Responses of Sea Surface Temperature in the South China Sea to Various El Niño Events during Boreal Autumn." Journal of Climate 29, no. 3 (2016): 1127–42. http://dx.doi.org/10.1175/jcli-d-15-0338.1.

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Abstract This study investigates variations of sea surface temperature (SST) anomalies in the South China Sea (SCS) during developing autumn of various El Niño events. The warm SST anomalies are observed in the SCS for canonical El Niño and El Niño Modoki I, whereas the cold SST anomalies are found for El Niño Modoki II. The ocean heat budget analyses show that the latent heat flux change induced by various types of El Niño events is a major contributor to the SCS SST variations. An anomalous anticyclone resides near the Philippine Sea for canonical El Niño and El Niño Modoki I, which induces

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10

Minuzzi, Rosandro Boligon, and Carolina Do Amaral Frederico. "Variabilidade de ondas de calor e a relação com o ENOS Modoki e Canônico em Santa Catarina." Journal of Environmental Analysis and Progress 2, no. 4 (2017): 421–29. http://dx.doi.org/10.24221/jeap.2.4.2017.1440.421-429.

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Dados diários de temperatura aparente de quatro localidades em Santa Catarina foram utilizados para analisar a variabilidade climática espacial e temporal de ondas de calor (OC) e suas relações com o El Niño (EN) e La Niña (LN) Modoki e Canônico. Definiu-se uma onda de calor, o evento com pelo menos três dias seguidos de temperatura aparente igual ou superior ao percentil 90 (‘dia de calor’) de cada período sazonal analisado (verão, outono, inverno e primavera). O número de ocorrências e a duração de OC local (OCL) e regional (OCR) foram analisadas em sequência para os anos da série histórica

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11

Gen, Li, Ren Bao-Hua, Yang Cheng-Yun, and Zheng Jian-Qiu. "Traditional El Niño and El Niño Modoki Revisited: Is El Niño Modoki Linearly Independent of Traditional El Niño?" Atmospheric and Oceanic Science Letters 3, no. 2 (2010): 70–74. http://dx.doi.org/10.1080/16742834.2010.11446845.

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12

Schultz, Colin. "Explaining away El Niño Modoki." Eos, Transactions American Geophysical Union 92, no. 30 (2011): 256. http://dx.doi.org/10.1029/2011eo300011.

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13

Alsepan, Givo, and Shoshiro Minobe. "Relations between Interannual Variability of Regional-Scale Indonesian Precipitation and Large-Scale Climate Modes during 1960–2007." Journal of Climate 33, no. 12 (2020): 5271–91. http://dx.doi.org/10.1175/jcli-d-19-0811.1.

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AbstractRegional-scale precipitation responses over Indonesia to major climate modes in the tropical Indo–Pacific Oceans, namely canonical El Niño, El Niño Modoki, and the Indian Ocean dipole (IOD), and how the responses are related to large-scale moisture convergences are investigated. The precipitation responses, analyzed using a high-spatial-resolution (0.5° × 0.5°) terrestrial precipitation dataset for the period 1960–2007, exhibit differences between the dry (July–September) and wet (November–April) seasons. Canonical El Niño strongly reduces precipitation in central to eastern Indonesia

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14

Da Silva, Djane Fonseca, Pedro Fernandes de Souza Neto, Silvania Donato da Silva, et al. "Identificação das causas climáticas dos eventos extremos e dos impactos dos ENOS Canônico e Modoki nas macrorregiões de Alagoas." Revista Brasileira de Geografia Física 14, no. 4 (2021): 1880–97. http://dx.doi.org/10.26848/rbgf.v14.4.p1880-1897.

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Anomalies of sea surface temperature that occur in some regions of the Equatorial Pacific Ocean are being studied because their cause different impacts and originate in different ways, are the ENOS, Modoki and Canonical. The objective of this work is to identify the climatic causes of the extreme events that occurred in the macro-regions of Alagoas, and at the same time, to compare the effects of ENOS Canonical and Modoki and their classes on the macro-regions of Alagoas. The daily precipitation data for 21 municipalities in the State of Alagoas were obtained through the National Water Agency

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15

Gonzales, Edgard, and Eusebio Ingol. "Determination of a New Coastal ENSO Oceanic Index for Northern Peru." Climate 9, no. 5 (2021): 71. http://dx.doi.org/10.3390/cli9050071.

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In 2017, extreme rainfall events occurred in the northern portion of Peru, causing nearly 100,000 victims, according to the National Emergency Operations Center (COEN). This climatic event was attributed to the occurrence of the El Niño Southern Oscillation (ENSO). Therefore, the main objective of this study was to determine and differentiate between the occurrence of canonical ENSO, with a new type of ENSO called “El Niño Costero” (Coastal El Niño). The polynomial equation method was used to analyze the data from the different types of existing ocean indices to determine the occurrence of ENS

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16

Ratnam, J. V., S. K. Behera, Y. Masumoto, and T. Yamagata. "Remote Effects of El Niño and Modoki Events on the Austral Summer Precipitation of Southern Africa." Journal of Climate 27, no. 10 (2014): 3802–15. http://dx.doi.org/10.1175/jcli-d-13-00431.1.

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Abstract Remote effects modulating the austral summer precipitation over southern Africa during El Niño/El Niño Modoki events are investigated by analyzing the observed events during December–February of the years from 1982/83 to 2010/11. Based on the composite analyses, it is found that southern Africa experiences significantly below normal precipitation during El Niño events compared to El Niño Modoki events. During these latter events, precipitation anomalies are not so significant although southern Africa as a whole receives below normal precipitations. The differences in the spatial distr

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17

Serna, Lina M., Paola A. Arias, and Sara C. Vieira. "Las corrientes superficiales de chorro del Chocó y el Caribe durante los eventos de El Niño y El Niño Modoki." Revista de la Academia Colombiana de Ciencias Exactas, Físicas y Naturales 42, no. 165 (2018): 410. http://dx.doi.org/10.18257/raccefyn.705.

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El objetivo de este artículo fue analizar la influencia de dos tipos de eventos de El Niño, conocidos como Canónico y Modoki, en las corrientes superficiales de chorro del Chocó y el Caribe, importantes mecanismos de transporte de humedad y generación de precipitación en Colombia. La influencia de estos tipos de eventos de El Niño en las corrientes superficiales de interés se examinó con base en las diferencias entre las características en la climatología de estos chorros durante dichos eventos y el análisis de correlaciones entre estos fenómenos. Los resultados obtenidos indicaron que en los

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18

Messié, Monique, and Francisco Chavez. "Global Modes of Sea Surface Temperature Variability in Relation to Regional Climate Indices." Journal of Climate 24, no. 16 (2011): 4314–31. http://dx.doi.org/10.1175/2011jcli3941.1.

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Abstract A century-long EOF analysis of global sea surface temperature (SST) was carried out and the first six modes, independent by construction, were found to be associated with well-known regional climate phenomena: the El Niño–Southern Oscillation (ENSO), the Atlantic multidecadal oscillation (AMO), the Pacific decadal oscillation (PDO), the North Pacific Gyre Oscillation (NPGO), El Niño Modoki, and the Atlantic El Niño. Four of the six global modes are dominated by Pacific changes, the other two (M2 and M6) being associated with the AMO and Atlantic El Niño, respectively. The principal co

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19

Chen, Guanghua. "How Does Shifting Pacific Ocean Warming Modulate on Tropical Cyclone Frequency over the South China Sea?" Journal of Climate 24, no. 17 (2011): 4695–700. http://dx.doi.org/10.1175/2011jcli4140.1.

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The different modulation of El Niño Modoki and canonical El Niño events on tropical cyclone (TC) frequency over the South China Sea (SCS) during boreal summer and fall for 1960–2009 is investigated. The bootstrap resampling method and two-sample permutation procedure are applied to simulate sampling distributions and conduct statistical tests, respectively. Results from the hypothesis testing indicate that the above-normal TC frequency over the SCS occurs during June–August (JJA) for the El Niño Modoki years, whereas the below-normal TC frequency is significant during September–November (SON)

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20

Liu, Lin, Guang Yang, Xia Zhao, et al. "Why Was the Indian Ocean Dipole Weak in the Context of the Extreme El Niño in 2015?" Journal of Climate 30, no. 12 (2017): 4755–61. http://dx.doi.org/10.1175/jcli-d-16-0281.1.

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The Indian Ocean witnessed a weak positive Indian Ocean dipole (IOD) event from the boreal summer to autumn in 2015, while an extreme El Niño occurred over the tropical Pacific. This was different from the case in 1997/98, when an extreme El Niño and the strongest IOD took place simultaneously. The analysis here suggests that the unique sea surface temperature anomaly (SSTA) pattern of El Niño in 2015 might have contributed to the weak IOD that year. El Niño in 2015 had a complex SSTA pattern, with positive warming over the central and eastern tropical Pacific. Such a combination of the classi

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Martín-Gómez, Verónica, Marcelo Barreiro, and Elsa Mohino. "Southern Hemisphere Sensitivity to ENSO Patterns and Intensities: Impacts over Subtropical South America." Atmosphere 11, no. 1 (2020): 77. http://dx.doi.org/10.3390/atmos11010077.

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El Niño flavors influence Subtropical South American (SSA) rainfall through the generation of one or two quasi-stationary Rossby waves. However, it is not yet clear whether the induced wave trains depend on the El Niño pattern and/or its intensity. To investigate this, we performed different sensitivity experiments using an Atmospheric General Circulation Model (AGCM) which was forced considering separately the Canonical and the El Niño Modoki patterns with sea surface temperature (SST) maximum anomalies of 1 and 3 °C. Experiments with 3 °C show that the Canonical El Niño induces two Rossby wa

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Sobaeva, D. A., Yu A. Zyulyaeva, and S. K. Gulev. "THE INFLUENCE OF LOCALIZATION OF POSITIVE SST ANOMALIES IN THE EQUATORIAL PACIFIC OCEAN ON TROPOSPHERESTRATOSPHERIC DYNAMICS IN IDEALIZED MODELING." Journal of Oceanological Research 52, no. 1 (2024): 34–56. http://dx.doi.org/10.29006/1564-2291.jor-2024.52(1).2.

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The paper shows the features of the dynamics of the Arctic stratospheric polar vortex (SPV) in winter under various large-scale ocean surface temperature (SST) anomalies in the equatorial zone of the Pacific Ocean. Based on the analysis of idealized modeling data, it was shown that positive SST anomalies in the Niño 3 (canonical El Niño) and Niño 4 (El Niño Modoki) regions lead to SPV weakening of varying degrees. In the experiments, SST anomalies were increased relative to observational data. With equal amplitude of SST anomalies in experiments with boundary conditions corresponding to canoni

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Ermakova, Tatiana S., Andrey V. Koval, Sergei P. Smyshlyaev, et al. "Manifestations of Different El Niño Types in the Dynamics of the Extratropical Stratosphere." Atmosphere 13, no. 12 (2022): 2111. http://dx.doi.org/10.3390/atmos13122111.

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The behavior of planetary waves and their influence on the global circulation of the Northern Hemisphere during different El Niño types is studied. Three sets of five boreal winters were chosen for each El Niño type: Modoki I and II and canonical El Niño. Based on data of the Japanese 55-year Reanalysis and the Modern-Era Retrospective Analysis for Research and Applications, the spatio-temporal structure of planetary waves and the residual mean circulation were analyzed. The results show that the canonical El Niño type is characterized by the weakest wave activity in March. It is also demonstr

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Matsuyama, Hiroshi. "Causes for the Occurrence of Severe Drought at the Ogasawara (Bonin) Islands during the El Niño Event in 2018–2019." Atmosphere 15, no. 8 (2024): 1005. http://dx.doi.org/10.3390/atmos15081005.

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The Ogasawara (Bonin) Islands, consisting of more than 30 islands and located approximately 1000 km south of central Tokyo, occasionally experience severe droughts. Severe drought does not typically occur during El Niño (EN) events in the Ogasawara Islands because convective activity around the tropical western Pacific is inactive during EN events and correspondingly induces substantial precipitation around the Ogasawara Islands through the Pacific–Japan (P-J) pattern. However, a severe drought in 2018–2019 occurred during EN. In this study, we investigated the causes of drought occurrence. In

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Redondo-Rodriguez, Ana, Scarla J. Weeks, Ray Berkelmans, Ove Hoegh-Guldberg, and Janice M. Lough. "Climate variability of the Great Barrier Reef in relation to the tropical Pacific and El Niño-Southern Oscillation." Marine and Freshwater Research 63, no. 1 (2012): 34. http://dx.doi.org/10.1071/mf11151.

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Understanding the nature and causes of recent climate variability on the Great Barrier Reef (GBR), Australia, is fundamental to assessing the impacts of future climate change on this complex ecosystem. New analytical tools, improved data quality and resolution, longer time-series and new variables provide an opportunity to re-assess existing paradigms. Here, we examined sea surface temperature (SST), sea level pressure, surface winds, sea surface height and ocean currents for the period from 1948 to 2009. We focussed on the relationship between GBR surface climate and the wider tropical Pacifi

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Vega, Inmaculada, David Gallego, Pedro Ribera, F. de Paula Gómez-Delgado, Ricardo García-Herrera, and Cristina Peña-Ortiz. "Reconstructing the Western North Pacific Summer Monsoon since the Late Nineteenth Century." Journal of Climate 31, no. 1 (2017): 355–68. http://dx.doi.org/10.1175/jcli-d-17-0336.1.

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Abstract A new index, the western North Pacific directional index (WNPDI), based on historical wind direction observations taken aboard sailing ships, has been developed to characterize the western North Pacific summer monsoon (WNPSM) since 1898. The WNPDI measures the persistence of the surface westerly winds in the region 5°–15°N, 100°–130°E and easterly winds in the region 20°–30°N, 110°–140°E, exhibiting a consistent relationship with the summer precipitation in the areas affected by the WNPSM throughout the entire twentieth century. Its length doubles that of the previous WNPSM index (194

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Prasetyo, Budi, and Nikita Pusparini. "RESPON CURAH HUJAN SULAWESI TERHADAP EL NIÑO MODOKI." Jurnal Meteorologi dan Geofisika 20, no. 1 (2019): 21. http://dx.doi.org/10.31172/jmg.v20i1.517.

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Karnauskas, Kristopher B. "Can we distinguish canonical El Niño from Modoki?" Geophysical Research Letters 40, no. 19 (2013): 5246–51. http://dx.doi.org/10.1002/grl.51007.

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Feng, Juan, and Jianping Li. "Contrasting Impacts of Two Types of ENSO on the Boreal Spring Hadley Circulation." Journal of Climate 26, no. 13 (2013): 4773–89. http://dx.doi.org/10.1175/jcli-d-12-00298.1.

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Abstract The possible influences of two types of ENSO [i.e., the canonical ENSO and ENSO Modoki (EM)] on Hadley circulation (HC) during the boreal spring are investigated during 1979–2010. El Niño events are featured with a symmetric pattern in equatorial zonal-mean sea surface temperature anomalies (SSTA), with a maximum around the equator. In contrast, the zonal-mean SSTA associated with El Niño Modoki events shows an asymmetric structure with a maximum around 10°N. The contrasting underlying thermal structures corresponding with ENSO and EM have opposite impacts on the simultaneous HC. In E

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Pascolini-Campbell, M., D. Zanchettin, O. Bothe, et al. "Toward a classification of the Central Pacific El Niño." Earth System Dynamics Discussions 3, no. 2 (2012): 979–98. http://dx.doi.org/10.5194/esdd-3-979-2012.

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Abstract. We investigate the various methods currently available for distinguishing between the Central Pacific (CP) El Niño (or "El Niño Modoki") and the canonical El Niño by considering 10 different methods and 5 sea surface temperature (SST) datasets from 1880 to 2010. Years which are classified as CP El Niños with the greatest convergence between method and SST dataset are considered to provide a more robust identification of these events. The results identify 13 yr which are classified the most consistently as CP events: 1885/1886, 1914/1915, 1940/1941, 1958/1959, 1963/1964, 1968/1969, 19

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Wang, Dongxiao, Yinghao Qin, Xianjun Xiao, Zuqiang Zhang, and Xiangyu Wu. "El Niño and El Niño Modoki variability based on a new ocean reanalysis." Ocean Dynamics 62, no. 9 (2012): 1311–22. http://dx.doi.org/10.1007/s10236-012-0566-0.

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Takahashi, K., A. Montecinos, K. Goubanova, and B. Dewitte. "ENSO regimes: Reinterpreting the canonical and Modoki El Niño." Geophysical Research Letters 38, no. 10 (2011): n/a. http://dx.doi.org/10.1029/2011gl047364.

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Arora, Kopal, and Prasanjit Dash. "The Indian Ocean Dipole: A Missing Link between El Niño Modokiand Tropical Cyclone Intensity in the North Indian Ocean." Climate 7, no. 3 (2019): 38. http://dx.doi.org/10.3390/cli7030038.

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This study is set out to understand the impact of El Niño Modoki and the Tropical Cyclone Potential Intensity (TCPI) in the North Indian Ocean. We also hypothesized and tested if the Indian Ocean Dipole (IOD) reveals a likely connection between the two phenomena. An advanced mathematical tool namely the Empirical Mode Decomposition (EMD) is employed for the analysis. A major advantage of using EMD is its adaptability approach to deal with the non-linear and non-stationary signals which are similar to the signals used in this study and are also common in both atmospheric and oceanic sciences. T

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Romanov, Yury A., Nina A. Romanova, and Peter Romanov. "Changing effect of El Niño on Antarctic iceberg distribution: From canonical El Niño to El Niño Modoki." Journal of Geophysical Research: Oceans 119, no. 1 (2014): 595–614. http://dx.doi.org/10.1002/2013jc009429.

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Cao, Qing, Zhenchun Hao, Feifei Yuan, et al. "Impact of ENSO regimes on developing- and decaying-phase precipitation during rainy season in China." Hydrology and Earth System Sciences 21, no. 11 (2017): 5415–26. http://dx.doi.org/10.5194/hess-21-5415-2017.

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Abstract. This study investigated the influence of five El Niño–Southern Oscillation (ENSO) types on rainy-season precipitation in China: central Pacific warming (CPW), eastern Pacific cooling (EPC), eastern Pacific warming (EPW), conventional ENSO and ENSO Modoki. The multi-scale moving t test was applied to determine the onset and withdrawal of rainy season. Results showed that the precipitation anomaly can reach up to 30 % above average precipitation during decaying CPW and EPW phases. Developing EPW could cause decreasing precipitation over large areas in China with 10–30 % lower than aver

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Navarro-Monterroza, Estefanía, Paola A. Arias, and Sara C. Vieira. "El Niño-Oscilación del Sur, fase Modoki, y sus efectos en la variabilidad espacio-temporal de la precipitación en Colombia." Revista de la Academia Colombiana de Ciencias Exactas, Físicas y Naturales 43, no. 166 (2019): 120. http://dx.doi.org/10.18257/raccefyn.704.

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Se analizó la posible influencia del fenómeno de El Niño-Oscilación del Sur (ENOS) en la variabilidad espaciotemporal de la precipitación en Colombia a partir de registros de estaciones in situ durante el período 1970-2015 y de datos provenientes de registros satelitales disponibles a partir de 1998. Mediante los índices de temperatura superficial del mar (TSM) asociados al fenómeno ENOS, se evaluaron las anomalías en la precipitación por trimestre para cada tipo de evento, así como las correlaciones mensuales simultáneas y rezagadas entre cada índice y las anomalías en la precipitación. Con b

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Seow, Marvin Xiang Ce. "A new type of tropical Pacific warming—El Niño Modoki." Physics Today 71, no. 12 (2018): 50–52. http://dx.doi.org/10.1063/pt.3.4092.

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Kim, Do-Woo, Ki-Seon Choi, and Hi-Ryong Byun. "Effects of El Niño Modoki on winter precipitation in Korea." Climate Dynamics 38, no. 7-8 (2011): 1313–24. http://dx.doi.org/10.1007/s00382-011-1114-1.

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Feng, Juan, Wen Chen, and Xiaocong Wang. "Reintensification of the Anomalous Western North Pacific Anticyclone during the El Niño Modoki Decaying Summer: Relative Importance of Tropical Atlantic and Pacific SST Anomalies." Journal of Climate 33, no. 8 (2020): 3271–88. http://dx.doi.org/10.1175/jcli-d-19-0154.1.

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AbstractThe El Niño Modoki–induced anomalous western North Pacific anticyclone (WNPAC) undergoes an interesting reintensification process in the El Niño Modoki decaying summer, the period when El Niño Modoki decays but warm sea surface temperature (SST) anomalies over the tropical North Atlantic (TNA) and cold SST anomalies over the central-eastern Pacific (CEP) dominate. In this study, the region (TNA or CEP) in which the SST anomalies exert a relatively important influence on reintensification of the WNPAC is investigated. Observational analysis demonstrates that when only anomalous CEP SST

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40

Taschetto, Andréa S., Reindert J. Haarsma, Alexander Sen Gupta, Caroline C. Ummenhofer, Khalia J. Hill, and Matthew H. England. "Australian Monsoon Variability Driven by a Gill–Matsuno-Type Response to Central West Pacific Warming." Journal of Climate 23, no. 18 (2010): 4717–36. http://dx.doi.org/10.1175/2010jcli3474.1.

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Abstract The objective of this study is to investigate the mechanisms that cause the anomalous intensification of tropical Australian rainfall at the height of the monsoon during El Niño Modoki events. In such events, northwestern Australia tends to be wetter in January and February when the SST warming is displaced to the central west Pacific, the opposite response to that associated with a traditional El Niño. In addition, during the bounding months, that is, December and March, there is below-average rainfall induced by an anomalous Walker circulation. This behavior tends to narrow and inte

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41

Ramsay, Hamish A., Michael B. Richman, and Lance M. Leslie. "Seasonal Tropical Cyclone Predictions Using Optimized Combinations of ENSO Regions: Application to the Coral Sea Basin." Journal of Climate 27, no. 22 (2014): 8527–42. http://dx.doi.org/10.1175/jcli-d-14-00017.1.

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Abstract This study examines combining ENSO sea surface temperature (SST) regions for seasonal prediction of Coral Sea tropical cyclone (TC) frequency. The Coral Sea averages ~4 TCs per season, but is characterized by strong interannual variability, with 1–9 TCs per season, over the period 1977–2012. A wavelet analysis confirms that ENSO is a key contributor to Coral Sea TC count (TCC) variability. Motivated by the impact of El Niño Modoki on regional climate anomalies, a suite of 38 linear models is constructed and assessed on its ability to predict Coral Sea seasonal TCC. Seasonal prediction

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42

Lima, Daniel Milano Costa de, Mateus Dias Nunes, and Glauber Lopes Mariano. "Impacto do ENOS na Variabilidade da Coluna Total de Ozônio Sobre a Região Nordeste do Brasil - Parte 2: La Niña Canônico e Modoki." Revista Brasileira de Meteorologia 35, spe (2020): 945–53. http://dx.doi.org/10.1590/0102-778635500104.

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Resumo Este estudo apresenta a segunda etapa da avaliação espaço-temporal das tendências a longo prazo nos valores da Coluna Total de Ozônio (CTO) sobre o Nordeste Brasileiro (NEB) durante a atuação do modo de variabilidade atmosférica El Niño - Oscilação Sul (ENOS), com foco na fase La Niña (modalidades Canônica e Modoki). O objetivo é analisar a variação anual e os efeitos desse fenômeno na região de estudo no período entre 1997 e 2018. Os dados utilizados são provenientes de sensoriamento remoto, gerados pelos sensores Total Ozone Mapping Spectrometer (TOMS) e Ozone Monitoring Instrument (O

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43

Feng, Juan, Wen Chen, C. Y. Tam, and Wen Zhou. "Different impacts of El Niño and El Niño Modoki on China rainfall in the decaying phases." International Journal of Climatology 31, no. 14 (2010): 2091–101. http://dx.doi.org/10.1002/joc.2217.

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44

Zubiaurre, I., and N. Calvo. "The El Niño-Southern Oscillation (ENSO) Modoki signal in the stratosphere." Journal of Geophysical Research: Atmospheres 117, no. D4 (2012): n/a. http://dx.doi.org/10.1029/2011jd016690.

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Behera, Swadhin, and Toshio Yamagata. "Imprint of the El Niño Modoki on decadal sea level changes." Geophysical Research Letters 37, no. 23 (2010): n/a. http://dx.doi.org/10.1029/2010gl045936.

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46

Sumesh, K. G., and M. R. Ramesh Kumar. "Tropical cyclones over north Indian Ocean during El-Niño Modoki years." Natural Hazards 68, no. 2 (2013): 1057–74. http://dx.doi.org/10.1007/s11069-013-0679-x.

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47

Huo, Wenjuan, and Ziniu Xiao. "Modulations of solar activity on El Niño Modoki and possible mechanisms." Journal of Atmospheric and Solar-Terrestrial Physics 160 (July 2017): 34–47. http://dx.doi.org/10.1016/j.jastp.2017.05.008.

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48

Bowman, K. W., J. Liu, A. A. Bloom, et al. "Global and Brazilian Carbon Response to El Niño Modoki 2011-2010." Earth and Space Science 4, no. 10 (2017): 637–60. http://dx.doi.org/10.1002/2016ea000204.

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49

Amaya, Dillon J., and Gregory R. Foltz. "Impacts of canonical and Modoki El Niño on tropical Atlantic SST." Journal of Geophysical Research: Oceans 119, no. 2 (2014): 777–89. http://dx.doi.org/10.1002/2013jc009476.

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50

Mayer, Michael, Kevin E. Trenberth, Leopold Haimberger, and John T. Fasullo. "The Response of Tropical Atmospheric Energy Budgets to ENSO*." Journal of Climate 26, no. 13 (2013): 4710–24. http://dx.doi.org/10.1175/jcli-d-12-00681.1.

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Abstract The variability of zonally resolved tropical energy budgets in association with El Niño–Southern Oscillation (ENSO) is investigated. The most recent global atmospheric reanalyses from 1979 to 2011 are employed with removal of apparent discontinuities to obtain best possible temporal homogeneity. The growing length of record allows a more robust analysis of characteristic patterns of variability with cross-correlation, composite, and EOF methods. A quadrupole anomaly pattern is found in the vertically integrated energy divergence associated with ENSO, with centers over the Indian Ocean

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