Downscaling rainfields in space and time, using the String of Beads model in time series mode

Citation
Ggs. Pegram et An. Clothier, Downscaling rainfields in space and time, using the String of Beads model in time series mode, HYDROL E S, 5(2), 2001, pp. 175-186
Citations number
17
Categorie Soggetti
Earth Sciences
Journal title
HYDROLOGY AND EARTH SYSTEM SCIENCES
ISSN journal
10275606 → ACNP
Volume
5
Issue
2
Year of publication
2001
Pages
175 - 186
Database
ISI
SICI code
1027-5606(200106)5:2<175:DRISAT>2.0.ZU;2-3
Abstract
The String of Beads model is a space-time model of rain fields measured by weather radar. It is here driven by two auto-regressive time series models. one at the image scale, the other at the pixel scale. to model the tempora l correlation structure of the wet-period process. The marginal distributio n of the pixel scale intensities on a given radar-rainfall image is describ ed by a log-normal distribution. The spatial dependence structure of each i mage is defined by a power spectrum approximated by a power law function wi th a negative exponent, It is demonstrated that this stochastic modelling a pproach is valid because the images sampled are effectively stationary abov e a scale of 30 km, which is less than a quarter of the image width. By adv ecting a simulated sequence of images along the same cumulative advection v ector as the observed event and matching the image-scale statistics of each simulated image with those of the corresponding observed image, a simulate d sequence of plausible images is generated which mimics (has the same spac e-time statistics as) the observed event but differs from it in detail. Agg regating the pixel scale intensities in each sequence over a number of time and space intervals and then comparing their spatial and temporal statisti cs, demonstrates that the model captures the intermediate scale behaviour w ell, showing satisfactorily its ability to downscale rainfall in space and time. The model thus has potential as an operational space-time model of ra infields.