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Statistics Seminar - University of EdinburghStatistics Seminar
School of Mathematics The University of Edinburgh Friday 10 October 2008 3.00 p.m. Room 5327, James Clerk Maxwell Building Chris Glasbey (Biomathematics and Statistics Scotland) Spatio-temporal weather models (joint with Dave Allcroft) We develop contrasting spatio-temporal models for two weather variables: solar radiation and rainfall. For solar radiation the aim is to assess the performance of area networks of photo-voltaic cells. Although radiation measured at a sufficiently fine temporal scale has a bimodal marginal distribution (Glasbey, 2001), averages of 10-minute or longer duration can be transformed to be approximately Gaussian, and we fit a spatio-temporal auto-regressive moving average (STARMA) process (Glasbey and Allcroft, 2008). For rainfall, the aim is to disaggregate to a finer spatial scale than that observed. To overcome the difficulty that the marginal distribution of hourly rainfall has a singularity at zero and so is highly non-Gaussian, we apply a monotonic transformation. This defines a latent Gaussian variable, with zero rainfall corresponding to censored values below a threshold, which we model using a spatio-temporal Gaussian Markov random field (Allcroft and Glasbey, 2003). For both models, computations are simplified by approximating space by a torus and using Fourier transforms. Allcroft, D.J. and Glasbey, C.A. (2003). A latent Gaussian Markov random field model for spatio-temporal rainfall disaggregation. Applied Statistics, 52, 487-498. Glasbey CA (2001). Nonlinear autoregressive time series with multivariate Gaussian mixtures as marginal distributions. Applied Statistics, 50, 143-154. Glasbey, C.A. and Allcroft, D.J. (2008). A STARMA model for solar radiation. Applied Statistics, 57, 343-355. Tea and coffee will be available after the seminar in the Mathematics Common Room (5212). Natalia Bochkina N.Bochkina@... -- The University of Edinburgh is a charitable body, registered in Scotland, with registration number SC005336. |
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Weather models RE: Statistics Seminar - University of EdinburghSorry I'm unable to get to Edinburgh for this(but must find an excuse soon)
It prompted me to ask the weather question we have all asked but I have never had a definitive answer: When we hear "Probability of precipitation in x on Sunday is y%", what does this mean? Is this statement a sum over all x (e.g. all UK) and all of Sunday i.e. the event that it will precipitate somewhere in UK sometime on Sunday? I can't see anything else that make sense, but I wd expect such probabilities to be close to 100% on virtually every day (and they are not). On the web I have found contradictory responses: e.g. sum over x, sum over Sunday, and sum over both. I'd appreciate any answer with web-link that will put my anxious mind at rest! :) Best Regards JOHN BIBBY for aa42.com Limited - International Data, Education and Trade Consultants Please visit www.aa42.com/mathemagic 1 Straylands Grove, York YO31 1EB (01904-330-334) -----Original Message----- From: A UK-based worldwide e-mail broadcast system mailing list [mailto:allstat@...] On Behalf Of Natalia Bochkina Sent: 08 October 2008 13:43 To: allstat@... Subject: Statistics Seminar - University of Edinburgh Statistics Seminar School of Mathematics The University of Edinburgh Friday 10 October 2008 3.00 p.m. Room 5327, James Clerk Maxwell Building Chris Glasbey (Biomathematics and Statistics Scotland) Spatio-temporal weather models (joint with Dave Allcroft) We develop consting spatio-temporal models for two weather variables: solar radiation and rainfall. For solar radiation the aim is to assess the performance of area networks of photo-voltaic cells. Although radiation measured at a sufficiently fine temporal scale has a bimodal marginal distribution (Glasbey, 2001), averages of 10-minute or longer duration can be transformed to be approximately Gaussian, and we fit a spatio-temporal auto-regressive moving average (STARMA) process (Glasbey and Allcroft, 2008). For rainfall, the aim is to disaggregate to a finer spatial scale than that observed. To overcome the difficulty that the marginal distribution of hourly rainfall has a singularity at zero and so is highly non-Gaussian, we apply a monotonic transformation. This defines a latent Gaussian variable, with zero rainfall corresponding to censored values below a threshold, which we model using a spatio-temporal Gaussian Markov random field (Allcroft and Glasbey, 2003). For both models, computations are simplified by approximating space by a torus and using Fourier transforms. Allcroft, D.J. and Glasbey, C.A. (2003). A latent Gaussian Markov random field model for spatio-temporal rainfall disaggregation. Applied Statistics, 52, 487-498. Glasbey CA (2001). Nonlinear autoregressive time series with multivariate Gaussian mixtures as marginal distributions. Applied Statistics, 50, 143-154. Glasbey, C.A. and Allcroft, D.J. (2008). A STARMA model for solar radiation. Applied Statistics, 57, 343-355. Tea and coffee will be available after the seminar in the Mathematics Common Room (5212). Natalia Bochkina N.Bochkina@... -- The University of Edinburgh is a charitable body, registered in Scotland, with registration number SC005336. |
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