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Current System Applications: Cloud Analysis and Forecasting

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Title: Current System Applications: Cloud Analysis and Forecasting


1
Current System ApplicationsCloud Analysis and
Forecasting
  • PolarMax
  • 25 October 2005

Dr. Thomas Kopp The Aerospace Corporation Meteoro
logical Satellite Systems
2
Overview
  • A Brief History of Operational Satellite-Based
    Cloud Analysis
  • The Two-channel Approach (RTNEPH)
  • Adding the Mid-wave (CDFS II CLAVR)
  • Throwing In the Kitchen Sink (MODIS)
  • Operational Cloud Forecasting
  • Trajectory Based Approaches (ADVCLD)
  • The Problems With NWP
  • Putting It All Together, Where We Stand Today
    (Stochastic)

3
The Two Channel Approach
  • The Real-Time NEPHanalysis (RTNEPH)
  • Produced Global, Three-Dimensional Cloud Analyses
    For AFWA From 1973-2002 (30 years!)
  • Produced Cloud Cover Over An 8th Mesh Grid (25
    NM) Along With Cloud Top Temperature/Height
    Cloud Base Height
  • Used the Two Visual/IR Channels On the DMSP
  • If the Reflectance/Brightness Temperature Was
    Brighter/Colder Than the Surface, It Was A Cloud
  • Three-Dimensional Characteristics Were Based On
    the IR Temperature and Associated Ancillary Data
    (NWP)

4
DMSP Visual Over S. America
  • Scene is Over Chile and the Eastern Pacific
  • Can You Find the Clouds?

5
DMSP IR Over S. America
  • How About This One?

6
And Heres The Result
  • Everything Appears Correct
  • But Snow Over Andes Was Identified As Cloud

7
DMSP 3D Cloud Analysis
  • Example Cloud Products
  • Source CMNS
  • Algorithm SERCAA
  • F15 07Oct04 16Z
  • Total Cloud Amount ()
  • Visual Imagery (2.8km)

8
The Next Source - AVHRR
  • Included Three Additional Channels
  • Broke the Visual Channel Into Two Components
  • Added Additional Channels In the IR, One Mid-wave
    and the Other Long-wave
  • These Channels Led To Improved Cloud Detection
    Techniques
  • Two Visual Channels Allow For Ratio Calculations
    Between the Two Reflectances
  • Significant Improvement In Nighttime Cloud
    Detection Possible From the Addition Of the
    MWIR/LWIR
  • Besides Further Detection Algorithms, Cloud
    Detection Became Less Dependent On Ancillary Data

9
Different Approaches
  • AFWA Brought In These Newer Methods Via SERCAA
  • Science Basis For CDFS II Replaced the RTNEPH
    In 2002
  • Techniques Applied To Both Geostationary and
    Polar-Orbiting Satellite Data
  • Three-dimensional Aspects Unchanged
  • NOAA/NESDIS Scientists Developed CLAVR
  • Also Based Their Product On Applying All Five
    Channels In An Optimum Manner
  • But, Unlike CDFS II, Focus Included A Cloud
    Clearing Mode
  • Spatial Uniformity Test Designed For Partly
    Cloudy Conditions and Subpixel Scale Clouds

10
A CLAVR Example
  • N-18, Visual
  • Southeast Asia
  • Wheres the Cloud?

11
A CLAVR Example
  • N-18, IR

12
A CLAVR Example
  • The Result
  • Clouds Are White
  • Probably Cloudy Condition Indicated By Shades of
    Gray

13
The Latest Wrinkle - MODIS
  • Virtual Explosion Of Visual/IR Channels Available
  • MODIS Contains 32 Channels In the Visual/IR Range
  • Not All Employed For Clouds, Though Some Are Used
    To Find Non-Cloud Features That Could Appear As
    Clouds
  • Approximately 10 Cloud Detection Tests Have Been
    Developed, Each Designed For Specific Situations
  • Main Users However Desire Clear Conditions, Not
    Cloudy Ones
  • Has Led To Multiple Cloud Masks Depending On Need
  • Main Algorithm the Basis For VIIRS (NPOESS)
  • Significant Increase in Number of Tuning
    Thresholds Complicates Development and Evaluation

14
MODIS Example
15
MODIS Example
16
Cloud Forecasting
  • Forecasting Cloud Cover And 3D Cloud
    Characteristics Has Proven Difficult With Only
    Limited Advances In the Last 30 Years
  • AFWA Has Based Short-Term Cloud Forecasts On
    Trajectory Based Methods, And Still Does Today
  • ADVect CLouD (ADVCLD) Combines 3D Wind Flow From
    NWP With Cloud Characteristics From CDFS II
  • Method Rapidly Deteriorates After 9 Hours
  • NWP Approaches Do Not Use or Produce Cloud Cover
  • No Direct Cloud Inputs Are Used In NWP
  • Output Is Cloud Liquid/Ice Content, No Clear
    Correlation Between These And Cloud Cover

17
The Newest Addition To theForecasting Arsenal
  • Stochastic Cloud Forecast Model
  • Combines CDFS II Cloud Parameters And the NCEP
    Global Forecast System (GFS)
  • Uses 9 Pressure Levels and the Output of CDFS II
    (WWMCA)
  • Products Include Total Cloud Cover and Cloud
    Freeness Across Various Atmospheric Layers
  • Now in routine operations at AFWA, Including
    JAAWIN
  • Diagnostic Cloud Forecast Model
  • Combines CDFS II and Regional MM5 Model Output
  • Statistically Correlates WWMCA to MM5 Model
    Predictors

18
Stochastic Forecast Example
19
(No Transcript)
20
Summary
  • Operational Cloud Analysis Has Taken Advantage of
    the Increased Number of Channels On Various
    Polar-Orbiting Satellites
  • Trend Is For More Tests Identifying Specific
    Types of Clouds
  • Recently Developed Cloud Masks Account For
    Subpixel Clouds
  • Cloud Forecasting Remains A Challenge, Especially
    For Cloud Amounts and Layers
  • Trajectory Based Models Still Best in the Short
    Term
  • NWP Advances Have Not Crossed the Bridge Between
    Cloud Amount and Cloud Liquid Water/Ice
  • Newest Operational Methods Combine Cloud Analyses
    and NWP Without An Explicit Forecast From the NWP
    Models
  • NPOESS is the Next Step In Operational Cloud
    Analysis
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