Andere Kunden interessierten sich auch für
![Numerical Study on the Southeast Asian summer monsoon]( "Numerical Study on the Southeast Asian summer monsoon")
Numerical Study on the Southeast Asian summer monsoon32,99 €![LOW LEVEL JETSTREAM OF ASIAN SUMMER MONSOON AND ITS VARIABILITY]( "LOW LEVEL JETSTREAM OF ASIAN SUMMER MONSOON AND ITS VARIABILITY")
LOW LEVEL JETSTREAM OF ASIAN SUMMER MONSOON AND ITS VARIABILITY38,99 €![Satellite data impact on monsoon depression]( "Satellite data impact on monsoon depression")
Satellite data impact on monsoon depression38,99 €![Simulation of Indian summer monsoon processes using numerical models]( "Simulation of Indian summer monsoon processes using numerical models")
Simulation of Indian summer monsoon processes using numerical models53,99 €![Chasing the Indian Summer Monsoon at its Gateway]( "Chasing the Indian Summer Monsoon at its Gateway")
Chasing the Indian Summer Monsoon at its Gateway46,99 €![On the Relative Impacts of ENSO and IODZM on Southern African Rainfall]( "On the Relative Impacts of ENSO and IODZM on Southern African Rainfall")
On the Relative Impacts of ENSO and IODZM on Southern African Rainfall32,99 €![Indian Summer Monsoon Circulation in the Warming Atmosphere]( "Indian Summer Monsoon Circulation in the Warming Atmosphere")
Indian Summer Monsoon Circulation in the Warming Atmosphere24,99 €
Two of the factors which influence the summer monsoon rainfall variability over the East Asian Domain are the El Nino and Southern Oscillation (ENSO) phenomenon and the recently identified Indian Ocean Dipole Mode (IODM). In this study impact of IODM and ENSO on the East Asian monsoon variability has been studied using observational data and modeling studies. Results reveal that the dipole mode influences the summer monsoon activity over East Asia, in particular the Korea-Japan sector three seasons later and ENSO affects monsoon variability over China simultaneously. This study has also identified one possible mechanism of the delayed impact of the dipole mode over the Indian Ocean on the summer monsoon variability over East Asia. General Circulation Model was used to investigate this mechanism. The delayed impact three seasons later is carried by the snow distribution over Eurasia. The snow distribution over Eurasia serves as a bridge connecting Indian Ocean and East Asian monsoon variability.