Development of Inter-model differences

Slides:



Advertisements
Similar presentations
Sampling: Final and Initial Sample Size Determination
Advertisements

Sampling Distributions (§ )
Statistical properties of Random time series (“noise”)
Probability Probability; Sampling Distribution of Mean, Standard Error of the Mean; Representativeness of the Sample Mean.
Approaches to Data Acquisition The LCA depends upon data acquisition Qualitative vs. Quantitative –While some quantitative analysis is appropriate, inappropriate.
CHAPTER 16 MARKOV CHAIN MONTE CARLO
Sampling Distributions. Review Random phenomenon Individual outcomes unpredictable Sample space all possible outcomes Probability of an outcome long-run.
Ch 6 Introduction to Formal Statistical Inference.
Chapter 14 Simulation. Monte Carlo Process Statistical Analysis of Simulation Results Verification of the Simulation Model Computer Simulation with Excel.
Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric.
/k Variation thinking 2WS02 Industrial Statistics A. Di Bucchianico.
Standard error of estimate & Confidence interval.
Review of Probability.
Why We Care or Why We Go to Sea.
Grid for Coupled Ensemble Prediction (GCEP) Keith Haines, William Connolley, Rowan Sutton, Alan Iwi University of Reading, British Antarctic Survey, CCLRC.
GEO7600 Inverse Theory 09 Sep 2008 Inverse Theory: Goals are to (1) Solve for parameters from observational data; (2) Know something about the range of.
Methodological approach to parameter perturbations in GEM-LAM simulations Leo Separovic, Ramon de Elia and Rene Laprise.
Montecarlo Simulation LAB NOV ECON Montecarlo Simulations Monte Carlo simulation is a method of analysis based on artificially recreating.
Probabilistic Mechanism Analysis. Outline Uncertainty in mechanisms Why consider uncertainty Basics of uncertainty Probabilistic mechanism analysis Examples.
Hypothesis test in climate analyses Xuebin Zhang Climate Research Division.
Ch 6 Introduction to Formal Statistical Inference
Shuhei Maeda Climate Prediction Division
Seasonal Modeling (NOAA) Jian-Wen Bao Sara Michelson Jim Wilczak Curtis Fleming Emily Piencziak.
Machine Design Under Uncertainty. Outline Uncertainty in mechanical components Why consider uncertainty Basics of uncertainty Uncertainty analysis for.
Probability Theory Modelling random phenomena. Permutations the number of ways that you can order n objects is: n! = n(n-1)(n-2)(n-3)…(3)(2)(1) Definition:
Robert W. Pinder, Alice B. Gilliland, Robert C. Gilliam, K. Wyat Appel Atmospheric Modeling Division, NOAA Air Resources Laboratory, in partnership with.
1 First results and methodological approach to parameter perturbations in GEM-LAM simulations PART II Leo Separovic, Ramon de Elia and Rene Laprise.
Chapter 18 - Part 2 Sampling Distribution Models for.
Geology 6600/7600 Signal Analysis 09 Sep 2015 © A.R. Lowry 2015 Last time: Signal Analysis is a set of tools used to extract information from sequences.
Random Numbers RANDOM VS PSEUDO RANDOM. Truly Random numbers  From Wolfram: “A random number is a number chosen as if by chance from some specified distribution.
Module 17 MM5: Climate Simulation BREAK. Regional Climate Simulation for the Pan-Arctic using MM5 William J. Gutowski, Jr., Helin Wei, Charles Vörösmarty,
1 Probability and Statistics Confidence Intervals.
A study on the spread/error relationship of the COSMO-LEPS ensemble Purpose of the work  The spread-error spatial relationship is good, especially after.
The application of ensemble Kalman filter in adaptive observation and information content estimation studies Junjie Liu and Eugenia Kalnay July 13th, 2007.
Sampling Distributions Chapter 18. Sampling Distributions If we could take every possible sample of the same size (n) from a population, we would create.
1 First results and methodological approach to parameter perturbations in GEM-LAM simulations PART I Leo Separovic, Ramon de Elia and Rene Laprise.
Introduction to the Practice of Statistics Fifth Edition Chapter 5: Sampling Distributions Copyright © 2005 by W. H. Freeman and Company David S. Moore.
Bias and Variability Lecture 27 Section 8.3 Wed, Nov 3, 2004.
Chapter 9 Sampling Distributions 9.1 Sampling Distributions.
National Oceanic and Atmospheric Administration’s National Weather Service Colorado Basin River Forecast Center Salt Lake City, Utah 11 The Hydrologic.
CHAPTER 10 Comparing Two Populations or Groups
Land Use in Regional Climate Modeling
Data Analysis.
An Introduction to the Climate Change Explorer Tool: Locally Downscaled GCM Data for Thailand and Vietnam Greater Mekong Sub-region – Core Environment.
Parameter versus statistic
Python Random numbers Peter Wad Sackett.
Grid Point Models Surface Data.
Introduction to estimation: 2 cases
Toward statistical inference
How Good is a Model? How much information does AIC give us?
Question 1 Given that the globe is warming, why does the DJF outlook favor below-average temperatures in the southeastern U. S.? Climate variability on.
Interval Estimation.
Data Analysis and Statistical Software I ( ) Quarter: Autumn 02/03
Random vs pseudo random
MEGN 537 – Probabilistic Biomechanics Ch.3 – Quantifying Uncertainty
Leo Separovic, Ramón de Elía, René Laprise and Adelina Alexandru
WGCM/WGSIP decadal prediction proposal
Section 7.7 Introduction to Inference
Andy Wood and Dennis P. Lettenmaier
Python Random numbers Peter Wad Sackett.
Additional notes on random variables
Additional notes on random variables
Computer Simulation Techniques Generating Pseudo-Random Numbers
Sampling Distributions (§ )
Influence of large-scale nudging on RCM’s internal variability
Sampling Distributions
Sampling Distributions
Simulation Berlin Chen
Maximum Likelihood Estimation (MLE)
Presentation transcript:

Development of Inter-model differences Example - pan-Arctic simulation

Model domain Baseline Run: 1 Oct. 1985 - 30 Sep. 1986 (grid: 51 x 91; 120 km) Baseline Run: 1 Oct. 1985 - 30 Sep. 1986 Wetlands Runs: 1 April 1986 - 30 Sep. 1986 Sensitivity Runs: Oct 85 or July 86

500 hPa Heights: RMS Difference vs. Time (MM5-NCEP) 150 100 50 [m] 1 OCT 1 NOV

RMS Difference vs. Baseline (500 hPa)

Random Numbers on a Computer Goals: Evenly distributed set of numbers in some range All sequences statistically independent of others Generated by an algorithm Hence, repeatable Hence, not truly random “Seed” gives a starting point for the algorithm True Random Numbers? Sample physical phenomena with known statistical properties Example: www.random.org

Ensemble Simulation Recognizes inherent “noise” of climate system Adds noise via starting conditions of forecast or climate simulation via changes in parameters or parameterizations Used to sample noise versus signal Ensemble: average appears to give more accurate result spread indicates periods of greater uncertainty?

Ensemble EdGCM Simulation