Global and regional surface wind datasets from spaceborne scatterometers are ”massive” and important for climate and weather. Applications require:
regular grids
uniform spatial O(10 km) and temporal O(diurnal) resolution
Blended scatterometer and weather-center analyses provide global, realistic high-wavenumber surface winds
impose spectral constraints via multi-resolution wavelets
Bayesian Hierarchical Models to exploit massive remote sensing datasets
measurement error models from cal/val studies (likelihoods)
process models from GFD (priors)
advances in MCMC
Tropical Winds Example (Wikle et al. 2001)
Bayesian Hierarchical Model for Air-Sea Interaction (Berliner et al 2002)
multi-platform data from scatterometer and altimeter
stochastic geostrophy (atmos) and quasi-geostrophy (ocean) priors
MCMC to ISMC linkage for posteriors
term-by-term uncertainty
realistic covariance structures
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