D. E. Harrison, Ph.D. (Harvard Univ.), Affiliate Professor.
harrison@pmel.noaa.gov. Ocean general circulation modeling and theory, and data analysis and modeling of tropical ocean-atmosphere interaction and climate variability. Oceanographer at Pacific Marine Environmental Laboratory/NOAA, and participant in the Global Climate Observing System, Global Ocean Observing System, Global Ocean Data Assimilation Experiment, other air-sea climate research programs, and Senior Fellow of the Joint Institute for Study of the Atmosphere and Ocean (JISAO). Affiliate Professor of Atmospheric Sciences.
Harrison, D.E. and S. Hankin (submitted) On the climatological seasonal cycle of central equatorial Pacific zonal currents: Some circulation model results and dynamical balances. Journal of Marine Research.
Bond, N.A. and D.E. Harrison (submitted) The Pacific Decadal Oscillation, air-sea interaction and central north Pacific winter atmospheric regimes. Geophysical Research Letters.
Larkin, N.K. and D.E. Harrison (submitted) The Cold Phase of ENSO: Near-global surface composites of ocean temperature, wind and pressure, 1946-1993. Journal of Climate.
Vecchi, G.A. and D.E. Harrison (submitted) Tropical Pacific sea surface temperature changes associated with westerly wind events. Journal of Climate.
Bennett, A.F., B.S. Chua, D.E. Harrison and M.J. McPhaden (submitted) Generalized inversion of Tropical Atmosphere-Ocean (TAO) data and a coupled model of the tropical Pacific. II. La Niña, error statistics and assessment. Journal of Climate.
Loukos, H., F. Vivier, P. Murphy and D.E. Harrison (submitted) Variability of the carbon dioxide evasion rates in the equatorial Pacific from 1982 to 1993 estimated from monthly temperature and salinity data. Geophysical Research Letters.
Harrison, D.E. and R. Weisberg (in press) Eastward surface jets in the central equatorial Pacific, November 1991-March 1992. Journal of Marine Research.
Harrison, D.E. and N.K. Larkin (1998) El Niño-Southern Oscillation sea surface temperature and wind anomalies, 1946–1993. Review of Geophysics 36: 353–399.
Harrison, D.E. and N.K. Larkin (1998) Seasonal U.S. temperature and precipitation anomalies associated with El Niño: Historical results and comparison with 1997–1998. Geophysical Research Letters 25: 3959–3962.
Bennett, A.F., B.S. Chua, D.E. Harrison and M.J. McPhaden (1998) Generalized inversion of Tropical Atmosphere-Ocean (TAO) data and a coupled model of the tropical Pacific. Journal of Climate 11: 1768–1792.
Craig, A.P., J.L. Bullister, D.E. Harrison, et al. (1998) A comparison of temperature, salinity, and chlorofluorocarbon observations with results from a 1° resolution three-dimensional global ocean model. Journal of Geophysical Research 103: 1099–1119.
Murphy, P.P., D.E. Harrison, R.A. Feely, T. Takahashi, R.F. Weiss and R.H. Gammon (1998) Variability of delta pCO2 in the subarctic North Pacific: A comparison of results from four expeditions. Tellus 50B: 185–204.
Stockdale, T.N, A.J. Busalacchi, D.E. Harrison and R. Seager (1998) Ocean modeling of ENSO. Journal of Geophysical Research 103: 14,325–14,355.
Hankin, S., J. Davison, J. Callahan, D.E. Harrison and K. O'Brien (1998) A configurable Web server for gridded data: A framework for collaboration. In 14th International Conference on Interactive Information and Processing Systems for Meteorology, Oceanography, and Hydrology: 417–418. AMS.
Harrison, D.E. and N.K. Larkin (1997) The Darwin Sea Level Pressure record, 1876-1996: Evidence for climate change? Geophysical Research Letters 24: 1779–1782.
Harrison, D.E. and G. Vecchi (1997) Westerly wind events in the tropical Pacific, 1986-1995. Journal of Climate 10: 3131–3156.
Murphy, P.P., D.E. Harrison, R.A. Feely, T. Takahashi, R.F. Weiss and R.H. Gammon (1997) Uncertainties in calculating regional fluxes for the subarctic North Pacific: Results from a study of pCO2 variability. In Tsunogai, S. (ed.) Biogeochemical Processes in the North Pacific: 80-86. Japan Marine Science Foundation.
Loukos, H., B.W. Frost, D.E. Harrison and J.W. Murray (1997) An ecosystem model with iron limitation of primary production in the equatorial Pacific at 140°W. Deep-Sea Research II 44: 2221–2250.