Misra, V., & Chan, S. (2009). Seasonal predictability of the Atlantic Warm Pool in the NCEP CFS.
Geophys. Res. Lett., 36(16).
Misra, V. (2010). Interaction of interannual and diurnal variations over equatorial Africa.
J. Geophys. Res., 115(D1).
Chan, S. C., Misra, V., & Smith, H. (2011). A modeling study of the interaction between the Atlantic Warm Pool, the tropical Atlantic easterlies, and the Lesser Antilles: ATLANTIC WARM POOL, EASTERLIES, ISLANDS INTERACTIONS.
J. Geophys. Res., 116(D21).
Misra, V., Moeller, L., Stefanova, L., Chan, S., O'Brien, J. J., Smith III, T. J., et al. (2011). The influence of the Atlantic Warm Pool on the Florida panhandle sea breeze: FLORIDA SEA BREEZE VARIATIONS.
J. Geophys. Res., 116(D21).
DiNapoli, S. M., & Misra, V. (2012). Reconstructing the 20th century high-resolution climate of the southeastern United States.
J. Geophys. Res., 117(D19), n/a-n/a.
Misra, V., Bhardwaj, A., & Noska, R. (2017). Understanding the Variations of the Length and the Seasonal Rainfall Anomalies of the Indian Summer Monsoon.
J. Climate, 30(5), 1753–1763.
Misra, V., Mishra, A., & Bhardwaj, A. (2018). Simulation of the Intraseasonal Variations of the Indian Summer Monsoon in a Regional Coupled Ocean-Atmosphere Model.
J. Climate, 31(8), 3167–3185.
Kozar, M. E., Misra, V., & Powell, M. D. (2016). Hindcasts of Integrated Kinetic Energy in Atlantic Tropical Cyclones: A Neural Network Prediction Scheme.
Mon. Wea. Rev., 144(12), 4591–4603.
Misra, V., & Bhardwaj, A. (2019). Defining the Northeast Monsoon of India.
Mon. Wea. Rev., 147(3), 791–807.
Abstract: This study introduces an objective definition for onset and demise of the Northeast Indian Monsoon (NEM). The definition is based on the land surface temperature analysis over the Indian subcontinent. It is diagnosed from the inflection points in the daily anomaly cumulative curve of the area-averaged surface temperature over the provinces of Andhra Pradesh, Rayalseema, and Tamil Nadu located in the southeastern part of India. Per this definition, the climatological onset and demise dates of the NEM season are 6 November and 13 March, respectively. The composite evolution of the seasonal cycle of 850hPa winds, surface wind stress, surface ocean currents, and upper ocean heat content suggest a seasonal shift around the time of the diagnosed onset and demise dates of the NEM season. The interannual variations indicate onset date variations have a larger impact than demise date variations on the seasonal length, seasonal anomalies of rainfall, and surface temperature of the NEM. Furthermore, it is shown that warm El Niño�Southern Oscillation (ENSO) episodes are associated with excess seasonal rainfall, warm seasonal land surface temperature anomalies, and reduced lengths of the NEM season. Likewise, cold ENSO episodes are likely to be related to seasonal deficit rainfall anomalies, cold land surface temperature anomalies, and increased lengths of the NEM season.
Misra, V. (2008). Coupled Air, Sea, and Land Interactions of the South American Monsoon.
J. Climate, 21(23), 6389–6403.