P2.1
Variability of monthly FSU wind stress and heat fluxes over the Atlantic Ocean
The FSU3 gridded fields are objectively produced from in situ ship and buoy (moored and drifting) observations through a variational method. In addition to the variational method, the fields also benefit from the inclusion of a surface flux model (adopted from Bourassa et al. 2005) that is used to determine the transfer coefficients needed for the bulk flux calculations. Fields prior to and including 1997 are generated using the International Comprehensive Ocean-Atmosphere Data Set (ICOADS; Woodruff et al. 1987), while data from the National Climatic Data Center (technical document Marine Surface Observations TD-1129; NCDC 2003) is used for the subsequent years. Three constraints are applied to the vector variables: a misfit to observations, a Laplacian smoothing term, and a misfit of the curl. The first two constraints are applied to scalar variables. Each constraint is multiplied by a weight that is determined using cross validation (Pegion et al. 2000) prior to the minimization of the functional. The weights, dependant on observing platform, take into consideration both the observational uncertainty and data coverage.