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Seitz, C. (2014). Estimating the Effects of Climate Change on Tropical Cyclone Activity. Master's thesis, Florida State University, Tallahassee, FL.
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Selman, C. (2012). Understanding the 21st Century Projection of the Wet Season over the Southeastern United States. Master's thesis, Florida State University, Tallahassee, FL.
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Selman, C. M. (2015). Simulating the Impacts and Sensitivity of the Southeastern United States Climatology to Irrigation. Ph.D. thesis, Florida State University, Tallahassee, FL.
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Selman, C., & Misra, V. (2017). The impact of an extreme case of irrigation on the southeastern United States climate. Clim Dyn, 48(3-4), 1309–1327.
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Selman, C., & Misra, V. (2016). The sensitivity of southeastern United States climate to varying irrigation vigor. J. Geophys. Res. Atmos., 121(13), 7606–7621.
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Selman, C., & Misra, V. (2015). Simulating diurnal variations over the southeastern United States. J. Geophys. Res. Atmos., 120(1), 180–198.
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Selman, C., Misra, V., Stefanova, L., Dinapoli, S., & Smith III, T. J. (2013). On the twenty-first-century wet season projections over the Southeastern United States. Reg Environ Change, 13(S1), 153–164.
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Selph, K. E., Landry, M. R., Taylor, A. G., Gutierrez-Rodriguez, A., Stukel, M. R., Wokuluk, J., et al. (2016). Phytoplankton production and taxon-specific growth rates in the Costa Rica Dome. J Plankton Res, 38(2), 199–215.
Abstract: During summer 2010, we investigated phytoplankton production and growth rates at 19 stations in the eastern tropical Pacific, where winds and strong opposing currents generate the Costa Rica Dome (CRD), an open-ocean upwelling feature. Primary production (14C-incorporation) and group-specific growth and net growth rates (two-treatment seawater dilution method) were estimated from samples incubated in situ at eight depths. Our cruise coincided with a mild El Nino event, and only weak upwelling was observed in the CRD. Nevertheless, the highest phytoplankton abundances were found near the dome center. However, mixed-layer growth rates were lowest in the dome center ( approximately 0.5-0.9 day-1), but higher on the edge of the dome ( approximately 0.9-1.0 day-1) and in adjacent coastal waters (0.9-1.3 day-1). We found good agreement between independent methods to estimate growth rates. Mixed-layer growth rates of Prochlorococcus and Synechococcus were largely balanced by mortality, whereas eukaryotic phytoplankton showed positive net growth ( approximately 0.5-0.6 day-1), that is, growth available to support larger (mesozooplankton) consumer biomass. These are the first group-specific phytoplankton rate estimates in this region, and they demonstrate that integrated primary production is high, exceeding 1 g C m-2 day-1 on average, even during a period of reduced upwelling.
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