COAPS Virtual Library (Publications)

Meyers, S. D., Melsom, A., Mitchum, G. T., & O'Brien, J. J. (1998). Detection of the fast Kelvin wave teleconnection due to El Niño-Southern Oscillation. J. Geophys. Res., 103(C12), 27655–27663. https://www.coaps.fsu.edu/bibliography/show.php?record=534
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. https://www.coaps.fsu.edu/bibliography/show.php?record=525
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. Keywords: Asia; Indian Ocean; Mixed layer; Monsoons; Atmosphere-ocean interaction; Regional models https://www.coaps.fsu.edu/bibliography/show.php?record=557
Misra, V., Bhardwaj, A., & Mishra, A. (2018). Characterizing the rainy season of Peninsular Florida. Climate Dynamics, 51(5-6), 2157–2167. Abstract: Peninsular Florida (PF) has a very distinct wet season that can be objectively defined with onset and demise dates based on daily rainfall. The dramatic onset of rains and its retreat coincides with the seasonal cycle of the regional scale atmospheric and upper ocean circulations and upper ocean heat content of the immediate surrounding ocean. The gradual warming of the Intra-Americas Seas (IAS; includes Gulf of Mexico, Caribbean Sea and parts of northwestern subtropical Atlantic Ocean) with the seasonal evolution of the Loop Current and increased atmospheric heat flux in to the ocean eventually enhance the moisture flux into terrestrial PF around the time of the onset of the Rainy Season of PF (RSPF). Similarly, the RSPF retreats with the cooling of the IAS that coincides with the weakening of the Loop Current and reduction of the upper ocean heat content of the IAS. It is also shown that anomalous onset and demise dates of the RSPF have implications on its seasonal rainfall anomalies. https://www.coaps.fsu.edu/bibliography/show.php?record=556
Mizoguchi, K., Meyers, S. D., Basu, S., & O'Brien, J. J. (1998). CEOF analysis of 1947-1992 SST in the North Atlantic. In 9th Conference on Interaction of the Sea and Atmosphere at the 78th American-Meteorogical-Society Annual Meeting (pp. 62–64). https://www.coaps.fsu.edu/bibliography/show.php?record=541
Mizoguchi, K. -ichi, Meyers, S. D., Basu, S., & O'Brien, J. J. (1999). Multi- and Quasi-Decadal Variations of Sea Surface Temperature in the North Atlantic. J. Phys. Oceanogr., 29(12), 3133–3144. https://www.coaps.fsu.edu/bibliography/show.php?record=524
Morey, S. L. (2002). The spring transition from horizontal to vertical thermal stratification on a midlatitude continental shelf. J. Geophys. Res., 107(C8). Keywords: continental shelf; stratification; Mixed Layer Dynamics; Coastal Ocean Modeling; West Florida Shelf https://www.coaps.fsu.edu/bibliography/show.php?record=493
Morey, S. L. (2003). Export pathways for river discharged fresh water in the northern Gulf of Mexico. J. Geophys. Res., 108(C10). Keywords: cross-shelf transport; fresh water; Gulf of Mexico https://www.coaps.fsu.edu/bibliography/show.php?record=471
Morey, S. L., Schroeder, W. W., O'Brien, J. J., & Zavala-Hidalgo, J. (2003). The annual cycle of riverine influence in the eastern Gulf of Mexico basin. Geophys. Res. Lett., 30(16). https://www.coaps.fsu.edu/bibliography/show.php?record=474
Morey, S. L., Zavala-Hidalgo, J., & O'Brien, J. J. (2003). Impacts of vertical resolution on a numerical model of the Gulf of Mexico. In OCEANS 2003 MTS/IEEE: Celebrating the Past... Teaming toward the Future (pp. 435–438). https://www.coaps.fsu.edu/bibliography/show.php?record=486

Abstract: Peninsular Florida (PF) has a very distinct wet season that can be objectively defined with onset and demise dates based on daily rainfall. The dramatic onset of rains and its retreat coincides with the seasonal cycle of the regional scale atmospheric and upper ocean circulations and upper ocean heat content of the immediate surrounding ocean. The gradual warming of the Intra-Americas Seas (IAS; includes Gulf of Mexico, Caribbean Sea and parts of northwestern subtropical Atlantic Ocean) with the seasonal evolution of the Loop Current and increased atmospheric heat flux in to the ocean eventually enhance the moisture flux into terrestrial PF around the time of the onset of the Rainy Season of PF (RSPF). Similarly, the RSPF retreats with the cooling of the IAS that coincides with the weakening of the Loop Current and reduction of the upper ocean heat content of the IAS. It is also shown that anomalous onset and demise dates of the RSPF have implications on its seasonal rainfall anomalies.

https://www.coaps.fsu.edu/bibliography/show.php?record=556

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