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My experience with STATMOS Whitney Huang Department of Statistics, Purdue University Spatial Statistics Seminar April 20, 2015 STATMOS April 20, 2015 1 / 25

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  • My experience with STATMOS

    Whitney Huang

    Department of Statistics, Purdue University

    Spatial Statistics Seminar

    April 20, 2015

    STATMOS April 20, 2015 1 / 25

  • Outline

    1 About STATMOS

    2 Statistical Climatology

    3 STATMOS visits/projects

    STATMOS April 20, 2015 2 / 25

  • What is STATMOS

    NSF funded research network for statistical methods for atmosphericand oceanic Sciences

    Allow collaboration within the network

    Summer schools, research workshops, online seminar

    STATMOS April 20, 2015 3 / 25

    https://www.statmos.washington.edu/members.html

  • Summer schools

    PastI Ten Lectures on Statistical Climatology, UW Seattle 2012I Visualization of Climate Data, NCAR Boulder 2013I Spatio-Temporal Statistics, Búzios, Brazil 2014

    UpcomingI Data Assimilation, NCAR Boulder 2015

    STATMOS April 20, 2015 4 / 25

    https://www.statmos.washington.edu/?p=42https://www2.image.ucar.edu/event/vcd2013http://www.stat.washington.edu/peter/PASI/PASI_2014.htmlhttp://www.stat.osu.edu/~oksana/summer-school-in-data-assimilation-2015.html

  • Workshops

    PastI Spatial Statistics Workshop and INLA Shortcourse, CSU Fort Collins

    2013I BIRS workshop on Oceans and Climate variability, Banff, Alberta 2013I Workshop on Spatial Statistics, TAMU College Station 2015

    UpcomingI Big Data in Environmental Science Workshop, UBC Vancouver, British

    Columbia 2015I Workshop on high performance computing for spatial statistics, UM

    Ann Arbor 2015

    STATMOS April 20, 2015 5 / 25

    http://www.stat.colostate.edu/statdepartment/statnews/SpatialWorkshop.htmlhttp://www.birs.ca/events/2013/5-day-workshops/13w5104http://www.stat.tamu.edu/workshop-on-spatial-statistics/http://www.pims.math.ca/scientific-event/150511-bdeshttps://www.statmos.washington.edu/?p=1506

  • Online seminar

    “Climate model emulation and future climate simulation”, Prof.Michael Stein

    “Bayesian Approaches to the Use of Computer Models ”, Prof. MarkBerliner

    “Tales of Tail Dependence”, Prof. Dan Cooley

    “Matern-based nonstationary cross-covariance models for globalprocesses”, Prof. Mikyoung Jun

    “Evaluating predictive performance”, Dr. Michael Scheuerer

    “Multi-resolution spatial methods for large data sets”, Dr. DougNychka

    “Spatial statistics for environmental-health data”, Prof. MontseFuentes

    STATMOS April 20, 2015 6 / 25

    http://www.stat.osu.edu/~pfc/statmos-seminars/

  • Outline

    1 About STATMOS

    2 Statistical Climatology

    3 STATMOS visits/projects

    STATMOS April 20, 2015 7 / 25

  • Climate vs. weather

    Climate is what you expect · · ·

    Weather is what you get · · ·

    STATMOS April 20, 2015 8 / 25

  • Observational data vs. data product

    weather station observations (with homogenization and qualitycontrol)

    Gridded data product: irregularly spaced observations are convertedinto values on a regular grid to make it easier to plot or compare tomodel output or other data products.

    STATMOS April 20, 2015 9 / 25

  • Data product example: PRISM

    STATMOS April 20, 2015 10 / 25

  • Model based data products: reanalysis datasets

    Ingredients

    xt : a representation of the 3-dimensional state of the atmosphere attime t

    yt : the observational data record at time t

    xt+1 = M(xt): a state-of-the art numerical weather prediction (NWP)model,that advances the state forward a few hours

    An approximate sequential Bayes analysis

    Forecast using model: xt+1 = M(xt) giving a prior distribution [xt+1]

    Update information using yt : compute [xt+1|yt+1]

    Repeat cycle for full period of analysis

    STATMOS April 20, 2015 11 / 25

  • Climate models

    Figure : Slide courtesy of Steve Sain

    STATMOS April 20, 2015 12 / 25

  • Climate models

    Figure : Slide courtesy of Steve Sain

    STATMOS April 20, 2015 13 / 25

  • Climate models: GCM vs. RCM

    General Circulation Model (GCM): a mathematical model of thegeneral circulation of a planetary atmosphere or ocean

    GCMs are run at coarse spatial resolutions and are unable to resolveimportant sub-grid scale features

    Regional Climate Model (RCM): a dynamical downscaling uses alimited-area, high-resolution model driven by boundary conditionsfrom a GCM to derive smaller-scale information

    STATMOS April 20, 2015 14 / 25

  • Statistical Climatology and Spatial Statistics

    Weather and climate are inherently spatio-temporal phenomena

    Spatial interpolation for climate data

    Changes in climate extremes

    STATMOS April 20, 2015 15 / 25

  • Outline

    1 About STATMOS

    2 Statistical Climatology

    3 STATMOS visits/projects

    STATMOS April 20, 2015 16 / 25

  • University of Chicago (with Prof. Michael Stein)To determine how the temperature extremes may be affected byincreased atmospheric CO2 levels1000 years GCM equilibrium experiment with three CO2 levelsPropose a graphical tool for studying changes in extremes

    + + + + + + + + + + + + + + + +

    + + + + + + + + + + + + + + + +

    + + + + + + + + + + + + + + + +

    + + + + + + + + + + + + + + + +

    + + + + + + + + + + + + + + + +

    + + + + + + + + + + + + + + + ++

    ++

    30° N

    35° N

    40° N

    45° N

    50° N

    120° W 110° W 100° W 90° W 80° W 70° W

    STATMOS April 20, 2015 17 / 25

  • Changes in return levels of warm temperature extremes0

    12

    34

    56

    Lon= 124

    5

    Cha

    nge

    in r

    etur

    n le

    vel °

    C

    Return period

    Summer Tmax 700 ppm vs. 289 ppm

    lat= 46lat= 43lat= 39lat= 35lat= 32lat= 28mean

    120 116 112 109 105 101 98 94 90 86 82 79 75 71 68

    STATMOS April 20, 2015 18 / 25

  • Changes in return levels of cold temperature extremes0

    24

    68

    1012

    Lon= 124

    100

    Cha

    nge

    in r

    etur

    n le

    vel °

    C

    Return period

    Winter Tmin 700 ppm vs. 289 ppm

    lat= 46lat= 43lat= 39lat= 35lat= 32lat= 28mean

    120 116 112 109 105 101 98 94 90 86 82 79 75 71 68

    STATMOS April 20, 2015 19 / 25

  • Changes in return levels of temperature extremes

    STATMOS April 20, 2015 20 / 25

  • Argonne National Laboratory

    Located near Lemont, IL, outside Chicago, two hours drive fromPurdue

    Presented a seminar talk in the Environmental Science Division

    Collaborating with Dr. Wang on a temperature extremes projectusing a very high resolution RCM run

    STATMOS April 20, 2015 21 / 25

  • National Climatic Data Center

    Located in Asheville, North Carolina

    The largest active archive of weather data in the world

    Great place to get different kinds of climate data

    STATMOS April 20, 2015 22 / 25

  • National Center for Atmospheric Research

    Located in Boulder, Colorado

    Presented a seminar talk in the Institute for Mathematics Applied toGeosciences (IMAGe)

    Just finished a two weeks visit hosting by Dr. Doug Nychka

    STATMOS April 20, 2015 23 / 25

  • Log density estimation (with Dr. Doug Nychka)X : the variable of interest with density function f (x)Model: f (x) ∝ eg(x)The function estimation of g(x) is achieve by using a flexible class ofspline function

    Daily Precip (cm)

    Den

    sity

    0 5 10 15

    0.0

    0.5

    1.0

    1.5

    −−−

    GPDLogspline roughLogspline smooth

    −2 −1 0 1 2

    −10

    −6

    −2

    02

    Log daily precip

    Log

    dens

    ity

    STATMOS April 20, 2015 24 / 25

  • Thank you for your attention!

    STATMOS April 20, 2015 25 / 25

    About STATMOSStatistical ClimatologySTATMOS visits/projects