in Last Interglacial compared to preindustrial periodMain causes are that orbitally‐induced enhancement of equatorial westward currents intensifies mean advection of anomalous cold waterThe concurrent suppression in El Nio–Southern Oscillation is unlikely to cause a weakening in the Indian Oce...
The Indian Ocean Dipole (IOD) strongly affects the climate of the Indo-Pacific. Observations suggest a shift towards stronger and earlier positive IOD (pIOD) events alongside an increased amplitude of sea surface temperature (SST) anomalies, but uncertainty remains, impeding assessments of ongoing ch...
The Indian Ocean Dipole and malaria risk in the highlands of western Kenya. Proc Natl Acad Sci U S A 106, 1857–1862 (2009). Article ADS CAS Google Scholar Pascual, M. et al. Shifting patterns: malaria dynamics and rainfall variability in an African highland. Proc R Soc B 275, 123...
Earlier proxy-observational studies, and a sole modeling study, suggest that the Indian Ocean Dipole (IOD), an important global climate driver, exhibited multi-scale temporal variability during the Last Millennium (LM; CE 0851–1849, with relatively high number of strong positive IOD events during...
[translate] aIndian Ocean Dipole Response to Global Warming: Analysis of Ocean–Atmospheric Feedbacks in a Coupled Model 印度洋对全球性变暖的偶极反应: 对海洋大气反馈的分析在一个被结合的模型[translate]
The Indian Ocean sea surface temperature (SST) variability has been represented with the two dominant variability modes: the Indian Ocean basin-wide (IOBW) and dipole (IOD) modes. Here we investigate future changes of the two modes together with mean state and El Nio and Southern Oscillation (...
Patterns of concerted fluctuation in populations—synchrony—can reveal impacts of climatic variability on disease dynamics. We examined whether malaria transmission has been synchronous in an area with a common rainfall regime and sensitive to the Indian Ocean Dipole (IOD), a global climatic ...
Most of the variability in the model short rains is linked to the basinwide large-scale coupled mode, that is, the Indian Ocean dipole (IOD) in the tropical Indian Ocean. The analysis of observed data and model results reveals that the influence of the IOD on short rains is overwhelming ...
Ocean41. A positive Indian Ocean Dipole event begins in austral autumn–winter and peaks during austral spring. In the Western Indian Ocean, south-easterly winds bring warmer waters resulting in increased sea surface temperatures and convection41. During a negative Indian Ocean Dipole phase, the ...
The tropical Indian Ocean dipole/zonal mode (IOD) is phase locked with the austral winter and spring seasons. This study describes three types of the IOD in terms of their peak time and duration. In particular, the authors focus on a new type that develops in May-June and matures in July...