Search results for "CMIP5"

showing 7 items of 7 documents

Future Projection of precipitation changes in the Júcar and Segura River Basins (Iberian Peninsula) by CMIP5 GCMs Local Downscaling

2021

The basins of the Júcar and Segura rivers, on the Mediterranean coast of the Iberian Peninsula, present a special water problem and are of particular interest regarding climate change. These basins are very vulnerable to a possible scenario of decreasing water resources. Recent studies on historic rainfall since 1955 have indicated an ongoing loss of precipitation in their headwaters, especially in the case of the Júcar river. The aim of the present study is to perform climate projections for the precipitation variable for several future periods (2021–2040, 2051–2070, 2081–2100) and emission scenarios (RCPs 4.5, 8.5) within the Júcar and Segura River Basin authorities. For this purpose, a s…

Mediterranean climateAtmospheric ScienceCMIP5 GCMs010504 meteorology & atmospheric sciencesTorrential rains0208 environmental biotechnologyDrainage basinClimate change02 engineering and technologyEnvironmental Science (miscellaneous)01 natural sciencesPeninsulaScenariosMeteorology. ClimatologyClimate changeDownscalingMeteorologiaPrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryscenariosdownscalingtorrential rainsEast of Iberian Peninsula020801 environmental engineeringWater resourceshydrological planningclimate changeAnálisis Geográfico RegionalHydrological planningEnvironmental scienceClimate modelPhysical geographyQC851-999Downscaling
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Climate change impact on the West African monsoon from June to October.

2015

Sixteen CMIP5 models are used toanalyse how climate changes over the West African Monsoon region between a “future period”, defined from 2031 to 2070under the rcp4.5 emission scenario, and the “current period”, defined from 1960 to 1999 under the historical emissionscenario. The results show an increase of the September to October rainfall amounts. Circulation anomalies include of anincreases of sea-level pressure over the Mediterranean Sea and Europe that allow a strengthening of the moisture flux fromEuro-Mediterranean regions into the Sahel. These changes are stronger in autumn.

CMIP5 modelschangement climatique[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyWest Africaseasonal cycleAfrique de l’OuestClimate change[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatologymodèles CMIP5cycle saisonnier
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Les changements futurs de la mousson africaine.

2013

7 pages; International audience; Nous analysons l’effet du changement climatique sur la mousson d’Afrique de l’ouest par l’utilisation de huitmodèles CMIP5 sous scénario RCP4.5, la réalisation d’un multi-modèle et l’approche « one model, one vote ». Les résultatsmontrent l’apparition d’un contraste pluviométrique zonal entre le centre et l’ouest du Sahel. Une mousson plus intensepermettrait une hausse de la convergence d’humidité et des précipitations au centre du Sahel. Un renforcement du jet d’estafricain et de la subsidence sur l’ouest du Sahel y permettrait en revanche une baisse de la pluviométrie.

changement climatique[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatologyrcp4.5SahelCMIP5[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology
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Last millennium northern hemisphere summer temperatures from tree rings: Part I: The long term context

2016

Текст статьи не публикуется в открытом доступе в соответствии с политикой журнала. Large-scale millennial length Northern Hemisphere (NH) temperature reconstructions have been progressively improved over the last 20 years as new datasets have been developed. This paper, and its companion (Part II, Anchukaitis et al. in prep), details the latest tree-ring (TR) based NH land air temperature reconstruction from a temporal and spatial perspective. This work is the first product of a consortium called N-TREND (Northern Hemisphere Tree-Ring Network Development) which brings together dendroclimatologists to identify a collective strategy for improving large-scale summer temperature reconstructions…

summer temperatures010506 paleontologyArcheologyGlobal and Planetary Changereconstruction010504 meteorology & atmospheric sciencesCalibration (statistics)34.03.02CMIP5 modelNorthern HemisphereGeologyContext (language use)01 natural sciencesWeightingTerm (time)Tree (data structure)last millenniumClimatologytree-ringsnorthern hemisphereScale (map)Ecology Evolution Behavior and SystematicsGeologyGlobal and Planetary Change0105 earth and related environmental sciences
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Tropical Temperate Toughs over southern Africa : mechanisms and evolution in response to climate change (2010-2099)

2014

In the Southern Hemisphere, Southern Africa and the south-west Indian Ocean are one of the three preferred regions where interactions between the tropics and midlatitudes develop. This is the South Indian Convergence Zone (SICZ), where northwest-southeast oriented cloud bands form at the synoptic scale (between 3 and 5 days). These bands are mainly found during the austral summer and are commonly referred to as tropical temperate troughs (TTTs). This research aims at improving our knowledge related to TTTs, with a study on the dynamics associated with these systems, and an analysis of their possible evolution during the 21st century.The first part of this thesis aims at identifying favorabl…

Changement climatiqueMidlatitude perturbationsTalweg tropical-tempéréAfrique australeGeneral circulation modelsRCP 8.5Perturbation des moyennes latitudesInteractions d’échelleClassificationModèles « système-Terre »[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyTropical-temperate toughClimate changeCMIP5Southern AfricaRCP2.6Scale interactions
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Tropical Temperate Toughs over southern Africa: mechanisms and evolution in response to climate change

2015

In the Southern Hemisphere, Southern Africa and the south-west Indian Ocean are one of the three preferred regions where interactions between the tropics and midlatitudes develop. This is the South Indian Convergence Zone (SICZ), where northwest-southeast oriented cloud bands form at the synoptic scale (between 3 and 5 days). These bands are mainly found during the austral summer and are commonly referred to as tropical temperate troughs (TTTs). This research aims at improving our knowledge related to TTTs, with a study on the dynamics associated with these systems, and an analysis of their possible evolution during the 21st century.The first part of this thesis aims at identifying favorab…

changement climatiqueperturbation des moyennes latitudesAfrique australe[SHS.GEO] Humanities and Social Sciences/Geographytropical-temperate toughgeneral circulation modelsRCP 8.5climate change[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatologyclassificationmodèles « système-Terre »talweg tropical-tempérémidlatitude perturbationsCMIP5.CMIP5scale interactionsSouthern Africainteractions d’échelleRCP2.6
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The climate change effect on the african monsoon region : evolution of the precipitation and atmospheric fields in the CMIP3 and CMIP5 simulations un…

2013

The fourth IPCC report in 2007 established the synthesis of previously published work onthe effects of climate change on global and regional scales. It shows in particular that no consensuscan be found with regard to the future of rainfall — and atmospheric dynamics- associatedwith region — African monsoon. This dissertation revisits this issue in the light of new dataand using an approach avoiding over-representation of the number of simulations available forone type of model and taking into account the diversity of models and their evolution in time :twenty general circulation models (GCMs) participating in the exercises CMIP3 (twelve GCMs)and CMIP5 (eight GCMs) under the A1B emissions sc…

Changement climatiqueA1B and rcp45 emission scenariosMousson africaineClimate ChangeSahel[SDU.STU] Sciences of the Universe [physics]/Earth SciencesAfrican MonsoonCMIP5[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesScénarios d’émission A1B et rcp45CMIP3General Circulation ModelsModèles de circulation générale
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