Kozar, M. E., & Misra, V. (2014). Statistical Prediction of Integrated Kinetic Energy in North Atlantic Tropical Cyclones.
Mon. Wea. Rev., 142(12), 4646–4657.
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.
Krishnamurti, T. N., Rajendran, K., Vijaya Kumar, T. S. V., Lord, S., Toth, Z., Zou, X., et al. (2003). Improved Skill for the Anomaly Correlation of Geopotential Heights at 500 hPa.
Mon. Wea. Rev., 131(6), 1082–1102.
Krishnamurti, T. N., Surendran, S., Shin, D. W., Correa-Torres, R. J., Vijaya Kumar, T. S. V., Williford, E., et al. (2001). Real-Time Multianalysis-Multimodel Superensemble Forecasts of Precipitation Using TRMM and SSM/I Products.
Mon. Wea. Rev., 129(12), 2861–2883.
LaRow, T. E. (2013). The Impact of SST Bias Correction on North Atlantic Hurricane Retrospective Forecasts.
Mon. Wea. Rev., 141(2), 490–498.
Liu, J., Curry, J. A., Clayson, C. A., & Bourassa, M. A. (2011). High-Resolution Satellite Surface Latent Heat Fluxes in North Atlantic Hurricanes.
Mon. Wea. Rev., 139(9), 2735–2747.
Meyers, S. D., O'Brien, J. J., & Thelin, E. (1999). Reconstruction of Monthly SST in the Tropical Pacific Ocean during 1868-1993Using Adaptive Climate Basis Functions.
Mon. Wea. Rev., 127(7), 1599–1612.
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., DiNapoli, S., & Powell, M. (2013). The Track Integrated Kinetic Energy of Atlantic Tropical Cyclones.
Mon. Wea. Rev., 141(7), 2383–2389.
Nielsen, E. R., Schumacher, R. S., & Keclik, A. M. (2016). The Effect of the Balcones Escarpment on Three Cases of Extreme Precipitation in Central Texas.
Mon. Wea. Rev., 144(1), 119–138.