Glacial fluctuations of the Indian monsoon and their relationship with North Atlantic climate: new data and modelling experiments
Texte intégral
Figure
Documents relatifs
Recent works suggest that mid-latitude coupled variability during late boreal winter may play a significant role in the onset and development of ENSO events: in the North
In the Picot valley, glacier advances during the Late Glacial were the largest, while large moraines formed during the Holocene, in particular during the LIA, are missing, if
Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation
121 Based on these facts, we revisit the Nice shallow submarine 122 slope area and investigate the seismic slope stability with cyclic 123 triaxial tests with loading patterns
en compte des atomes de bords permet d’exprimer l’anisotropie par atome pour des ilots en fonction de leur taille. nombre d’atomes du centre à un sommet, tous les deux inclus)
Finally, texture-induced mechanical anisotropy of the lithospheric mantle effectively converts poloidal flow (convergent or divergent plate motions) into toroidal
Extended winter Pacific North America oscillation as a precursor of the Indian summer monsoon rainfall.. Peings, Hervé Douville,
The impact of diurnal SST coupling and vertical oceanic resolution on the simulation of the Indian 24.. Summer Monsoon (ISM) and its relationships with El