1
Introduction It is a cooperative effort between the National Oceanic and Atmospheric Administration (NOAA) and the European Organization for the Exploitation of Meteorological (EUMETSAT) to provide and improve the operational meteorological and environmental forecasting and global climate monitoring services worldwide. The NOAA National Environmental Satellite, Data, and Information Services (NESDIS) has been a pioneer in producing and distributing atmospheric sounding data products as a part of its operation for operating a fleet of civilian, Polar Orbiting Environmental Satellites (POES) and providing users and researchers a suite of operational atmospheric and environmental data products. Sounding Data Products are being generated from the advance TIROS Operational Vertical Sounder (ATOVS), onboard NOAA polar orbiting satellites (currently operational NOAA-15 and NOAA-18), and Infrared Atmospheric Sounding Interferometer (IASI) onboard Meteorological Operational Satellite (MetOp-1). IASI is a state-of-the-art sounding system developed to support Initial Joint Polar-Orbiting Operational Satellite System at NESDIS for generating operational calibrated and navigated radiances, reconstructed radiances, cloud cleared radiances, principal components, temperature profile, water vapor profile, ozone profile, and trace gases profiles such as methane, carbon dioxide, and carbon monoxide. IASI is a Fourier Transform Spectrometer based upon a Michelson Interferometer (8461 channels), spectral range from 645 to 2760 cm-1, with a constant sample spectral interval at a 0.25 cm, and apodized spectral resolution at a 0.5 cm. It provides enhancements to the NESDIS current operational ATOVS sounding system to generate temperature and moisture profiles with a vertical accuracy of 1 degree Kelvin and 10% per 1-km layer, respectively. Recently, the IASI level -1 products system was successfully transitioned into operation at NESDIS. It was declared operational in October 2007. Level-1 data have been made available to both real-time users and climate users through NESDIS Environment Satellite Processing Center (ESPC) Data Distribution Sever (DDS) and Comprehensive Large Array-data Stewardship System (CLASS). In this presentation, we discuss the transition of IASI from research to operation, its operational implementation procedures, products validation, monitoring and dissemination. This presentation will include the discussion on the ESPC system architecture involving sounding data processing and distribution for ATOVS and IASI, improvements made for data quality measurements, pipeline processing and distribution via DDS, and user timeliness requirements envisioned from the next generation of satellites. There have been significant changes in the operational system due to system upgrades, algorithm updates, and value added data products and services. User requirements for data products and services for sounders like ATOVS and IASI would help us determine the products and services required from the next generation of sounders such as Cross-Track Infrared Sounder/ Advanced Technology Microwave Sounder (Cris/ATMS) as planned for the National Polar-orbiting Operational Environmental Satellite System (NPOESS) program and the future missions of the EUMSAT satellites. Detailed information on the operational products and their applications are also presented. NOAA/NESDIS UPDATES ON OPERATIONAL SOUNDING DATA PRODUCTS AND SERVICES A.K. Sharma NOAA/NESDIS Office of Satellite Data Processing and Distribution – OSDPD Near Real-Time IASI Data Browse Granule Data Monitoring (Granule data comes in ~3-minutes) Click Granule in the Granule Map below to Browse the image or Click Granule number in the table: [Show Granule Table] A Near Real- Time IASI Data Browse Data Available Data Unavailable 04/18/2008 001 04/18/2008 002 04/18/2008 003 04/18/2008 004 04/18/2008 005 04/18/2008 006 04/18/2008 007 04/18/200 8 04/18/2008 009 04/18/2008 010 04/18/2008 011 04/18/2008 012 04/18/2008 013 04/18/2008 014 04/18/2008 015 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/200 8 023 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 031 04/18/2008 032 04/18/2008 033 04/18/2008 034 04/18/2008 035 04/18/2008 036 04/18/2008 037 04/18/200 8 04/18/2008 039 04/18/2008 040 04/18/2008 041 04/18/2008 042 04/18/2008 043 04/18/2008 044 04/18/2008 045 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/200 8 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 061 04/18/2008 062 04/18/2008 063 04/18/2008 064 04/18/2008 065 04/18/2008 066 04/18/2008 067 04/18/200 8 04/18/2008 069 04/18/2008 070 04/18/2008 071 04/18/2008 072 04/18/2008 073 04/18/2008 074 04/18/2008 075 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/200 8 083 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 04/18/2008 361 04/18/2008 362 04/18/2008 363 04/18/2008 364 04/18/2008 365 04/17/2008 366 04/17/2008 367 04/17/200 8 04/17/2008 369 04/17/2008 370 04/17/2008 371 04/17/2008 372 04/17/2008 373 04/17/2008 374 04/17/2008 375 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/200 8 383 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 391 04/17/2008 392 04/17/2008 393 04/17/2008 394 04/17/2008 395 04/17/2008 396 04/17/2008 397 04/17/200 8 04/17/2008 399 04/17/2008 400 04/17/2008 401 04/17/2008 402 04/17/2008 403 04/17/2008 404 04/17/2008 405 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/200 8 413 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 421 04/17/2008 422 04/17/2008 423 04/17/2008 424 04/17/2008 425 04/17/2008 426 04/17/2008 427 04/17/200 8 04/17/2008 429 04/17/2008 430 04/17/2008 431 04/17/2008 432 04/17/2008 433 04/17/2008 434 04/17/2008 435 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/200 8 443 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 04/17/2008 Cloud Cleared Radiances Global Grids Data Retrieved Temperature and Water Vapor at ~800mb The plot is the IASI cloud cleared radiance (CCR) at the channel 965.5cm-1. Browsing the map can check if the CCR range is reasonable. Ch-15 Ch-1 Global Grids Data Compare retrieved Temperature with ECMWF at ~500mb AMSU MHS ATOVS IASI L1C Monitoring Interface System Diagram of NOAA Retrieval Algorithm: Operational Mode Retrieval products Diagnostic tools AIRS IASI Retrieval Code CrIS Sequence of Steps of the Retrieval Algorithm 1) A microwave retrieval module which derives cloud liquid water flags and microwave surface emissivity uncertainty; 2) A fast eigenvector regression retrieval for temperature and moisture that is trained using the ECMWF analysis and IASI cloudy radiances; 3) A cloud clearing module that uses a set of microwave and IR channels to produce the cloud-cleared IR radiance product and reject those cases violating the cloud-clearing requirements; 4) A fast eigenvector regression retrieval for temperature and moisture that is trained using the ECMWF analysis and IASI cloud cleared radiances; 5) The final IR retrieval module, which uses the regression retrieval as an initial solution and produces the final version of the physical retrieval by an iterated regularized least squared minimization. We start with the temperature retrieval, because temperature is the most linear component of the RTA equation, followed by water vapor, ozone, etc. All adjustments to the algorithm pertain the first 5 steps. Optimizations of the parameters involved in the following trace gas retrievals are only minor adjustments. Simplified flow diagram of the NOAA retrieval algorithm Microwave Physical for T(p), q(p), LIQ(p), ε(f) Climatological First Guess Initial Cloud Clearing, ηj , Rccr Improved Cloud Clearing, ηj , Rccr Final Cloud Clearing, ηj , Rccr R ccr Regression for Ts, ε(ν), T(p), q(p) IR Physical T s , ε(ν), ρ(ν) IR Physical T s , ε(ν), ρ(ν) IR Physical T(p) IR Physical T(p) IR Physical T s , ε(ν), ρ(ν) IR Physical q(p) IR Physical O 3 (p) IR Physical CO(p) IR Physical HNO 3 (p) IR Physical CH 4 (p) IR Physical CO 2 (p) IR Physical N 2 O(p) MIT FG CCR RET R warm Regression for Ts, T(p), q(p) ATOVS Weekly Vertical Statistics Soundings ATOVS Monitoring-

NOAA/NESDIS UPDATES ON OPERATIONAL SOUNDING DATA … · This presentation will include the discussion on the ESPC system architecture involving sounding data processing and distribution

  • Upload
    others

  • View
    0

  • Download
    0

Embed Size (px)

Citation preview

Page 1: NOAA/NESDIS UPDATES ON OPERATIONAL SOUNDING DATA … · This presentation will include the discussion on the ESPC system architecture involving sounding data processing and distribution

IntroductionIt is a cooperative effort between the National Oceanic and Atmospheric Administration (NOAA) and the European Organization for the Exploitation of Meteorological (EUMETSAT) to provide and improve the operational meteorological and environmental

forecasting and global climate monitoring services worldwide. The NOAA National Environmental Satellite, Data, and Information Services (NESDIS) has been a pioneer in producing and distributing atmospheric sounding data products as a part of its operation for operating a fleet of civilian, Polar Orbiting Environmental Satellites (POES) and providing users and researchers a suite of operational atmospheric and environmental data products. Sounding Data Products are being generated from the

advance TIROS Operational Vertical Sounder (ATOVS), onboard NOAA polar orbiting satellites (currently operational NOAA-15 and NOAA-18), and Infrared Atmospheric Sounding Interferometer (IASI) onboard Meteorological Operational Satellite (MetOp-1). IASI is a state-of-the-art sounding system developed to support Initial Joint Polar-Orbiting Operational Satellite System at NESDIS for generating operational calibrated and navigated radiances, reconstructed radiances, cloud cleared radiances, principal

components, temperature profile, water vapor profile, ozone profile, and trace gases profiles such as methane, carbon dioxide, and carbon monoxide. IASI is a Fourier Transform Spectrometer based upon a Michelson Interferometer (8461 channels), spectral range from 645 to 2760 cm-1, with a constant sample spectral interval at a 0.25 cm, and apodized spectral resolution at a 0.5 cm. It provides enhancements to the NESDIS current operational ATOVS sounding system to generate temperature and

moisture profiles with a vertical accuracy of 1 degree Kelvin and 10% per 1-km layer, respectively. Recently, the IASI level -1 products system was successfully transitioned into operation at NESDIS. It was declared operational in October 2007. Level-1 data have been made available to both real-time users and climate users through NESDIS Environment Satellite Processing Center (ESPC) Data Distribution Sever (DDS) and Comprehensive Large Array-data Stewardship System (CLASS). In this presentation,

we discuss the transition of IASI from research to operation, its operational implementation procedures, products validation, monitoring and dissemination. This presentation will include the discussion on the ESPC system architecture involving sounding data processing and distribution for ATOVS and IASI, improvements made for data quality measurements, pipeline processing and distribution via DDS, and user timeliness requirements envisioned from the next generation of satellites. There have been

significant changes in the operational system due to system upgrades, algorithm updates, and value added data products and services. User requirements for data products and services for sounders like ATOVS and IASI would help us determine the products and services required from the next generation of sounders such as Cross-Track Infrared Sounder/ Advanced Technology Microwave Sounder (Cris/ATMS) as planned for the National Polar-orbiting Operational Environmental Satellite System

(NPOESS) program and the future missions of the EUMSAT satellites. Detailed information on the operational products and their applications are also presented.

IntroductionIt is a cooperative effort between the National Oceanic and Atmospheric Administration (NOAA) and the European Organization for the Exploitation of Meteorological (EUMETSAT) to provide and improve the operational meteorological and environmental

forecasting and global climate monitoring services worldwide. The NOAA National Environmental Satellite, Data, and Information Services (NESDIS) has been a pioneer in producing and distributing atmospheric sounding data products as a part of its operation for operating a fleet of civilian, Polar Orbiting Environmental Satellites (POES) and providing users and researchers a suite of operational atmospheric and environmental data products. Sounding Data Products are being generated from the

advance TIROS Operational Vertical Sounder (ATOVS), onboard NOAA polar orbiting satellites (currently operational NOAA-15 and NOAA-18), and Infrared Atmospheric Sounding Interferometer (IASI) onboard Meteorological Operational Satellite (MetOp-1). IASI is a state-of-the-art sounding system developed to support Initial Joint Polar-Orbiting Operational Satellite System at NESDIS for generating operational calibrated and navigated radiances, reconstructed radiances, cloud cleared radiances, principal

components, temperature profile, water vapor profile, ozone profile, and trace gases profiles such as methane, carbon dioxide, and carbon monoxide. IASI is a Fourier Transform Spectrometer based upon a Michelson Interferometer (8461 channels), spectral range from 645 to 2760 cm-1, with a constant sample spectral interval at a 0.25 cm, and apodized spectral resolution at a 0.5 cm. It provides enhancements to the NESDIS current operational ATOVS sounding system to generate temperature and

moisture profiles with a vertical accuracy of 1 degree Kelvin and 10% per 1-km layer, respectively. Recently, the IASI level -1 products system was successfully transitioned into operation at NESDIS. It was declared operational in October 2007. Level-1 data have been made available to both real-time users and climate users through NESDIS Environment Satellite Processing Center (ESPC) Data Distribution Sever (DDS) and Comprehensive Large Array-data Stewardship System (CLASS). In this presentation,

we discuss the transition of IASI from research to operation, its operational implementation procedures, products validation, monitoring and dissemination. This presentation will include the discussion on the ESPC system architecture involving sounding data processing and distribution for ATOVS and IASI, improvements made for data quality measurements, pipeline processing and distribution via DDS, and user timeliness requirements envisioned from the next generation of satellites. There have been

significant changes in the operational system due to system upgrades, algorithm updates, and value added data products and services. User requirements for data products and services for sounders like ATOVS and IASI would help us determine the products and services required from the next generation of sounders such as Cross-Track Infrared Sounder/ Advanced Technology Microwave Sounder (Cris/ATMS) as planned for the National Polar-orbiting Operational Environmental Satellite System

(NPOESS) program and the future missions of the EUMSAT satellites. Detailed information on the operational products and their applications are also presented.

NOAA/NESDIS UPDATES ON OPERATIONAL SOUNDING DATA PRODUCTS AND SERVICES

A.K. SharmaNOAA/NESDIS Office of Satellite Data Processing and Distribution – OSDPD

Near Real-Time IASI Data Browse

•Granule Data Monitoring (Granule data comes in ~3-minutes)

•Click Granule in the Granule Map below to Browse the image or

•Click Granule number in the table: [Show Granule Table]

AA

Near Real- Time IASI Data Browse

Data Available

Data Unavailable

04/18/2008

00104/18/2008

00204/18/2008

00304/18/2008

00404/18/2008

00504/18/2008

00604/18/2008

00704/18/200

8

008

04/18/2008

00904/18/2008

01004/18/2008

01104/18/2008

01204/18/2008

01304/18/2008

01404/18/2008

015

04/18/2008

01604/18/2008

01704/18/2008

01804/18/2008

01904/18/2008

02004/18/2008

02104/18/2008

02204/18/200

8

023

04/18/2008

02404/18/2008

02504/18/2008

02604/18/2008

02704/18/2008

02804/18/2008

02904/18/2008

030

04/18/2008

03104/18/2008

03204/18/2008

03304/18/2008

03404/18/2008

03504/18/2008

03604/18/2008

03704/18/200

8

038

04/18/2008

03904/18/2008

04004/18/2008

04104/18/2008

04204/18/2008

04304/18/2008

04404/18/2008

045

04/18/2008

04604/18/2008

04704/18/2008

04804/18/2008

04904/18/2008

05004/18/2008

05104/18/2008

05204/18/200

8

053

04/18/2008

05404/18/2008

05504/18/2008

05604/18/2008

05704/18/2008

05804/18/2008

05904/18/2008

060

04/18/2008

06104/18/2008

06204/18/2008

06304/18/2008

06404/18/2008

06504/18/2008

06604/18/2008

06704/18/200

8

068

04/18/2008

06904/18/2008

07004/18/2008

07104/18/2008

07204/18/2008

07304/18/2008

07404/18/2008

075

04/18/2008

07604/18/2008

07704/18/2008

07804/18/2008

07904/18/2008

08004/18/2008

08104/18/2008

08204/18/200

8

083

04/18/2008

08404/18/2008

08504/18/2008

08604/18/2008

08704/18/2008

08804/18/2008

08904/18/2008

090

04/18/2008

36104/18/2008

36204/18/2008

36304/18/2008

36404/18/2008

36504/17/2008

36604/17/2008

36704/17/200

8

368

04/17/2008

36904/17/2008

37004/17/2008

37104/17/2008

37204/17/2008

37304/17/2008

37404/17/2008

375

04/17/2008

37604/17/2008

37704/17/2008

37804/17/2008

37904/17/2008

38004/17/2008

38104/17/2008

38204/17/200

8

383

04/17/2008

38404/17/2008

38504/17/2008

38604/17/2008

38704/17/2008

38804/17/2008

38904/17/2008

390

04/17/2008

39104/17/2008

39204/17/2008

39304/17/2008

39404/17/2008

39504/17/2008

39604/17/2008

39704/17/200

8

398

04/17/2008

39904/17/2008

40004/17/2008

40104/17/2008

40204/17/2008

40304/17/2008

40404/17/2008

405

04/17/2008

40604/17/2008

40704/17/2008

40804/17/2008

40904/17/2008

41004/17/2008

41104/17/2008

41204/17/200

8

413

04/17/2008

41404/17/2008

41504/17/2008

41604/17/2008

41704/17/2008

41804/17/2008

41904/17/2008

420

04/17/2008

42104/17/2008

42204/17/2008

42304/17/2008

42404/17/2008

42504/17/2008

42604/17/2008

42704/17/200

8

428

04/17/2008

42904/17/2008

43004/17/2008

43104/17/2008

43204/17/2008

43304/17/2008

43404/17/2008

435

04/17/2008

43604/17/2008

43704/17/2008

43804/17/2008

43904/17/2008

44004/17/2008

44104/17/2008

44204/17/200

8

443

04/17/2008

44404/17/2008

44504/17/2008

44604/17/2008

44704/17/2008

44804/17/2008

44904/17/2008

450

Cloud Cleared RadiancesGlobal Grids Data

Retrieved Temperature and Water Vapor at ~800mb

The plot is the IASI cloud cleared radiance (CCR) at the channel 965.5cm-1. Browsing the map can check if the CCR range is reasonable.

Ch-15 Ch-1

Ch-15 Ch-1

Global Grids DataCompare retrieved Temperature with ECMWF at ~500mb

AMSU MHS

ATOVS

IASI L1C Monitoring Interface System Diagram of NOAA Retrieval Algorithm: Operational Mode

Retrieval products

Diagnostic tools

AIRS

IASI

Retrieval Code

CrIS

Sequence of Steps of the Retrieval Algorithm1) A microwave retrieval module which derives cloud liquid water

flags and microwave surface emissivity uncertainty;2) A fast eigenvector regression retrieval for temperature and

moisture that is trained using the ECMWF analysis and IASI cloudy radiances;

3) A cloud clearing module that uses a set of microwave and IR channels to produce the cloud-cleared IR radiance product and

reject those cases violating the cloud-clearing requirements;4) A fast eigenvector regression retrieval for temperature and

moisture that is trained using the ECMWF analysis and IASI cloud cleared radiances;

5) The final IR retrieval module, which uses the regression retrieval as an initial solution and produces the final version of the physical retrieval by an iterated regularized least squared

minimization.We start with the temperature retrieval, because temperature is the

most linear component of the RTA equation, followed by water vapor, ozone, etc.

All adjustments to the algorithm pertain the first 5 steps. Optimizations of the parameters involved in the following trace

gas retrievals are only minor adjustments.

Simplified flow diagram of the NOAA retrieval algorithm

Microwave Physical for T(p), q(p), LIQ(p), ε(f)

Climatological First Guess

Initial Cloud Clearing, ηj , Rccr

Improved Cloud Clearing, ηj , Rccr

Final Cloud Clearing, ηj , Rccr

Rccr Regression for Ts, ε(ν), T(p), q(p)

IR Physical Ts , ε(ν), ρ(ν)

IR Physical Ts , ε(ν), ρ(ν)

IR Physical T(p)

IR Physical T(p)

IR Physical Ts , ε(ν), ρ(ν)

IR Physical q(p)

IR Physical O3 (p)

IR Physical CO(p)

IR Physical HNO3 (p)

IR Physical CH4 (p)

IR Physical CO2 (p)

IR Physical N2 O(p)

MIT

FG

CCR

RET

Rwarm Regression for Ts, T(p), q(p)

ATOVS Weekly Vertical StatisticsSoundings ATOVS Monitoring-