Shin, D. W., LaRow, T. E., Cocke, S., & O'Brien, J. J. (2005). The role of the CLM2 in the surface air temperature and precipitation of the FSU climate model. Research Activities in Atmospheric and Ocean Modeling, CAS/JSC Working Group on Numerical Experimentation.
|
Shin, D. W., Baigorria, G. A., Lim, Y. - K., Cocke, S., LaRow, T. E., O'Brien, J. J., et al. (2010). Assessing Maize and Peanut Yield Simulations with Various Seasonal Climate Data in the Southeastern United States. J. Appl. Meteor. Climatol., 49(4), 592–603.
|
Shin, D. W., Bellow, J. G., LaRow, T. E., Cocke, S., & O'Brien, J. J. (2006). The Role of an Advanced Land Model in Seasonal Dynamical Downscaling for Crop Model Application. J. Appl. Meteor. Climatol., 45(5), 686–701.
|
Shin, D. W., Cocke, S., & LaRow, T. E. (2007). Diurnal cycle of precipitation in a climate model. J. Geophys. Res., 112(D13).
|
Shin, D. W., Cocke, S., & Larow, T. E. (2003). Ensemble Configurations for Typhoon Precipitation Forecasts. Journal of the Meteorological Society of Japan, 81(4), 679–696.
|
Shin, D. W., Cocke, S., LaRow, T. E., & O'Brien, J. J. (2005). Seasonal Surface Air Temperature and Precipitation in the FSU Climate Model Coupled to the CLM2. J. Climate, 18(16), 3217–3228.
|
Shin, D. W., LaRow, T. E., & Cocke, S. (2003). Convective scheme and resolution impacts on seasonal precipitation forecasts. Geophys. Res. Lett., 30(20).
|
Strazzo, S., Elsner, J. B., LaRow, T., Halperin, D. J., & Zhao, M. (2013). Observed versus GCM-Generated Local Tropical Cyclone Frequency: Comparisons Using a Spatial Lattice. J. Climate, 26(21), 8257–8268.
|
Strazzo, S. E., Elsner, J. B., & LaRow, T. E. (2015). Quantifying the sensitivity of maximum, limiting, and potential tropical cyclone intensity to SST: Observations versus the FSU/COAPS global climate model. J. Adv. Model. Earth Syst., 7(2), 586–599.
|
Strazzo, S. E., Elsner, J. B., LaRow, T. E., Murakami, H., Wehner, M., & Zhao, M. (2016). The influence of model resolution on the simulated sensitivity of North Atlantic tropical cyclone maximum intensity to sea surface temperature. J. Adv. Model. Earth Syst., 8(3), 1037–1054.
|