State space model of precipitation rate Tamre Cardoso

Скачать презентацию State space model of precipitation rate Tamre Cardoso Скачать презентацию State space model of precipitation rate Tamre Cardoso

a7fcb4892ee8eb1a21c835f7130cb30e.ppt

  • Количество слайдов: 24

State space model of precipitation rate (Tamre Cardoso, Ph. D UW 2004) Updating wave State space model of precipitation rate (Tamre Cardoso, Ph. D UW 2004) Updating wave height forecasts using satellite data (Anders Malmberg, Ph. D U. Lund 2005) Model emulators (O’Hagan and coworkers )

Rainfall measurement Rain gauge (1 hr) High wind, low rain rate (evaporation) Spatially localized, Rainfall measurement Rain gauge (1 hr) High wind, low rain rate (evaporation) Spatially localized, temporally moderate Radar reflectivity (6 min) Attenuation, not ground measure Spatially integrated, temporally fine Cloud top temp. (satellite, ca 12 hrs) Not directly related to precipitation Spatially integrated, temporally sparse Distrometer (drop sizes, 1 min) Expensive measurement Spatially localized, temporally fine

Radar image Radar image

Drop size distribution Drop size distribution

Basic relations Rainfall rate: v(D) terminal velocity for drop size D N(t) number of Basic relations Rainfall rate: v(D) terminal velocity for drop size D N(t) number of drops at time t f(D) pdf for drop size distribution Gauge data: g(w) gauge type correction factor w(t) meteorological variables such as wind speed

Basic relations, cont. Radar reflectivity: Observed radar reflectivity: Basic relations, cont. Radar reflectivity: Observed radar reflectivity:

Structure of model Data: [G|N(D), q. G] [Z|N(D), q. Z] Processes: [N|m. N, q. Structure of model Data: [G|N(D), q. G] [Z|N(D), q. Z] Processes: [N|m. N, q. N] [D|xt, q. D] log GARCH LN Temporal dynamics: [m. N(t)|qm] AR(1) Model parameters: [q. G, q. Z, q. N, qm, q. D|q. H] Hyperparameters: q. H

MCMC approach MCMC approach

Observed and predicted rain rate Observed and predicted rain rate

Observed and calculated radar reflectivity Observed and calculated radar reflectivity

Wave height prediction Wave height prediction

Misalignment in time and space Misalignment in time and space

The Kalman filter Gauss (1795) least squares Kolmogorov (1941)-Wiener (1942) dynamic prediction Follin (1955) The Kalman filter Gauss (1795) least squares Kolmogorov (1941)-Wiener (1942) dynamic prediction Follin (1955) Swerling (1958) Kalman (1960) recursive formulation prediction depends on how far current state is from average Extensions

A state-space model Write the forecast anomalies as a weighted average of EOFs (computed A state-space model Write the forecast anomalies as a weighted average of EOFs (computed from the empirical covariance) plus small-scale noise. The average develops as a vector autoregressive model:

EOFs of wind forecasts EOFs of wind forecasts

Kalman filter forecast emulates forecast model Kalman filter forecast emulates forecast model

The effect of satellite data The effect of satellite data

Model assessment Difference from current forecast of Previous forecast Kalman filter Satellite data assimilated Model assessment Difference from current forecast of Previous forecast Kalman filter Satellite data assimilated

Statistical analysis of computer code output Often the process model is expensive to run Statistical analysis of computer code output Often the process model is expensive to run (in time, at least), especially if different runs needed for MCMC Need to develop real-time approximation to process model Kalman filter is a dynamic linear model approximation SACCO is an alternative Bayesian approach

Basic framework An emulator is a random (Gaussian) process (x) approximating the process model Basic framework An emulator is a random (Gaussian) process (x) approximating the process model for input x in Rm. Prior mean m(x) = h(x)T Prior covariance Run the model at n input values to get n output values, so

The emulator Integrating out and 2 we get where q = dim( ) and The emulator Integrating out and 2 we get where q = dim( ) and where t(x)T = (c(x, x 1), …, c(x, xn)) m** is the emulator, and we can also calculate its variance

An example y=7+x+cos(2 x) q=1, h. T(x)=(1 x) n=5 An example y=7+x+cos(2 x) q=1, h. T(x)=(1 x) n=5

Conclusions Model assessment constraints: • amount of data • data quality • ease of Conclusions Model assessment constraints: • amount of data • data quality • ease of producing model runs • degree of misalignment Ideally the model should have • similar first and second order properties to the data • similar peaks and troughs to data (or simulations based on the data)




  • Мы удаляем страницу по первому запросу с достаточным набором данных, указывающих на ваше авторство. Мы также можем оставить страницу, явно указав ваше авторство (страницы полезны всем пользователям рунета и не несут цели нарушения авторских прав). Если такой вариант возможен, пожалуйста, укажите об этом.