GC104-0012
Process oriented diagnostics of monsoon sub-seasonal variability in NCUM global and regional models
Abstract:
The results obtained here are consistent with our understanding that moisture advection acts a leading term in inducing the break conditions over central Indian and adjoining oceanic regions. Specifically, dry air advection from the northwest regions strongly dries the atmospheric column nearly 7-10 days before and the peak dry phase over Indian subcontinent. Movement of this dryness, with time, towards central India and Arabian Sea is consistent with anomalous total precipitable water content seen from satellite observations. Preliminary results are encouraging and one of the direct implications of this work is that the lead times obtained in the moisture budget assessment can be used for understanding and improvement of the model forecasts.