March 9, 1999Comet Class: SatMet 99-11 DERIVED MOTION FIELDS from the GOES SATELLITES Jaime Daniels...
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Transcript of March 9, 1999Comet Class: SatMet 99-11 DERIVED MOTION FIELDS from the GOES SATELLITES Jaime Daniels...
March 9, 1999 Comet Class: SatMet 99-1 1
DERIVED MOTION FIELDS from the DERIVED MOTION FIELDS from the GOES SATELLITESGOES SATELLITES
Jaime DanielsJaime Daniels
NOAA/NESDISNOAA/NESDIS
Office of Research and ApplicationsOffice of Research and Applications
Forecast Products Development TeamForecast Products Development Team
andand
Donald G. GrayDonald G. Gray
NOAA/NESDISNOAA/NESDIS
GOES Products ManagerGOES Products Manager
Office of Systems DevelopmentOffice of Systems Development
March 9, 1999 Comet Class: SatMet 99-1 2
Satellite Derived Motion Fields:Satellite Derived Motion Fields:TOPICSTOPICS
PhilosophyPhilosophy Review of GOES visible, IR, WV channelsReview of GOES visible, IR, WV channels Basic methodologyBasic methodology GOES-Next optimized data processing GOES-Next optimized data processing
strategiesstrategies GOES wind products - What’s new ?GOES wind products - What’s new ? VerificationVerification
March 9, 1999 Comet Class: SatMet 99-1 3
Satellite Derived Motion Fields:Satellite Derived Motion Fields:TOPICS cont’dTOPICS cont’d
Current and new/planned applicationsCurrent and new/planned applications SummarySummary Product availability and recommended Product availability and recommended
readingreading Discussion/questionsDiscussion/questions
March 9, 1999 Comet Class: SatMet 99-1 4
Satellite Derived Motion Fields:PHILOSOPHY
Clouds are “passive” tracers of winds at Clouds are “passive” tracers of winds at a single levela single level– use infrared and visible radiancesuse infrared and visible radiances
Water vapor features (ie., moisture Water vapor features (ie., moisture gradients are “passive” tracers of winds)gradients are “passive” tracers of winds)– both in clear air and cloudy conditionsboth in clear air and cloudy conditions– use water vapor infrared radiancesuse water vapor infrared radiances
We can properly assign height of tracerWe can properly assign height of tracer
March 9, 1999 Comet Class: SatMet 99-1 5
Satellite Derived Motion Fields:GOES Visible, IR, WV
Channels ImagerImager
– Water vapor channel (6.7um) Water vapor channel (6.7um) Band 3Band 3– Longwave IR window chan. (10.7um) Longwave IR window chan. (10.7um) Band 4Band 4– Visible Channel (0.65um) Visible Channel (0.65um) Band 1Band 1
SounderSounder– Water vapor channel (7.3um) Water vapor channel (7.3um) Band 10Band 10– Water vapor channel (7.0um) Water vapor channel (7.0um) Band 11Band 11
March 9, 1999 Comet Class: SatMet 99-1 6
Satellite Derived Motion Fields:BASIC METHODOLOGY
Image acquisitionImage acquisition
Automated registration of imageryAutomated registration of imagery
Target selection processTarget selection process
Height assignment of targetsHeight assignment of targets
Target tracking Target tracking
Quality control (Autoeditor)Quality control (Autoeditor)
March 9, 1999 Comet Class: SatMet 99-1 7
Satellite Derived Motion Fields: Image Acquisition
Select 3 consecutive images in timeSelect 3 consecutive images in time
Which channels are selected is a function of Which channels are selected is a function of
which wind product (cloud-drift, water which wind product (cloud-drift, water
vapor, visible) is to be generatedvapor, visible) is to be generated
Extended Northern Hemisphere Extended Northern Hemisphere
Southern HemisphereSouthern Hemisphere
Coverage Diagrams
March 9, 1999 Comet Class: SatMet 99-1 8
Satellite Derived Motion Fields:Auto-registration of Imagery
Registration is a measure of Registration is a measure of consistencyconsistency of of navigation between successive imagesnavigation between successive images
Landmark features (ie., coastlines) Landmark features (ie., coastlines) mustmust remain stationary from image to imageremain stationary from image to image
Satellite-derived winds are much more Satellite-derived winds are much more sensitive to sensitive to changes in registrationchanges in registration than to than to errors in navigationerrors in navigation
Navigation of the 3-axis stabilized GOES Navigation of the 3-axis stabilized GOES satellites much more difficultsatellites much more difficult
March 9, 1999 Comet Class: SatMet 99-1 9
Satellite Derived Motion Fields:Auto-registration (Cont’d)
Manual registration corrections applied Manual registration corrections applied operationally to imagery 5% of the timeoperationally to imagery 5% of the time
New automatedNew automated registration QC : registration QC : – hundreds of landmarks usedhundreds of landmarks used– each landmark is sought in all imageseach landmark is sought in all images– middle image in loop is assumed to have middle image in loop is assumed to have
“perfect” navigation“perfect” navigation– mean line and element correction is computed mean line and element correction is computed
and and possibly appliedpossibly applied for the 1st and 3rd image for the 1st and 3rd image
March 9, 1999 Comet Class: SatMet 99-1 10
Satellite Derived Motion Fields:TARGET SELECTION PROCESS
Consider small sub-areas (target area) of Consider small sub-areas (target area) of
an image in successionan image in succession
Perform a spatial coherence analysis of Perform a spatial coherence analysis of
all targets. all targets. Filter outFilter out targets where: targets where:
– scene is too “coherent”scene is too “coherent”
– multi-deck cloud signatures are evidentmulti-deck cloud signatures are evident
March 9, 1999 Comet Class: SatMet 99-1 11
Satellite Derived Motion Fields:TARGET SELECTION PROCESS (Cont’d)
Locate maxima in brightnessLocate maxima in brightness
Select target/feature associated with Select target/feature associated with
strongest gradientstrongest gradient
Target density is controlled by size of Target density is controlled by size of
target selector areatarget selector area
March 9, 1999 Comet Class: SatMet 99-1 12
Satellite Derived Motion Fields:Height Assignment of Targets
Infrared window techniqueInfrared window technique– oldest method of assigning heights to cloud-oldest method of assigning heights to cloud-
motion windsmotion winds– not suitablenot suitable for assigning heights of semi- for assigning heights of semi-
transparent cloud (ie., thin cirrus)transparent cloud (ie., thin cirrus)– still provides a still provides a suitable fallbacksuitable fallback to other to other
methodsmethods
March 9, 1999 Comet Class: SatMet 99-1 13
Satellite Derived Motion Fields:Target Height Assignment (Cont’d)
COCO22 Slicing Technique Slicing Technique
– most accuratemost accurate means of assigning heights to means of assigning heights to
semi-transparent tracerssemi-transparent tracers
– utilizes IR window and COutilizes IR window and CO22 (13um) absorption (13um) absorption
channels viewing the same FOV channels viewing the same FOV
– However, COHowever, CO22 absorption band absorption band absentabsent on on
current GOES imagerscurrent GOES imagers
March 9, 1999 Comet Class: SatMet 99-1 14
Satellite Derived Motion Fields:Satellite Derived Motion Fields:Target Height Assignment (Cont’d)Target Height Assignment (Cont’d)
HH22O Intercept MethodO Intercept Method
– Utilizes WV channel (6.7um) Utilizes WV channel (6.7um) Band 3 Band 3 and and
longwave IR window chan. (10.7um) longwave IR window chan. (10.7um) Band 4Band 4
– Algorithm: these two sets of radiances from a Algorithm: these two sets of radiances from a
single-level cloud decksingle-level cloud deck vary linearly with cloud vary linearly with cloud
amountamount
– Adequate replacementAdequate replacement of CO of CO22 slicing method slicing method
March 9, 1999 Comet Class: SatMet 99-1 15
Satellite Derived Motion Fields:Satellite Derived Motion Fields:TARGET TRACKING ALGORITHMTARGET TRACKING ALGORITHM
Define tracking area centered over each targetDefine tracking area centered over each target Search area in second image which best Search area in second image which best
matches radiances in tracking areamatches radiances in tracking area Confine search to “search” area centered Confine search to “search” area centered
around guess (AVN Forecast) displacement of around guess (AVN Forecast) displacement of targettarget
Two vectors per target: 1 for image 1&2; 1 for Two vectors per target: 1 for image 1&2; 1 for image 2&3image 2&3
March 9, 1999 Comet Class: SatMet 99-1 16
Satellite Derived Motion Fields:Quality Control (Autoeditor)
FunctionsFunctions– Target height reassignmentTarget height reassignment
– Wind quality estimation flagWind quality estimation flag Method (4 Steps)Method (4 Steps)
– 1)1) 3-dimensional objective analysis 3-dimensional objective analysis of model forecast wind field on 1st passof model forecast wind field on 1st pass
– 2)2) Incorporate satwinds into analysis on Incorporate satwinds into analysis on 2nd pass. 2nd pass. Remove those differing Remove those differing significantlysignificantly from analysis from analysis
March 9, 1999 Comet Class: SatMet 99-1 17
Satellite Derived Motion Fields:Quality Control (Cont’d)
Method (Cont’d)Method (Cont’d)– 3)3) Target heights readjusted by minimizing Target heights readjusted by minimizing
a penalty function which seeks the a penalty function which seeks the optimum “fit”optimum “fit” of the vector to the of the vector to the analysisanalysis
– 4)4) Perform another 3-dimensional Perform another 3-dimensional objective analysis (objective analysis (at reassigned at reassigned pressurespressures) and assign quality flag) and assign quality flag
March 9, 1999 Comet Class: SatMet 99-1 18
Height Assignment Related to Satellite Wind Type (Approximations)
Imager Cloud Drift Winds
Imager Water Vapor Winds
Imager Visible Winds
Sounder Water Vapor Winds
100mb - 250mb - 400mb - 600mb - 250mb 400mb 600mb 1000mb35% 30% 20% 15%
55% 40% <5% <5%
N/A N/A N/A 30% 600-800 70% 800-1000
<5% 55% 40% <5%
March 9, 1999 Comet Class: SatMet 99-1 19
GOES High Density Water Vapor Winds
100mb - 250mb
250mb - 400mb
400mb - 700mb
March 9, 1999 Comet Class: SatMet 99-1 20
GOES High Density Cloud Drift Winds
100mb - 400mb
400mb - 700mb
Below 700mb
March 9, 1999 Comet Class: SatMet 99-1 21
GOES High Density Winds(Cloud Drift, Imager H2O, Sounder H2O)
March 9, 1999 Comet Class: SatMet 99-1 23
GOES High Density Visible WindsTropical System Circulations
Hurricane Earl
800mb-1000mb
> 34 Knots(Tropical Storm
Strength)
March 9, 1999 Comet Class: SatMet 99-1 24
Satellite Derived Motion Fields:Optimal Data Processing Strategies Take advantage of new sensor technologyTake advantage of new sensor technology
– silicon photodiode detectors (improved signal-to-noise)silicon photodiode detectors (improved signal-to-noise)
– higher spatial resolution and bit depthhigher spatial resolution and bit depth
– improved spectral sampling & sampling ratesimproved spectral sampling & sampling rates
Take advantage of automation techniques and Take advantage of automation techniques and processing powerprocessing power– eliminate manual labor-intensive taskseliminate manual labor-intensive tasks– increase data volumeincrease data volume
March 9, 1999 Comet Class: SatMet 99-1 25
Satellite Derived Motion Fields:Optimal Data Processing Strategies Take advantage of improved viewing capabilityTake advantage of improved viewing capability
– temporal sampling (including rapid scans)temporal sampling (including rapid scans)
– independent imager and sounderindependent imager and sounder
OptimizeOptimize processing strategy processing strategy– high data volume/density (x,y,z,t) coveragehigh data volume/density (x,y,z,t) coverage
– multi-spectral data integration (Hmulti-spectral data integration (H2 2 O winds)O winds)
– multi-satellite (data fusion)multi-satellite (data fusion)
March 9, 1999 Comet Class: SatMet 99-1 26
Satellite Derived Motion Fields:Satellite Derived Motion Fields:Optimal Data Processing StrategiesOptimal Data Processing Strategies Focus processing strategy Focus processing strategy towards the towards the
meteorologymeteorology– circulations and environmental featurescirculations and environmental features
AdaptAdapt the data quality control the data quality control Take advantage of improved Take advantage of improved
communicationscommunications– timely data disseminationtimely data dissemination
March 9, 1999 Comet Class: SatMet 99-1 28
Satellite Derived Motion Fields: GOES Wind Products: What’s New ?
Product Coverage Frequency
Cloud-drift*10.7 um (Band 4)High Density
NH,SH 8x/day
Water vapor*
6.7 um (Band 3)High Density
NH,SH 8x/day
Sounder WV7.3 um (Band
10)7.0 um (Band 11)
Tropical Scans 4x/day
Visible0.65 um (Band 1)
Atlantic/Pacific
4x/day
March 9, 1999 Comet Class: SatMet 99-1 29
Satellite Derived Motion Fields:Current and New/Planned Applications Mid-latitude Oceanic AnalysesMid-latitude Oceanic Analyses
– NWS offices have access to high density wind productsNWS offices have access to high density wind products via internet; AWIPS access to follow via internet; AWIPS access to follow
Numerical Weather Prediction (NWP) and Data Numerical Weather Prediction (NWP) and Data AssimilationAssimilation– What’s happening at NCEP/EMC ?What’s happening at NCEP/EMC ?– ECMWF is utilizing GOES high density wind productsECMWF is utilizing GOES high density wind products
Tropical Cyclone Analysis and ForecastingTropical Cyclone Analysis and Forecasting– Tropical Prediction Center (TPC) has access to the GOES Tropical Prediction Center (TPC) has access to the GOES
multi-spectral wind data setsmulti-spectral wind data sets– GFDL & NRL are performing model impact studies using the GFDL & NRL are performing model impact studies using the
GOES multi-spectral winds to improve tropical storm track GOES multi-spectral winds to improve tropical storm track forecastsforecasts
– CIMSS routinely generating water vapor and visible winds CIMSS routinely generating water vapor and visible winds from GMS-5from GMS-5
March 9, 1999 Comet Class: SatMet 99-1 30
Satellite Derived Motion Fields:NWP and Data Assimilation
EMC Status/PlansEMC Status/Plans
Operational use of high density Cloud Drift winds Operational use of high density Cloud Drift winds
in Global and Regional forecast models began in in Global and Regional forecast models began in December 1997.December 1997.
Evaluation of high density Water Vapor (imager Evaluation of high density Water Vapor (imager
and sounder) and Visible winds planned for 1999 - and sounder) and Visible winds planned for 1999 - focus on assimilation of focus on assimilation of layerlayer wind estimates. wind estimates.
March 9, 1999 Comet Class: SatMet 99-1 31
Satellite Derived Motion Fields:NWP and Data Assimilation
NESDIS Status/PlansNESDIS Status/Plans– Routine production of GOES sounder WV and VIS Routine production of GOES sounder WV and VIS
winds began in late 1997. Work with EMC to winds began in late 1997. Work with EMC to support evaluation in EMC operational database in support evaluation in EMC operational database in 1999.1999.
– NESDIS/CIMSS and FSL will coordinate on model NESDIS/CIMSS and FSL will coordinate on model impact study involving the generation of multi-impact study involving the generation of multi-spectral (vis,ir,wv) windsspectral (vis,ir,wv) winds and their assimilation into and their assimilation into the MAPS/RUC modelsthe MAPS/RUC models.
March 9, 1999 Comet Class: SatMet 99-1 32
Satellite Derived Motion Fields:Satellite Derived Motion Fields:VVerificationerification
Sources of errors in satellite-derived windsSources of errors in satellite-derived winds Satellite winds vs. rawinsondes vs. model Satellite winds vs. rawinsondes vs. model
colocation statisticscolocation statisticsModel impact studiesModel impact studies Satellite minus forecast wind fieldSatellite minus forecast wind fieldMean tropical storm track forecast errorsMean tropical storm track forecast errors
March 9, 1999 Comet Class: SatMet 99-1 33
Comparison of Model Forecast and Satellite Derived Wind FieldsAVN Forecast
AVN Forecast + Sat Winds
March 9, 1999 Comet Class: SatMet 99-1 36
Satellite Derived Motion Fields:Satellite Derived Motion Fields:Sources of ErrorsSources of Errors
Assumption that clouds and water vapor Assumption that clouds and water vapor
features are passive tracers of the wind features are passive tracers of the wind
fieldfield
Image registration errorsImage registration errors
Target identification and tracking errorsTarget identification and tracking errors
Inaccurate height assignment of targetInaccurate height assignment of target
March 9, 1999 Comet Class: SatMet 99-1 37
Satellite Derived Motion Fields:Satellite Derived Motion Fields:SummarySummary
Higher resolution data, improved science, and full automationHigher resolution data, improved science, and full automation
- resulted in satwinds which are superior in both quality - resulted in satwinds which are superior in both quality
and quantity to any done previously at NOAA/NESDISand quantity to any done previously at NOAA/NESDIS
Improved automated QCImproved automated QC is the most significant change in the is the most significant change in the
winds processing system over the past 5 yearswinds processing system over the past 5 years
Improved target selectionImproved target selection avoids mix-level scenes and avoids mix-level scenes and
concentrates on providing greater targeting density for concentrates on providing greater targeting density for
features of interest. features of interest. Water vapor intercept method.Water vapor intercept method. Numerous applicationsNumerous applications
March 9, 1999 Comet Class: SatMet 99-1 38
Satellite Derived Motion Fields:Product Availability & References
E-mail: E-mail: [email protected]@nesdis.noaa.gov
[email protected]@noaa.gov
Web SitesWeb Sites– http://cimss.ssec.wisc.edu http://cimss.ssec.wisc.edu
– http://orbit-net.nesdis.noaa.gov/goes/wind.htmlhttp://orbit-net.nesdis.noaa.gov/goes/wind.html
Reference MaterialReference Material– Nieman et al., 1997: Fully automated cloud-drift winds in NESDIS Nieman et al., 1997: Fully automated cloud-drift winds in NESDIS
operations. Bull. Amer. Meteor. Soc., 78, 1121-1133.operations. Bull. Amer. Meteor. Soc., 78, 1121-1133.– Veldon et. al., 1997: Upper-tropospheric winds derived from geostationary Veldon et. al., 1997: Upper-tropospheric winds derived from geostationary
satellite water vapor observations. Bull. Amer. Meteor. Soc., 78, 173-195.satellite water vapor observations. Bull. Amer. Meteor. Soc., 78, 173-195.