Title: Providing distributed forecasts of precipitation using a Bayesian nowcast scheme
1Providing distributed forecasts of precipitation
using a Bayesian nowcast scheme
- Neil I. Fox Chris K. Wikle
- University of Missouri - Columbia
2Contents
- Reasoning
- Method / model
- Statistical method
- Dynamics
- More reasoning
- Products
- Case study example
- Development
3Reasoning
- Need realistic representation of uncertainty in
precipitation forecasts - Previous methods too deterministic (no measure of
uncertainty) or too probabilistic (stochastic) - This methodology allows for the integration of
some real physics with a realistic statistical
formulation that can provide genuine information
on forecast uncertainty
4Hierarchical Model
- 5 stage model
- Data
- Process
- Spatial distributions
- Parameters
5Spatio-Temporal Dynamic Models
Hierarchical Space-Time Framework
6Used in
- Ecology e.g. Model species dispersion
- Data sparse obs e.g. Scatterometer winds
- Long-term modeling e.g. SST prediction
7Model formulation
- Stage 3 The integro-difference equation (IDE)
ks(r?s) is a redistribution kernel that
describes how the process Y at time t is
redistributed spatially at time t1.
8IDE Kernel Parameterization
For 2-D space, consider the multivariate Gaussian
kernel for location s
The kernel is centered at s µ(?s) and thus the
µ parameters control the translation and the
covariance parameters control the dilation and
orientation. These parameters can be given
spatial distributions at the next level of the
hierarchy!! Alternative kernel parameterization
ellipse foci, e.g., Higdon et al. 1999
9Spatial distribution
- Model the ?s parameters with a spatial
distribution at the next level of the hierarchy - Gaussian random field
- Diffusive wave fronts shape and speed of
diffusion depend on kernel width and tail
behavior (dilation) (e.g., Kot et al. 1996) - Non-diffusive propagation via relative
displacement of kernel (translation) e.g., Wikle
(2001 2002)
10Model implementation MCMC
- Markov Chain Monte-Carlo
- Gibbs sampler
11Things this can do
- Full spatial variance field
- Where do we have least confidence in the forecast
- Quantitative uncertainty for defined points and
areas (i.e. catchment QPF uncertainty)
12More things we can do
- Incorporation of physics
- ? can become a spatially varying growth parameter
- Kernel can incorporate windfield information
13Products - domain
- Nowcast fields
- Mean nowcast
- to T60 (10 minute intervals at present)
- Variance fields
- Uncertainty
14Mean nowcast fields
15Indication of uncertainty in space
16Products - point / catchment
- Nowcast reflectivity
- 10 minute intervals to T60
- With variance
- Nowcast Rainfall
- Point or group of points
- Mean or median nowcast rainfall or accumulation
out to T60 - Cumulative frequency / probability distributions
17(No Transcript)
18Rainrate distribution
19Cumulative frequency of nowcast rainrate
Pixel 1
Pixel 2
Pixel 3
3 pixel aggreg
20Cumulative frequency of nowcast rain accumulations
Pixel 1
Pixel 2
Pixel 3
3 pixel aggreg
21In the future
- Verification and adjustment
- Incorporation of physics
- Computational efficiency
- Hydrology
- lumped model probabilities
- distributed probabilistic input
22References
- Wikle, C.K., Berliner, L.M., and Cressie, N.
(1998). Hierarchical Bayesian space-time models.
Environmental and Ecological Statistics, 5,
117-154. - Wikle, C.K., Milliff, R.F., Nychka, D., and L.M.
Berliner, 2001 Spatiotemporal hierarchical
Bayesian modeling Tropical ocean surface winds,
Journal of the American Statistical Association,
96, 382-397. - Berliner, L.M., Wikle, C.K., and Cressie, N.,
2000 Long-lead prediction of Pacific SSTs via
Bayesian dynamic modeling. Journal of Climate,
13, 3953-3968. - Xu, B., Wikle, C.K., and N.I. Fox, 2003 A
kernel-based spatio-temporal dynamical model for
nowcasting radar precipitation. Journal of the
American Statistical Association. In review.
Available at http//solberg.snr.missouri.edu/Peop
le/fox/research/xuetal2003.pdf