The origin of summer monsoon rainfall at New Delhi by deuterium excess

Figure 9 shows spatial distributions of monthly mean dust- induced change of precipitation from the WRF-Chem sim- ulations in June, July, and August averaged for 1995–2009 over the

As mulheres também têm muita diversão na praia, como buscar o filho afogado e caminhar vinte quilômetros pra encontrar o outro pé do chinelo.. Já os homens ficam com as tarefas

The annual rainfall anomaly is an east-west dipole over tropical South America, with drought to the west over the Amazon basin whose discharge is documented at Manaus, and with

On average, the summer QTDW is amplified after a maximum of zonal wind shear which is connected with the summer mesospheric jet and there is a possible correlation of the summer

For example, with ERAI, 149 events are detected with the relative vorticity at 850 hPa (RV850), 117 with the mean sea-level pressure anomaly (MSLP ANOM) and 91 with the 10 m wind

At annual scale, sea level anomalies (SLAs) are generated by the Asian monsoon; interannual sea level variability is determined by the El Niño–Southern Oscillation (ENSO) and the

While the changes of summer monsoon over South Asia and south- ern China are mainly controlled by global climate conditions (e.g. warmer sea surface temperature), the summer

This summer rainfall deficit over India during the summer monsoon is the largest impact of the vegetation changes to land precipitation, and the weakening of the Tropical Easterly