Dukhovskoy, D. S., Ubnoske, J., Blanchard-Wrigglesworth, E., Hiester, H. R., & Proshutinsky, A. (2015). Skill metrics for evaluation and comparison of sea ice models.
J. Geophys. Res. Oceans, 120(9), 5910–5931.
Farneti, R., Downes, S. M., Griffies, S. M., Marsland, S. J., Behrens, E., Bentsen, M., et al. (2015). An assessment of Antarctic Circumpolar Current and Southern Ocean meridional overturning circulation during 1958-2007 in a suite of interannual CORE-II simulations.
Ocean Modelling, 93, 84–120.
Jones, C. S., Cenedese, C., Chassignet, E. P., Linden, P. F., & Sutherland, B. R. (2015). Gravity current propagation up a valley.
J. Fluid Mech., 762, 417–434.
Liu, B., Zhou, T., & Lu, J. (2015). Quantifying contributions of model processes to the surface temperature bias in FGOALS-g2.
J. Adv. Model. Earth Syst., 7(4), 1519–1533.
Nguyen, T. - T., Morey, S. L., Dukhovskoy, D. S., & Chassignet, E. P. (2015). Nonlocal impacts of the Loop Current on cross-slope near-bottom flow in the northeastern Gulf of Mexico.
Geophys. Res. Lett., 42(8), 2926–2933.
Paget, A. C., Bourassa, M. A., & Anguelova, M. D. (2015). Comparing in situ and satellite-based parameterizations of oceanic whitecaps.
J. Geophys. Res. Oceans, 120(4), 2826–2843.
Proshutinsky, A., Dukhovskoy, D., Timmermans, M. - L., Krishfield, R., & Bamber, J. L. (2015). Arctic circulation regimes.
Philos Trans A Math Phys Eng Sci, 373(2052).
Abstract: Between 1948 and 1996, mean annual environmental parameters in the Arctic experienced a well-pronounced decadal variability with two basic circulation patterns: cyclonic and anticyclonic alternating at 5 to 7 year intervals. During cyclonic regimes, low sea-level atmospheric pressure (SLP) dominated over the Arctic Ocean driving sea ice and the upper ocean counterclockwise; the Arctic atmosphere was relatively warm and humid, and freshwater flux from the Arctic Ocean towards the subarctic seas was intensified. By contrast, during anticylonic circulation regimes, high SLP dominated driving sea ice and the upper ocean clockwise. Meanwhile, the atmosphere was cold and dry and the freshwater flux from the Arctic to the subarctic seas was reduced. Since 1997, however, the Arctic system has been under the influence of an anticyclonic circulation regime (17 years) with a set of environmental parameters that are atypical for this regime. We discuss a hypothesis explaining the causes and mechanisms regulating the intensity and duration of Arctic circulation regimes, and speculate how changes in freshwater fluxes from the Arctic Ocean and Greenland impact environmental conditions and interrupt their decadal variability.
Selman, C., & Misra, V. (2015). Simulating diurnal variations over the southeastern United States.
J. Geophys. Res. Atmos., 120(1), 180–198.
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.
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.