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Reconciling Tropospheric Temperature Trends from the Microwave Sounding Unit
Reconciling tropospheric temperature trends from the microwave sounding unit Stephen Po-Chedley A dissertation submitted in partial fulfillment of the requirements for the degree of Master of Science University of Washington 2012 Program Authorized to Offer Degree: Department of Atmospheric Sciences University of Washington Abstract Reconciling tropospheric temperature trends from the microwave sounding unit Stephen Po-Chedley Chair of the Supervisory Committee: Professor Qiang Fu Department of Atmospheric Sciences The University of Alabama at Huntsville (UAH), Remote Sensing Systems (RSS), and the National Oceanic and Atmospheric Administration (NOAA) have constructed long- term temperature records for deep atmospheric layers using satellite microwave sounding unit (MSU) and advanced microwave sounding unit (AMSU) observations. However, these groups disagree on the magnitude of global temperature trends since 1979, including the trend for the mid-tropospheric layer (TMT). This study evaluates the selection of the MSU TMT warm target factor for the NOAA-9 satellite using five homogenized radiosonde prod- ucts as references. The analysis reveals that the UAH TMT product has a positive bias of 0.051 ± 0.031 in the warm target factor that artificially reduces the global TMT trend by an estimated 0.042 K decade−1 for 1979 - 2009. Accounting for this bias, we estimate that the global UAH TMT trend should increase from 0.038 K decade−1 to 0.080 K decade−1, effectively eliminating the trend difference between UAH and RSS and decreasing the trend difference between UAH and NOAA by 47%. This warm target factor bias directly affects the UAH lower tropospheric (TLT) product and tropospheric temperature trends derived from a combination of TMT and lower stratospheric (TLS) channels. -
Downloaded 10/04/21 02:53 AM UTC OCTOBER 2014 Z O U E T a L
2206 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 31 Connecting the Time Series of Microwave Sounding Observations from AMSU to ATMS for Long-Term Monitoring of Climate XIAOLEI ZOU Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, Florida FUZHONG WENG NOAA/NESDIS/Center for Satellite Applications and Research, College Park, Maryland H. YANG Earth System Science Interdisciplinary Center, University of Maryland, College Park, College Park, Maryland (Manuscript received 18 October 2013, in final form 8 May 2014) ABSTRACT The measurements from the Microwave Sounding Unit (MSU) and the Advanced Microwave Sounding Unit-A (AMSU-A) on board NOAA polar-orbiting satellites have been extensively utilized for detecting atmospheric temperature trend during the last several decades. After the launch of the Suomi National Polar- orbiting Partnership (Suomi-NPP) satellite on 28 October 2011, MSU and AMSU-A time series will be over- lapping with the Advanced Technology Microwave Sounder (ATMS) measurements. While ATMS inherited the central frequency and bandpass from most of AMSU-A sounding channels, its spatial resolution and noise features are, however, distinctly different from those of AMSU. In this study, the Backus–Gilbert method is used to optimally resample the ATMS data to AMSU-A fields of view (FOVs). The differences between the original and resampled ATMS data are demonstrated. By using the simultaneous nadir overpass (SNO) method, ATMS-resampled observations are collocated in space and time with AMSU-A data. The intersensor biases are then derived for each pair of ATMS–AMSU-A channels. It is shown that the brightness temperatures from ATMS now fall well within the AMSU data family after resampling and SNO cross calibration. -
Argos-3 Satellite Communication System: Implementation on the Arvor Oceanographic Profiling Floats
1902 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 32 Argos-3 Satellite Communication System: Implementation on the Arvor Oceanographic Profiling Floats XAVIER ANDRÉ Institut Français de Recherche et d’Exploitation de la Mer, Brest, France BERTRAND MOREAU Société d’Ingénierie et de Conseils en Technologies, Brest, France SERGE LE RESTE Institut Français de Recherche et d’Exploitation de la Mer, Brest, France (Manuscript received 9 December 2014, in final form 10 April 2015) ABSTRACT The scientific community observes the ocean for applications in the fields of oceanography and climate research. To recover in situ data, more than 3000 profiling floats are operated in the framework of the Argo program. Each float performs cycles between the sea surface and a depth of 2000 m. Scientific data are gathered while the float is traveling upward from the depths of the oceans and are then transmitted via a satellite communication system at the end of each cycle. During its time at the surface, mainly dedicated to transmissions, the float is vulnerable and subject to drift, which limits its use in many studies. Moreover, transmission times are becoming longer due to a trend toward high-resolution or multisensor profiles. Con- sequently, the transmission system embedded in the profiling floats had to evolve. Argos-3 is the latest generation of the Argos satellite communication system. It has been designed to allow instruments to transmit more data in a small time budget and as an alternative to Iridium, already im- plemented on profiling floats in restrictive applications. This study aims to evaluate the implementation of Argos-3 on Arvor profiling floats. -
Argos User's Manual
Argos User’s Manual © 2007-2008 CLS Last updated, October 14, 2008 Table Of Contents 1. Introduction.......................................................................................................................................... 1 2. System components ............................................................................................................................ 2 2.1 Overview ........................................................................................................................................ 2 2.2 Platforms........................................................................................................................................ 2 2.3 Satellites ........................................................................................................................................ 3 2.4 Receiving stations.......................................................................................................................... 5 2.5 Processing centers ........................................................................................................................ 5 2.6 User Services centers across the world ........................................................................................ 6 3. Location calculations ........................................................................................................................... 8 3.1 Overview ....................................................................................................................................... -
NOAA Satellite Operations Facility (NSOF)
Jason Taylor – User Services Coordinator Thomas Renkevens – SPSD Division Chief Natalia Donoho – User Services Coordinator Satellite Products and Services Division (SPSD) Office of Satellite and Product Operations (OSPO) NOAA/NESDIS/OSPO/SPSD January 14, 2016 12th Annual Symposium on New Generation Operational Environmental Satellite Systems American Meteorological Society (AMS) 96th Annual Meeting, New Orleans, LA 1 Presentation Contributors NESDIS / OSPO / SPSD @ NCWCP • Matt Seybold, GOES-R Data Ops Manager • John Paquette, Physical Scientist • Shuang Qiu, Suomi NPP Product Area Lead (PAL) • Awdesh Sharma, Satellite Operational Soundings PAL • Antonio Irving, Chief - Satellite Products Branch National Center for Weather & Climate Prediction (NCWCP) NESDIS / OSPO / MOD @ NSOF • Donna McNamara, Data Access Manager • Chris Sisko, JPSS Data Operations Manager • Carl Gliniak, Acting POES Lead • Mark Danehy, Chief – Facility Engineering Branch • John Tsui, GOES Lead NOAA Satellite Operations Facility (NSOF) 2 Presentation Outline • Overview of OSPO • Status of Satellite Operations – GOES & POES • Development Initiatives, Products & Hot Topics • Data Access and Distribution • Q&A 3 NESDIS Office of Satellite and Product Operations (OSPO) • Operates the Nation’s 15 environmental satellites: – 3 Geostationary (GOES) by NOAA – 3 Polar-Orbiting (POES) by NOAA – 6 Defense Meteorological Satellite program (DMSP) operated by NOAA – 1 OSTM Jason-2 (Ocean Surface Topography Mission) - Joint NOAA, NASA, CNES, EUMETSAT effort – 1 Suomi National Polar-orbiting -
DORIS Coordination Centre
III.4 DORIS Coordination Centre III.4 DORIS Coordination Centre Overview DORIS was developed for precise orbit determination and precise positioning on Earth. Following the inclusion of DORIS as a new technique in IERS, six groups have been participating as Analysis Centers: CNES/ SOD, GRGS, and IGN in France, UT/CSR in the USA, DUT in the Netherlands and MCC in Russia. The first four groups have submit- ted regular results to IERS either for polar motion determination or for tracking stations coordinates and velocities. Other groups are still developing their processing capabilities. Two IERS Data Centers have been providing the scientific community with DORIS measure- ments for several years: NASA/CDDIS and IGN/LAREG. In 1999, following the recent IERS reorganization, it has been decided at the IAG General Assembly (Birmingham, UK, August 1999) to create a DORIS Pilot Experiment. Such a Pilot Experi- ment would give time to all groups to coordinate and improve their operationability in order to create on the long term an International DORIS Service (IDS). In the future, this scientific service would structure the DORIS community in order to provide scientific prod- ucts for a broad range of potential users, starting by the IERS itself. This is done as common activity of the IERS and the IAG/CSTG (Commission on International Coordination of Space Techniques for Geodesy and Geodynamics of the International Association of Geodesy ). This is very similar to what is done for GPS by the IGS, or for VLBI by the IVS or for SLR and LLR by the ILRS. The International DORIS For the DORIS Pilot Experiment an international Call for Participa- Pilot Experiment tion has been issued in September 1999. -
Guide to Data Collection and Location Services Using Service Argos Was Prepared by Dr
Intergovernmental Oceanographic World Commission of UNESCO Meteorological Organization DATA BUOY COOPERATION PANEL GUIDE TO DATA COLLECTION AND LOCATION SERVICES USING ARGOS DBCP Technical Document No. 3 - 1 - [this page left blank intentionally] - 2 - Intergovernmental Oceanographic World Commission of UNESCO Meteorological Organization DATA BUOY CO-OPERATION PANEL GUIDE TO DATA COLLECTION AND LOCATION SERVICES USING ARGOS DBCP Technical Document No. 3 REVISION 1 2011 - 3 - CONTENTS PREFACE.........................................................................................................................................5 BACKGROUND TO THIS DOCUMENT........................................................................................5 1. INTRODUCTION ...................................................................................................................6 1.1. OVERVIEW OF THE SYSTEM....................................................................................................... 6 1.2. ARGOS FOR METEOROLOGY AND OCEANOGRAPHY .................................................................... 7 1.3. GEOPHYSICAL VARIABLES....................................................................................................... 10 1.4. INTERNATIONAL COORDINATION THROUGH JCOMM – ARGO, DATA BUOY COOPERATION PANEL, SHIP OBSERVATIONS TEAM AND OCEANSITES........................................................................ 12 2. DRIFTING BUOY HARDWARE ........................................................................................ -
NOAA 2018 Update to the Ocean Studies Board
Argos Data Collection and location System (Argos DCS) Scott Rogerson National Environmental Satellite, Data, and Information Service (NESDIS) National Oceanic and Atmospheric Administration (NOAA) September 10, 2018 September 10, 2018 Department of Commerce // National Oceanic and Atmospheric Administration // 1 Argos DCS Overview • Continuous operations since 1978. • Provides global space-based coverage on polar-orbiting satellites. • USA-International public-private partnership: • Government provides space segment • French Space Agency (CNES) provides Argos instruments. • Six Argos instruments in orbit today. • Four new generation Argos instruments from CNES ready to launch. • Global ground system network of 60+ receive stations. • Two global processing centers (one in Europe & one in USA) provides data processing and customer interface. Department of Commerce // National Oceanic and Atmospheric Administration // 2 18,000 Platforms – 2,000 Users – 100 Countries Avian Wildlife Drifting Buoy Marine Wildlife Fixed Station Terrestrial Wildlife Moored Buoy Vessel Sub-Float Department of Commerce // National Oceanic and Atmospheric Administration // 3 Key Advantages of Argos DCS • Transmitters are very small (as light as a few grams) & require low power. • Highly reliable. • Support long term monitoring programs. • Doppler shift calculations can be used to independently locate platforms anywhere on Earth. • Rapid refresh: – Currently six satellite constellation – Global ground system network of 60+ stations – Data timeliness of 30-60 minutes – 24x7 data availability • Operates on a non-interference basis with commercial systems. Department of Commerce // National Oceanic and Atmospheric Administration // 4 How the Argos DCS Works • Users complete system use agreement and deploy platforms. • Platforms transmit to satellites as they pass overhead. • Satellites transmit data to ground system stations. • Data sent to ground processing centers and then delivered to users. -
CGMS-39, NOAA-WP-19 Prepared by C.-Z
CGMS-39, NOAA-WP-19 Prepared by C.-Z. Zou and L. Wang Agenda Item: xxx Discussed in xxx NOAA's Stratospheric Temperature Climate Data Record Derived from Recalibrated Stratospheric Sounding Unit Observations In response to CGMS Recommendation 38.13 Summary of the Working Paper NOAA/NESDIS has generated a 27-year (1978-2006) stratospheric temperature data record from Stratospheric Sounding Unit (SSU) observations for climate trend and variability detection. The dataset includes gridded global layer temperatures of mid-stratosphere, upper-stratosphere, and top- stratosphere. Calibration algorithms for developing the data record include corrections of gas leaking problem in the SSU instrument CO2 cells, variation of the atmospheric CO2 concentration, incident angle effect, diurnal drift effect, and Earth-location dependent residual inter-satellite biases. The products have a grid resolution of 2.50 latitude by 2.50 longitude and both monthly and pentad data are available for seamless climate monitoring. This is the first set of well-documented and well-calibrated global gridded dataset available to the climate community for long-term stratospheric temperature monitoring and investigation and for validating climate model simulations of the stratospheric climate change. For 1979-2006, the dataset had a global mean stratospheric temperature trend around -0.93 to -1.24 K/decade. Spatial trend pattern analyses indicated that this cooling occurred globally with larger cooling over the tropical stratosphere. CGMS-39, NOAA-WP-19 NOAA's Stratospheric Temperature Climate Data Record Derived from Recalibrated Stratospheric Sounding Unit Observations 1 INTRODUCTION The stratosphere has been recognized as an important component in the global change scenario. -
GES DISC DAAC Data Guide: Microwave Sounding Unit Daily Deep Layer Temperatures and Oceanic Precipitation Data Set Guide Document
GES DISC DAAC Data Guide: Microwave Sounding Unit Daily Deep Layer Temperatures and Oceanic Precipitation Data Set Guide Document Summary: This document supports the Daily Deep Layer Temperatures and Oceanic Precipitation data sets derived from the Microwave Sounding Unit (MSU) flown aboard the NOAA polar orbiting satellites. The NOAA satellites contributing to these data sets are, in order of their launch, TIROS-N, NOAA-6, NOAA-7, NOAA- 9, NOAA-10, NOAA-11, and NOAA-12. NOAA-8 data were not used due to poor data quality. Table of Contents: 1 Data Set Overview 2 Investigator(s) 3 Theory of Measurements 4 Equipment 5 Data Acquisition Methods 6 Observations 7 Data Description 8 Data Organization 9 Data Manipulations 10 Errors 11 Notes 12 Application of the Data Set 13 Future Modifications and Plans 14 Software 15 Data Access 16 Output Products and Availability 17 References 18 Glossary of Terms 19 List of Acronyms 20 Document Information 1. Data Set Overview: Data Set Identification: Microwave Sounding Unit Daily Deep Layer Temperatures and Oceanic Precipitation Data Set Data Set Introduction: The temperature data set contains the Limb 93 correction and is stored in a native binary format as well as in the Hierarchical Data Format (HDF). The NOAA satellites contributing to these data sets are, in order of their launch, TIROS-N, NOAA-6, NOAA-7, NOAA-9, NOAA-10, NOAA-11, and NOAA-12. NOAA-8 data were not used due to poor data quality. The data set period of record is January 1979- December 1993 for the temperatures, and 1979 thru May 1994 for oceanic precipitation. -
TOPEX/POSEIDON Satellite.....…………………….………………
M I S S I O N T O P L A N E T E A R T H TOPEX/POSEIDON NASA/CNES PRESS KIT AUGUST, 1992 PUBLIC AFFAIRS CONTACTS Brian Dunbar Headquarters, Washington, D.C. (Phone: 202/358-0873) Mary Hardin Jet Propulsion Laboratory, Pasadena, Calif. (Phone: 818/354-5011) CONTENTS General Release.......................................………………………......................1 Mission Overview And Science Objectives...…………..................................3 Satellite Tracking.....................................…………………………..………..4 TOPEX/POSEIDON Satellite.....…………………….………………...........5 Science Instruments And Spacecraft......................……..…………..............6 Mission Phases......................................…………………………………......8 Mission Timeline....................................……………………………….......9 Spacecraft Specifics..................................……………………….……….10 U.S.-French Cooperation...................………………………..…...............10 Mission Management.................................………………………….........11 RELEASE 92-126 U.S., FRANCE SATELLITE TO STUDY OCEANS AND CLIMATE On Aug. 10, the United States and France will undertake a mission to help provide a new understanding of Earth's environment by determining how the global system of the Earth's oceanic currents influence climate. The means to this end is the TOPEX/POSEIDON satellite, a joint mission of NASA and France’s space agency, the Centre National dUEtudes Spatiales (CNES). "TOPEX/POSEIDON is an investment in our future," said NASA's Program Scientist Dr. William Patzert. "Without TOPEX/POSEIDON, -
ARGOS Instruments in Operations
System Improvements DBCP 28 Meeting - Fremantle October 2012 Space Agency collaboration 4 x DCS-2 2 x DCS-4 11 x DCS-1 5 x DCS-3 (+ 1 for ADEOS II) ( + 4 to be decided) ARGOS Instruments in Operations ARGOS 1 ARGOS 2 ARGOS 3 ARGOS 4 NOAA I NOAA J NOAA K NOAA L NOAA M NOAA N NOAA N’ Free Flyer JPSS2 Juillet 1993 Déc. 1994 05/1998 09/2000 06/2002 05/2005 2009 2016 USA / NOAA ARGOS 3 ARGOS 3 METOP-A METOP-B METOP-C EPS SG 10/2006 2012 2016 EUROPE / EUMETSAT Average constellation age: 7 years ARGOS 3 SARAL 2012 INDIA / ISRO Argos‐3 satellites – Metop A • Launched on October 19th 2006 • Operational downlink – NOAA 19 • Launched on Feb 6th 2009 • Downlink stopped on Friday 13/11/2009 – Metop B • Launched on Sept 17th 2012 • Same orbit than MetOp A but ½ orbit later. – Saral (A3 + AltiKa = Altimetry in Ka band) th • Launch planned for December 12 2012 • Download of 100’ orbit in real time – Metop C: • Launch planned for October: 2016 • Metop A replacement Metop B Launch September 17th 2012 Page 4 Argos system status N19 N18 / 2.48’/m MetOp A 5 x Argos-2 2 x Argos-3 N16 / 3.92’/m Saral 1800 0600 Local time Local time N15 N17 / -4.28’/m MetOp B 2012 : Free Flyer 5 1200 local sun time SARAL & MetOp-B launch Argos‐4 features • Uplink: – Low data rate @ 400 bps / 401.650 MHz +/- 30 KHz – Very low data rate PM @ 124 bps (200mW) - CV – Medium and High Data Rate GMSK @ 1200/4800 bps (3 watts) - TC – Frequency band: 640 KHz at satellite level (8 freq.