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).
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.
Karmakar, N., & Misra, V. (2019). The Relation of Intraseasonal Variations With Local Onset and Demise of the Indian Summer Monsoon.
J. Geophys. Res. Atmos., 124(5), 2483–2506.
Abstract: Two of the most important hydroclimatic features of the Indian Summer Monsoon (ISM) rainfall are its onset/demise and Intraseasonal Oscillations (ISOs) manifested by the active‐break cycles. In this study, we aim to understand the quantitative association between these two phenomena. An objective definition of local onset/demise of the ISM based on more than a century‐long India Meteorological Department (IMD) rain‐gauge observation is taken into consideration. Using multichannel singular spectrum analysis (MSSA) we isolate northward propagating low‐ (20–60 days; LF‐ISO) and northwestward propagating high‐ (10–20 days; HF‐ISO) frequency ISOs from the daily ISM rainfall. Our results suggest that a large number of local onset (59%) and demise (62%) events occur during positive developing phases and positive decaying phases of two ISOs, respectively, with phase‐locking between LF‐ISO and HF‐ISO being particularly important. Local onset is largely associated with favorable phases of ISOs across India except for LF‐ISO over eastern India and HF‐ISO over western Ghats and central India (CI). We find that local demise is more coherent with the ISO phases, especially with HF‐ISO across the domain. We performed a case study to understand large‐scale association with the onset of the ISM over CI. In 44 of total 58 cases (1948–2005), when CI onset occurred during favorable LF‐ISO or HF‐ISO phase, they are either linked with a northward propagation of convection from the equator in LF‐ISO timescale (28 cases) or westward propagating structures from the western Pacific in HF‐ISO timescale (27 cases).
Kozar, M. E., Mann, M. E., Camargo, S. J., Kossin, J. P., & Evans, J. L. (2012). Stratified statistical models of North Atlantic basin-wide and regional tropical cyclone counts.
J. Geophys. Res., 117(D18).
Kozar, M. E., Mann, M. E., Emanuel, K. A., & Evans, J. L. (2013). Long-term variations of North Atlantic tropical cyclone activity downscaled from a coupled model simulation of the last millennium.
J. Geophys. Res. Atmos., 118(24), 13,383–13,392.
Li, H., Kanamitsu, M., & Hong, S. - Y. (2012). California reanalysis downscaling at 10 km using an ocean-atmosphere coupled regional model system.
J. Geophys. Res., 117(D12).
Misra, V., & Mishra, A. (2016). The oceanic influence on the rainy season of Peninsular Florida.
J. Geophys. Res. Atmos., 121(13), 7691–7709.
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).
Selman, C., & Misra, V. (2015). Simulating diurnal variations over the southeastern United States.
J. Geophys. Res. Atmos., 120(1), 180–198.
Selman, C., & Misra, V. (2016). The sensitivity of southeastern United States climate to varying irrigation vigor.
J. Geophys. Res. Atmos., 121(13), 7606–7621.