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El Niño (/ ɛ l ˈ n iː n j oʊ /; The composite of Modoki vertical velocity (Fig 3, right panel) shows an upward motion through the deep troposphere centered at 180°W, shifted westward when compared to the rising air in the conventional ENSOcomposite circulation The distribution of velocity potential at 0 hPa also confirms anomalous divergence shifted slightly to the westThe ENSO Modoki events, just as by the ENSO and IOD 50 As seen in Figures 13b and 13c, it is inferred that the events Nakamura and Shimpo, 04;

Climate Dynamics Of Enso Modoki Phenomena Oxford Research Encyclopedia Of Climate Science
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Enso modoki- Trilobes of Modoki In Chapter 12 of the book we model — via LTE — the canonical El Nino Southern Oscillation (ENSO) behavior, fitting to closelycorrelated indices such as NINO34 and SOI Another El Nino index was identified circa 07 that is not closely correlated to the wellknown ENSO indices The El Niño Modoki involves oceanatmosphere coupled processes which include a unique tripolar sea level pressure pattern during the evolution, analogous to the Southern Oscillation in the case of El Niño Hence the total entity is named as El Niño–Southern Oscillation (ENSO) Modoki




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Central Pacific El Niños have different effects than Eastern Pacific El Niños For example, Modoki El Niño tends to have more hurricanes in Atlantic and Gulf of Mexico regions Modoki El Niños may have been around going back to the 13th century, possibly before The El Niño which developed in 15 is a Modoki version of the phenomenonThe El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of oceanatmosphere coupled variability in the tropical Pacific Ocean The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impactsEl Nino Modoki activities tend to moisten the lower and middle strato˜ sphere, but dry the upper stratosphere It was also found that the canonical El Nino˜ signal can overlay linearly on the QBO signal in the stratosphere, whereas the interaction between the El Nino Modoki and QBO signals is nonlinear Because of these˜
In 17, 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 The El Niño (La Niña) Modoki (ENSO Modoki, hereafter EM) 1 is a newly acknowledged phenomenon characterized by warm (cool) central Pacific sea surface temperature (SST) flanked by cool (warm)ENSO Modoki events from those of the ENSO and Indian Ocean Dipole (IOD) El Nin˜o Modoki events introduce an anomalous blocking over central eastern Australia, which suppresses the storm track activity from southwest till centraleast, reducing the stormassociated rainfall in southeastern tip and portions of the southeast On the
With these research findings in mind, ENSO Modoki is definitely a climatic process to be aware of when evaluating seasonal climate risk to understand impacts on seasonal conditions In terms of impact on rainfall and climate in cotton regions, researchers at the Australian Bureau of Meteorology and University of NSW found ENSO Modoki is the Since 07 a new type of ENSO, ie ENSO Modoki, has been identified and subsequent observational studies have reported contrasting effects on climate patterns worldwide (eg Wang and Hendon, 07, Ashok et al, 07, Ashok This suggests that El Nino Modoki is actually the signature ENSO mode of the warm ocean phase (warm PDO) as opposed to the cool phase measured prior to 1980 Bill, I don't know It could be that there is a complex mixture of things going on that make every el ninola nina cycle different I think it likely the solar factor is important




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El Nino Wikipedia
The monthly Nino 3 index (5 °N–5 °S, 150°–90 °W), hereafter N3I, and the ENSO Modoki index, hereafter EMI, were used to identify monthly occurrences of canonical El Niño events and El Niño Modoki events, respectively N3I was defined as the areamean SSTA over the region (5 °S–5 °N, 150°–90 °W) Trilobes of Modoki In Chapter 12 of the book we model — via LTE — the canonical El Nino Southern Oscillation (ENSO) behavior, fitting to closelycorrelated indices such as NINO34 and SOI Another El Nino index was identified circa 07 that is not closely correlated to the wellknown ENSO indices On the other hand, the ENSO Modoki shows a negative skewness Since there are less cooccurrence between La Niña Modoki and the negative IOD (Supplementary Table 1), the influences of ENSO Modoki on the wheat yields may have some independence from IOD, and they may increase in future with increasing variability (Fig 4e,f)




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El Nino Wikipedia
Noncanonical El Niño;s, including Modoki, are characterized by the warmest SST anomalies in the central equatorial Pacific, whereas the traditional El Niño events peak in the eastern equatorial Pacific In this study, the impacts of canonical and Modoki El Niño on tropical Atlantic SST were quantified using composite analysis The Indian summer monsoon (ISM) rainfall is often influenced by El NiñoSouthern Oscillation (ENSO) on the interannual time scale Physical mechanisms that link the canonical El Niño and ISM rainfall have been well documented Very few studies have discussed the pathways that link El Niño Modoki and ISM rainfall variations In recent years, El Niño Modoki (a type of pseudoEl Niño) has been distinguished as a unique largescale ocean warming phenomenon happening in the central tropical Pacific that is quite different from the traditional El Niño In this study, EOF analysis was used to successfully separate El Niño and El Niño Modoki The abilities of the NINO3 index, NINO34 index, NINO12




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Abstract and Figures From the th to 21st century, the tropical Pacific witnessed a hitherto unobserved interannual coupled manifestation, which is now known as the ElEl Nino Modoki events are a rarer subset of regular El Nino's, and are marked by warming water in the Pacific, but not along the Equator Instead, the warming is in the midPacific and the warming is not as strong as in regular El Nino events Many times in a strong Modoki, water actually cools below normal off the coast of Peru, which is the Modoki is Japanese for "same but different" Modoki events are a rarer subset of regular El Niño's and are marked by warmer water centered in the central Pacific With a Modoki El Niño, the core of strongest warming is located within the center of the Pacific




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Abstract From the th to 21st century, the tropical Pacific witnessed a hitherto unobserved interannual coupled manifestation, which is now known as the El Niño Modoki (EM) It is now referred to as a new type of El Niño (EL) and not necessarily a distinct phenomenon altogetherENSOneutral is favored through the Northern Hemisphere summer (78% chance for the JuneAugust season) and fall (50% chance for the SeptemberNovember season)* During September to March 21, the core of the strongest negative SST anomalies shifted from the eastern to The study diagnoses the relative impacts of the four known tropical IndoPacific drivers, namely, El Niño Southern Oscillation (ENSO), ENSO Modoki




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El NinoSouthern Oscillation (ENSO) is known to be the largest source of interannual variability in the tropical troposphere However, the variability in the tropical Pacific since 1979 seems to be associated not only with "canonical" ENSO events but also with a variation thereof known as ENSO Modoki, which is characterized by warm anomalies in the central Pacific, west from thoseA comparison of the effects of El Niño and El Niño Modoki on subdaily extreme precipitation occurrences across the contiguous United States Lejiang Yu1,2, Shiyuan Zhong2, Warren E Heilman3, and Xindi Bian3 1Key Laboratory for Polar Science of SOA, Polar Research Institute of China, Shanghai, China, 2Department of Geography, Environment and Spatial Sciences, MichiganThe ENSO Modoki events significantly influence the temperature and precipitation over many parts of the globe Depending on the season, the impacts over regions such as the Far East including Japan, New Zealand, western coast of United States, etc, are opposite to those of the conventional ENSO The difference maps between the two periods of




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Climate Dynamics Of Enso Modoki Phenomena Oxford Research Encyclopedia Of Climate Science
El Nino Modoki has its own distinct pattern and is affecting many parts of the world For example, the west coastal region of the United States receives more rainfall during El Niño but the region becomes dry during El Niño Modocci Rainfall in India and South Africa is also being affected due to ENSO Modoki El Niño Modoki is a coupled oceanatmosphere phenomenon in the tropical Pacific It is different from another coupled phenomenon in the tropical Pacific namely, El Niño Conventional El Niño is characterized by strong anomalous warming in the eastern equatorial Pacific The Modokilook continues but conventional El Nino is over Fig 12 The Nino34 SSTA is at zero indicating neutral ENSO although the much warmer central Pacific maintains the Modokilook Fig 3 The North Pacific SSTA analysis identifying the Modokilook to ENSO Fig 4 Air mass trajectory as related to the NCEP CFS V2 SSTA forecast for DEC/JAN/FEB 19




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SST anomalies of Modoki events are different from those of canonical ENSO, the response of the atmosphere to the two types of ENSO is also different (Trenberth and Smith 06, Xie et al 12, Zubiaurre and Calvo 12) Modoki activity has been increasing in frequency, especially since the 1980s (Ashok and Yamagata 09, Yeh et al 09) The The El Niño–Southern Oscillation (ENSO) Modoki phenomenon has a substantial influence on regional climate In this study, the results derived from observational and reanalyzed datasets show that the boreal winter climate anomalies over the Pacific and its rim in the different phases of ENSO Modoki are asymmetric during 1979–17 El Nino Modoki Fenomena Baru JAKARTA, KOMPAScom — Fenomena El Nino atau menghangatnya suhu muka laut di Samudra Pasifik mulai menggejala akhir Mei lalu dan cenderung menguat pada bulan ini Namun, melihat pola dan lokasi "kolam panas"—areal permukaan laut yang menghangat—ada kecenderungan versi baru El Nino yang disebut El Nino Modoki



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1
El Niño–Southern Oscillation (ENSO) is an irregular periodic variation in winds and sea surface temperatures over the tropical eastern Pacific Ocean, affecting the climate of much of the tropics and subtropics The warming phase of the sea temperature is known as El Niño and the cooling phase as La Niña ENSO Flavor of the Month No, we're not just talking about ice cream in this post (mmm yum), but about the different types, or flavors, of the El NiñoSouthern Oscillation (ENSO) These different flavors of ENSO are usually based on the location where tropical Pacific sea surface temperature (SST) anomalies are the largestAshok et al, 07, atmospheric response to the El Nin˜o Modoki is baroclinic in may induce teleconnections in higher latitudes the tropics, whereas it has an equivalent barotropic structure 51




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A Japanese scientist called it El Niño Modoki a Japanese word that means "a similar but different thing" A conventional El Niño starts with unusually warm waters in the eastern Pacific, all the way to the coast of South America It triggers changes in climate for the United States and many other parts of the world Weekly ENSO Diagnostics El Nino Modoki is trying to develop Discussion The El Nino Modoki Index eclipses 1 and given the stark difference in the buoyant warming near the Dateline and near normal SSTA in the eastern equatorial Pacific El Nino Modoki appears to be developing The evolution follows a weak El Nino present the past 4 monthsOn Concepts of ENSO, El NinoLa Nina,



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Modoki in Japanese means "a similar but different thing" El Niño Modoki is also referred to as Date Line El Niño (Larkin and Harrison 05), central Pacific El Niño (Yu and Kao 07), and warm pool El Niño (Kug et al 09)Spanish ) is the warm phase of the El Niño–Southern Oscillation (ENSO) and is associated with a band of warm ocean water that develops in the central and eastcentral equatorial Pacific (approximately between the International Date Line and 1°W), including the area off the Pacific coast of South AmericaThe ENSO is the cycle of warm and cold seaEna(ie,ElNiño‐SouthernOscillation(ENSO)and"ElNiño Modoki") but rather the nonlinear evolution of ENSO We introduce two new uncorrelated indices (E and C), based on the leading EOFs, that respectively account for extreme warmeventsintheeasternandcold/moderatewarmeventsin the central equatorial Pacific, corresponding to regimes with



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Ebook Link https//mithilacraftcom/product/simplifiedclimatologyebook/This is the 31st in the series of lectures;The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of oceanatmosphere coupled variability in the tropical Pacific OceanPartial suspension of access to the data and services on our website JAMSTEC is currently suspending access to some of the data, service, etc on our website, due to




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The possible ENSO Modoki influence on the stratospheric circulation, tracer constituents, and perhaps, eventually, the troposphere The cold phase of ENSO Modoki (La Niña Modoki), characterized by an anomalous cooling in the central Pacific and flanked by anomalous warming in the eastern and western Pacific Ashok and Yamagata, 09, However, the variability in the tropical Pacific since 1979 seems to be associated not only with "canonical" ENSO events but also with a variation thereof known as ENSO Modoki, which is characterized by warm anomalies in the central Pacific, west from those occurring during a What is a Modoki El Nino?




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El Nino Modoki events are a rarer subset of regular El Nino's, and are marked by warming water in the Pacific, but not along the Equator Warming during a regular Nino is observed on the eastern side of the Pacific Modoki events involve cooler SST's there and the warmer SST'S in the Central Pacific El Niño Modoki is a coupled oceanatmosphere phenomenon in the tropical Pacific It is different from another coupled phenomenon in the tropical Pacific namely, El Niño Conventional El Niño is characterized by strong anomalous warming in the eastern equatorial Pacific In addition, new insights into how ENSO Modoki and the IPO modulate TC activity according to phase and season are identified Importantly, we show that depending on phase, the IPO can enhance or alter the spatial modulation of TC genesis during ENSO/ENSO Modoki events, in favour of the northeast/southwest modulations typical of IPO positive




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