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Seasonal Dependence of the MJO-ENSO Relationship

Harry H. Hendon, +2 more
- 01 Feb 2007 - 
- Vol. 20, Iss: 3, pp 531-543
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TLDR
In this paper, the Madden-Julian oscillation (MJO) activity in late boreal spring leads El Nino in the subsequent autumn-winter for the period 1979-2005.
Abstract
Observations of the development of recent El Nino events suggest a pivotal role for the Madden–Julian oscillation (MJO). Previous attempts to uncover a systematic relationship between MJO activity and the El Nino–Southern Oscillation (ENSO), however, have yielded conflicting results. In this study the MJO–ENSO relationship is stratified by season, and the focus is on MJO activity in the equatorial western Pacific. The results demonstrate that MJO activity in late boreal spring leads El Nino in the subsequent autumn–winter for the period 1979–2005. Spring is the season when MJO activity is least asymmetric with respect to the equator and displays the most sensitivity to SST variations at the eastern edge of the warm pool. Enhanced MJO activity in the western Pacific in spring is associated with an eastward-expanded warm pool and low-frequency westerly surface zonal wind anomalies. These sustained westerly anomalies in the western Pacific are hypothesized to project favorably onto a developing El N...

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Two Types of El Niño Events: Cold Tongue El Niño and Warm Pool El Niño

TL;DR: In this paper, two types of El Nino events are classified based on spatial patterns of the sea surface temperature (SST) anomaly, namely cold tongue (CT) and warm pool (WP) events.
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On the Remote Drivers of Rainfall Variability in Australia

TL;DR: This article identified and documented a suite of large-scale drivers of rainfall variability in the Australian region, including El Nino-Southern Oscillation (ENSO), Indian Ocean dipole (IOD), Madden-Julian oscillation and atmospheric blocking.
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Madden–Julian Oscillation: Bridging Weather and Climate

TL;DR: The Madden-Julian oscillation exerts broad influences on global weather and climate as its center of convection moves from the tropical Indian Ocean into the Pacific. as mentioned in this paper provides a brief summary of the connections between the Madden and climate phenomena.
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The Impact of Convection on ENSO: From a Delayed Oscillator to a Series of Events

TL;DR: The NCAR Community Climate System Model, version 3 (CCSM3) exhibits persistent errors in its simulation of the El Nino-Southern Oscillation (ENSO) mode of coupled variability.
References
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Journal ArticleDOI

The NCEP/NCAR 40-Year Reanalysis Project

TL;DR: The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art global data assimilation system and a database as complete as possible, except that the horizontal resolution is T62 (about 210 km) as discussed by the authors.
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Improved Global Sea Surface Temperature Analyses Using Optimum Interpolation

TL;DR: The new NOAA operational global sea surface temperature (SST) analysis is described in this paper, which uses 7 days of in situ (ship and buoy) and satellite SST.
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Variations in Tropical Sea Surface Temperature and Surface Wind Fields Associated with the Southern Oscillation/El Niño

TL;DR: In this article, the evolution of sea surface temperature (SST) anomalies, surface wind fields, and precipitation anomaly patterns during major warm episodes in the eastern and central tropical Pacific are described in terms of composite SST and wind fields (30°N−30°S) for six warm episodes since 1949, and time series and cross-spectral analyses of mean monthly data along six shipping lanes which cross the equator between the South American coast and 170°W.
Journal ArticleDOI

Description of Global-Scale Circulation Cells in the Tropics with a 40–50 Day Period

TL;DR: In this article, a long time series (5-10 years) of station pressure and upper air data from stations located in the tropics are subjected to spectral and cross-spectral analysis to investigate the spatial extent of a previously detected oscillation in various variables with a period range of 40-50 days.
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