Search results for "Indian Ocean Dipole"

showing 6 items of 6 documents

A sea surface temperature reconstruction for the southern Indian Ocean trade wind belt from corals in Rodrigues Island (19°S, 63°E)

2016

Abstract. The western Indian Ocean has been warming rapidly over recent decades, causing a greater number of extreme climatic events. It is therefore of paramount importance to improve our understanding of links between Indian Ocean sea surface temperature (SST) variability, climate change and sustainability of tropical coral reef ecosystems. Here we present monthly resolved coral Sr ∕ Ca records from two different locations from Rodrigues Island (63° E, 19° S) in the south-central Indian Ocean trade wind belt. We reconstruct SST based on a linear relationship with the Sr ∕ Ca proxy with records starting from 1781 and 1945, respectively. We assess relationships between the observed long-ter…

010506 paleontology010504 meteorology & atmospheric sciences550Corallcsh:LifeClimate changeMonsoon010502 geochemistry & geophysics01 natural sciencesddc:570lcsh:QH540-549.514. Life underwaterEcology Evolution Behavior and SystematicsEarth-Surface Processes0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySubtropical Indian Ocean Dipolelcsh:QE1-996.5Coral reeflcsh:GeologySea surface temperaturelcsh:QH501-531Oceanography13. Climate actionClimatologyIndian Ocean Dipolelcsh:EcologyGeologyTeleconnection
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Oceanic and atmospheric linkages with short rainfall season intraseasonal statistics over Equatorial Eastern Africa and their predictive potential

2014

Despite earlier studies over various parts of the world including equatorial Eastern Africa (EEA) showing that intraseasonal statistics of wet and dry spells have spatially coherent signals and thus greater predictability potential, no attempts have been made to identify the predictors for these intraseasonal statistics. This study therefore attempts to identify the predictors (with a 1-month lead time) for some of the subregional intraseasonal statistics of wet and dry spells (SRISS) which showed the greatest predictability potential during the short rainfall season over EEA. Correlation analysis between the SRISS and seasonal rainfall totals on one hand and the predefined predictors on th…

Atmospheric ScienceMagnitude (mathematics)Seasonalitymedicine.diseaseSea surface temperatureBayesian multivariate linear regressionClimatologyStatisticsmedicineEnvironmental sciencePrecipitationIndian Ocean DipolePredictabilityPartial correlationInternational Journal of Climatology
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Modification of the southern African rainfall variability/ENSO relationship since the late 1960s

2000

Analysis of 149 raingauge series (1946–1988) shows a weak positive correlation between late summer rainfalls (January–March) in tropical southern Africa and the Southern Oscillation Index (SOI). The correlation coefficients have been unstable since World War II. They were close to zero before 1970 and significant thereafter. Before 1970, southern African late summer rainfalls were more specifically correlated with regional patterns of sea surface temperature (SST), mainly over the southwestern Indian Ocean. After 1970, teleconnections with near global SST anomaly patterns, i.e. over the central Pacific and Indian oceans, dominate the regional connections. The increase in the sensitivity of …

Atmospheric ScienceSea surface temperatureOceanographyRain gaugeSubtropical Indian Ocean DipoleEl NiñoAtmospheric circulationClimatologyExtratropical cycloneSubtropicsGeologyTeleconnectionClimate Dynamics
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Precipitation responses to ENSO and IOD in the Maldives: Implications of large-scale modes of climate variability in weather-related preparedness

2020

Abstract This research seeks to address the extent to which indices of large-scale modes of climate variability (El Nino Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD)) can be linked to physical differences in the local mean and extreme rainfall conditions experienced in the Maldives in order to suggest implications for disaster risk reduction (DRR). While some significant differences in precipitation metrics do occur at the local level between different phases of the large-scale modes of climate variability studied, they do not occur for all sites studied. While the constrained availability of historical meteorological data in the region is a limiting factor in this analysis, th…

Limiting factor021110 strategic defence & security studies010504 meteorology & atmospheric sciencesDisaster risk reduction0211 other engineering and technologiesGeology02 engineering and technologyGeotechnical Engineering and Engineering Geology01 natural sciencesEl Niño Southern OscillationClimatologyPreparednessEnvironmental sciencePrecipitationIndian Ocean DipoleScale (map)Safety ResearchSea level0105 earth and related environmental sciencesInternational Journal of Disaster Risk Reduction
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Nile Basin Climates

2009

The climate of the Nile Basin is characterised by a strong latitudinal wetness gradient. Whereas the areas north of 18°N remain dry most of the year, to the south there is a gradual increase of monsoon precipitation amounts. Rainfall regimes can be divided into 9 types, among which summer peak regimes dominate. In the southern half of the basin, mesoscale circulation features and associated contrasts in local precipitation patterns develop as a result of a complex interplay involving topography, lakes and swamps. Precipitation changes and variability show up as 3 distinct modes of variability. Drying trends since the 1950s are found in central Sudan and to some extent the Ethiopian Highland…

Monsoon of South Asiageographygeography.geographical_feature_categoryTropicsSahara pump theoryStructural basinSea surface temperature[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyIndian Ocean DipolePrecipitation[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyOceanic basinGeology
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Interannual variability of rainfall in the eastern horn of Africa and indicators of atmospheric circulation

1993

Relationships between rainfall variations in the Eastern Horn of Africa, the Southern Oscillation, and the Indian Ocean temperature and pressure surface fields are studied for the period 1932–83. Rainfall data consist of stations and regional indices calculated for three selected areas experiencing quite different rainfall patterns. The results indicate significant negative correlations between northern autumn rains in Somalia and the Southern Oscillation during the same season. These rains are also negatively correlated with pressure in the Western Indian Ocean, and positively correlated in the Eastern Indian Ocean. The reverse pattern is shown with sea-surface temperature. This agrees ver…

Wet seasonAtmospheric ScienceOceanographyGeographySubtropical Indian Ocean DipoleEl NiñoAtmospheric circulationClimatologyIndian Ocean DipoleStructural basinMonsoonTeleconnectionInternational Journal of Climatology
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