Intraseasonal Variability of the Indian Monsoon as Simulated by a Global Model

• Published in: Pure and applied geophysics Vol. 175; no. 6; pp. 2323 - 2340
• Main Authors: Joshi, Sneh, Kar, S. C.
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.06.2018; Springer Nature B.V
• Subjects: Annual variations; Anomalies; Climatology; Computer simulation; Convection; Convection modes; Earth and Environmental Science; Earth Sciences; Equatorial regions; Equatorial waves; Geophysics/Geodesy; Humidity; Life cycle; Life cycle engineering; Life cycles; Monsoons; Ocean currents; Propagation; Rain; Rainfall; Rainfall anomalies; Sea surface temperature; Specific humidity; Spectral analysis; Surface temperature; Temperature (air-sea); Variability; Wind; India; initial conditions; rainfall; Monsoon; intraseasonal; simulations; equatorial waves
• ISSN: 0033-4553; 1420-9136
• DOI: 10.1007/s00024-018-1786-0

This study uses the global forecast system (GFS) model at T126 horizontal resolution to carry out seasonal simulations with prescribed sea-surface temperatures. Main objectives of the study are to evaluate the simulated Indian monsoon variability in intraseasonal timescales. The GFS model has been integrated for 29 monsoon seasons with 15 member ensembles forced with observed sea-surface temperatures (SSTs) and additional 16-member ensemble runs have been carried out using climatological SSTs. Northward propagation of intraseasonal rainfall anomalies over the Indian region from the model simulations has been examined. It is found that the model is unable to simulate the observed moisture pattern when the active zone of convection is over central India. However, the model simulates the observed pattern of specific humidity during the life cycle of northward propagation on day − 10 and day + 10 of maximum convection over central India. The space–time spectral analysis of the simulated equatorial waves shows that the ensemble members have varying amount of power in each band of wavenumbers and frequencies. However, variations among ensemble members are more in the antisymmetric component of westward moving waves and maximum difference in power is seen in the 8–20 day mode among ensemble members.