Space Weather from the SEM-N Sensor Suite for Operational Use W.F. Denig 1, P. Purcell 1,2 & C.D. Reimer 3 1 NOAA National Geophysical Data Center 2 CSU.

Slides:



Advertisements
Similar presentations
Abstract Real-time images of Earths space environment from NASAs IMAGE satellite will soon be available on the NOAA Space Environment Center Web site.
Advertisements

Space Weather in CMA Xiaonong Shen Deputy Administrator China Meteorological Administration 17 May 2011 WMO Cg-XVI Side Event Global Preparedness for Space.
The challenges and problems in measuring energetic electron precipitation into the atmosphere. Mark A. Clilverd British Antarctic Survey, Cambridge, United.
National Polar-orbiting Operational Environmental Satellite System (NPOESS) Space Environment Sensing Capabilities Lt Col Mike Bonadonna USAF User Liaison.
18-OCT-2005 Lyndon B. Johnson Space Center space radiation analysis group 1 Operational Aspects of Space Radiation Analysis October 18, 2005 Mark Weyland.
ACTIVITY ON THE SUN: Prominences Sunspots Solar Flares CME’s – Coronal Mass Ejections Solar Wind Space Weather.
Algorithm Working Group Space Weather Team Activities and Plans S. Hill, H. Singer, T. Onsager, R. Viereck, D. Biesecker, C. Balch – NOAA/NWS/NCEP/SEC.
ESA SSA Programme Objective:
Propagation Index and Short Wave Communications Rodney Wolfe N3XG.
Space Weather. Coronal loops Intense magnetic field lines trap plasma main_TRACE_loop_arcade_lg.jpg.
Future Plans for Space Weather Observations – U.S. NOAA Perspective Terry Onsager National Oceanic and Atmospheric Administration Space Weather Prediction.
Space Weather Causes and Consequences An introduction to Space Weather What is it? Where does it come from? Who is impacted? Rodney Viereck NOAA Space.
Passive Microwave Rain Rate Remote Sensing Christopher D. Elvidge, Ph.D. NOAA-NESDIS National Geophysical Data Center E/GC2 325 Broadway, Boulder, Colorado.
Aerospace Environment ASEN-5335 Instructor: Prof. Xinlin Li (pronounce: Shinlyn Lee) Contact info:
From Geo- to Heliophysical Year: Results of CORONAS-F Space Mission International Conference «50 Years of International Geophysical Year and Electronic.
PHOEBUS* on LISA: A Proposal for Solar Physics on LISA INFN-SPAZIO/2 Riunione sulle prospettive della Fisica Astroparticellare nello spazio LNF, 16 Febbraio.
NOAA Space Environment Center The Status of Solar Cycle 23 Joe Kunches Chief, Space Weather Operations NOAA Space Environment Center Boulder, Colorado.
NGDC’s Solar and Space Weather Program Eric A. Kihn and William Denig.
NOAA Space Environmental Data Paper AMS W.F. Denig National Geophysical Data Center Boulder, CO Monday, 03 Feb 14 / 2:00 PM.
Remote Sensing Space-based Earth exploration and planetary exploration began with the International Geophysical Year (IGY) which was also the beginning.
New Operational Algorithms for Charged Particle Data from Low-Altitude Polar-Orbiting Satellites J. L. Machol 1,2 *, J.C. Green 1, J.V. Rodriguez 3,4,
Energetic Particles in the Atmosphere J.M. Wissing and M.-B. Kallenrode.
Sponge: List the six layers of the Earth.. Atmosphere A mixture of gases: N 2 78% O 2 21% Ar0.9% CO %
Space Weather Major sources of space weather ● Solar wind – a stream of plasma consisting of high energy charged particles released from the upper atmosphere.
Prospects for Improved Global Mapping of Development Using VIIRS Data Chris Elvidge Earth Observation Group NOAA-NESDIS National Geophysical Data Center.
Space Weather Aviation Operational Needs
Solar Weather and Tropical Cyclone Activity Abstract Worldwide tropical cyclone energy and frequency data was obtained from the Unisys Weather database.
Space Weather: What is it? How Will it Affect You? An introduction to Space Weather What is it? Where does it come from? What does it do? Rodney Viereck.
NOAA Operational Space Env Monitoring Paper J1.2 - AMS W.F. Denig 1 & P Mulligan 2 1 National Geophysical Data Center 2 Office of Systems Development Wednesday,
Space Weather: Magnetosphere-Ionosphere Coupling 14 November 2011 William J. Burke Air Force Research Laboratory/Space Vehicles Directorate Boston College.
K9LA Vancouver 2003 Disturbances to Propagation Carl Luetzelschwab K9LA CQ DX?Where’d everybody go?
Understand band condition information Use a propagation gadget
Localized Thermospheric Energy Deposition Observed by DMSP Spacecraft D. J. Knipp 1,2, 1 Unversity of Colorado, Boulder, CO, USA 2 High Altitude Observatory,
High Data Volume Transfer Issues at NOAA Christopher D. Elvidge Earth Observation Group National Oceanic and Atmospheric Administration National Geophysical.
Lesson 2 Space Environment & Orbital Mechanics A537 SPACE ORIENTATION.
In Situ Measurements of Auroral Acceleration Regions Wu Tong
The ionosphere of Mars never looked like this before Paul Withers Boston University Space Physics Group meeting, University of Michigan.
Comparison of Magnesium II Core-to-Wing Ratio Measurements J. Machol 1,2*, M. Snow 3, R. Viereck 4, M. Weber 5, E. Richard 3, L. Puga 4 1 NOAA/National.
Background source: Better modeling through MATLAB: Connecting the auroral oval and the convection reversal boundary.
Contact Information: Dr. Howard J. Singer, Chief Research and Development Division NOAA Space Environment Center 325 Broadway Boulder, CO
Space Environment SSE-120 Please type in your questions and raise your hand so we can answer it during class.
Collective Security in Space: Asian Perspective Chinese Society of Astronautics To Develop Space Peacefully for Benefits of Human beings Yang Junhua Vice.
REMOTE SENSING IN EARTH & SPACE SCIENCE
An introduction to our active ionosphere begin
AFOSR SPACE SCIENCES 15 Jul 05 Major David L. Byers Program Manager AFOSR Air Force Research Laboratory Distribution C: Distribution authorized to U.S.
SOLSTICE II -- Magnesium II M. Snow 1*, J. Machol 2,3, R. Viereck 4, M. Weber 5, E. Richard 1 1 Laboratory for Atmospheric and Space Physics, University.
Topics in Space Weather Earth Atmosphere & Ionosphere
11 Space Weather Services in Support of Global Air Navigation – Role of the Neutron Monitor Doug Biesecker Bob Rutledge NOAA Space Weather Prediction Center.
Contact Information: Dr. Howard J. Singer, Chief Research and Development Division NOAA Space Environment Center 325 Broadway Boulder, CO
Preliminary Presentation By Matthew Lewis 2 nd December 2005.
CRRES observations indicate an abrupt increase in radiation belt fluxes corresponding to the arrival of a solar wind shock. The processes(s) which accelerate.
What does it cover? This session addresses “Why?”, “When?”, and “What Sensors?” will be on GOES- R, and presents examples of what to expect. If is a look.
What is a geomagnetic storm? A very efficient exchange of energy from the solar wind into the space environment surrounding Earth; These storms result.
Bringing 93,000,000 Miles to 40,000 Feet: Space Weather & Aviation An introduction to Space Weather What is it? Where does it come from? What does it do?
National Oceanic and Atmospheric Administration, April 2015 Coordination Group for Meteorological Satellites - CGMS NOAA: Space Weather Overview Presented.
Radio Wave Propagation
KMA Space Weather Service Presented to CGMS-44 on Working Group SWTT.
Gyeongbok Jo 1, Jongdae Sohn 2, KyeongWook Min 2, Yu Yi 1, Suk-bin Kang 2 1 Chungnam National University 2 Korea Advanced Institute of Science.
When Lower Atmosphere Waves Invade the Upper Atmosphere
JMA Report on Satellite-based Space Weather Activities in Japan
2016 Solar Storms with NASA/NOAA GOES-R Satellite Primed to Support Space Weather Predictive Capabilities On 20 December 2016 Earth encountered a stream.
Connecting Earth to Space: NASA Heliophysics Provides Data on how Space Weather Impacts Earth’s Environment Using NASA Van Allen Probes mission data, researchers.
Scientists demonstrate a new Solar Energetic Particle warning technique using K-COR ground coronagraph data A Heliophysics science publication using ESA/NASA.
The Atmosphere.
THEMIS and Space Weather
R. Bucˇık , K. Kudela and S. N. Kuznetsov
Solar Activity and Space Weather
Earth’s Ionosphere Lecture 13
BU Astronomy Symposium
The Centre of the Solar System Earth Science 11
Presentation transcript:

Space Weather from the SEM-N Sensor Suite for Operational Use W.F. Denig 1, P. Purcell 1,2 & C.D. Reimer 3 1 NOAA National Geophysical Data Center 2 CSU Cooperative Institute for Research in the Atmosphere 3 SMC Defense Meteorological Satellite Program Systems Group 91 st Annual Meeting – AMS

2 AMS, Jan 2011 REFERENCE ONLY NOT PRESENTED ABSTRACT New Operational SWx Sensor SPACE WEATHER FROM THE SPACE ENVIRONMENT MONITOR-NEXT (SEM-N) SENSOR SUITE FOR OPERATIONAL USE W. F. Denig 1, P. Purcell 1,2 and C. D. Reimer 3 1 NOAA/National Geophysical Data Center (NGDC), 325 Broadway, Boulder, CO U.S.A. 2 Cooperative Institute for Research in the Atmosphere (CIRA), Colorado State University, Fort Collins, CO U.S.A. 3 SMC Defense Meteorological Satellite Program Systems Group, Los Angeles AFB, CA U.S.A. Monitoring the near-earth environment is essential for protection of space assets and their capabilities from extremes in space weather. Particle radiation impacts military communication, navigation, aviation and spacecraft operations, as these systems may be vulnerable to high energy particles. Using in situ high energy particle sensors allow modeling of the earth environmental response to solar activity and provide space weather predictions for satellite protection and management - from possible planning of satellite maneuvers to shutting down on-board systems and sensors to avoid damage. Additionally, knowledge of the particle environment constrains engineering design of satellites for survivability and allows sensor data to be corrected for contamination by particle fluxes. Synergism with UV and V is remote sensing of atmospheric disturbances (e.g. aurora) allows calibration checks of the electro-optical sensors and independent input to atmospheric models. The Defense Weather Satellite System (DWSS), the follow-on DoD program to the National Polar-orbiting Operational Environmental Satellite System (NPOESS), will fly the Space Environment Monitor – Next (SEM-N) for detection of such space particles. SEM-N is a suite of sensors based on heritage particle sensors flying on the Defense Meteorological Satellite Program (DMSP) and the Polar Operational Environmental Satellite (POES) system for the DoD and DOC/NOAA, respectively, and on NASA planetary research missions. The sensor suite will provide space particle data continuity for DMSP and POES. This paper will focus on the performance capabilities of SEM-N for space weather forecasting, for early warning to protect military assets in space and on the ground, and to provide effective operational planning.

3 AMS, Jan 2011 USAF Polar Weather Satellite Defense Weather Satellite System (DWSS) Follow-on Program to DMSP Defense Meteorological Satellite Program Sun-synchronous orbit at 840 km / 98.7 o  Single satellite 17:30 LTAN Complements 13:30 LTAN Complements 21:30 LTAN Space Environment EDRs  Auroral Boundary (AB)  Auroral Energy Deposition (AED)  Supra-thermal to Auroral Charged Part. (SACP)  Medium-energy Charged Particles (MECP)  Energetic Ions (EI) Space Environment Monitor – Next (SEM-N)  SSJ5-N – Electrostatic Analyzer  EPM – Energetic Particle Monitor  HES – High Energy Sensor LTAN – Local Time of Ascending Node EDR – Environmental Data Record JPSS – Joint Polar Satellite System (NOAA) Photo Credit: Lockheed Martin Auroral over Greenland - DMSP

4 AMS, Jan 2011 SEM-N Hardware Space Environment Monitor - Next Sensor Suite Characteristics: SSJ5-N – Electro-Static Analyzer Measures electrons & protons Energy range: 30 eV – 30 keV Total field of view: 90 o x 4 o Heritage: DMSP SSJ4/5 EPM – Particle Spectrometer Measures electrons & protons Electron range: 30 keV to <1 MeV Proton range: 30 keV to 10 MeV Some ion mass discrimination Time-of-flight capabilities Heritage: NASA Messenger HES – High Energy (Ion) Sensor Shielded solid-state detectors Proton range: 10 MeV to >140 MeV Heritage: POES MEPED SEM-N H/W under development by the JHU Applied Physics Laboratory. First DWSS launch is in ~2018. Special Sensor J5 (SSJ5-N) Energetic Particle Monitor (EPM) High Energy Sensor (HES)

5 AMS, Jan 2011 SEM-N Algorithms Space Environment Monitor - Next MECP Data Flow Diagram (Logical View) The NOAA National Geophysical Data Center (NGDC) is responsible for the development of the SEM-N ground-processing algorithms (science codes). Algorithm Theoretical Basis Documents (ATBDs) & code flow diagrams under development (post-PDR maturity). Program Office is considering the use of the Algorithm Development Language (ADL) for the operational code.

6 AMS, Jan 2011 SEM-N Traceability Chart Sensor to System Impacts Slide provided by Tom Sotirelis (JHU/APL)

7 AMS, Jan hour auroral composite from DMSP OLS Historical operational methods used white-light imagery data from the DMSP Operational Linescan System (see Meng [1976]). Auroral boundary identification Monitoring has now transitioned to a particle-based approach using the DMSP SSJ series of sensors (see Gussenhoven et al. [1987]). Alternative approaches include ultra-violet (UV) imaging of the auroral zone. ABNPAB Environmental Data Record Monitoring the Auroral Boundary DMSP polar pass using the SSJ AB = Auroral Boundary NP = ~North Pole Credit: Elvidge, NOAA/NGDC Credit: Denig, AFRL

8 AMS, Jan 2011 Environmental Data Record Auroral Energy Deposition Used to create a synthetic auroral oval map. Current methodology developed by Dave Evans (see Foster et al. [1986]). Alternative approaches under consideration. Calculates the total hemispheric power input from auroral electron precipitation (see Emery et al. [2008]). Credit: Unknown

9 AMS, Jan 2011 Environmental Data Record Supra-thermal to Auroral Energy Particles Energetic charged particle data used operationally to determine the equatorial aurora boundary and auroral energy deposition. Data from current operational sensors used in many scientific investigations including simple case studies and in multi-sensor investigations (White Paper submitted to the NRC Decadal Survey). DMSP SSJ5 Credit: Newell, JHU/APL Credit: Amptek

10 AMS, Jan 2011 Environmental Data Record Medium Energy Charged Particles Used to monitor the space radiation environment. Precipitating energetic protons and electrons within energy ranges up to several MeV are located at high latitudes and within the region of the South Atlantic Anomaly (SAA). Particle deposition can degrade radio communication can disrupt the proper operation of satellite systems and, when intensities are sufficiently high, increase the radiation dose to astronauts in space. Image Courtesy of ESA SEM MEPS Electron Data Channel

11 AMS, Jan 2011 Environmental Data Record Energetic Ions Measurement of very energetic protons, mostly of solar origin. Geo-effective energetic protons (>10 MeV) produce enhanced levels of ionization at altitudes below 100 km. Short wave radio waves at relatively high frequencies are absorbed by the increased ionospheric densities causing a complete blackout of radio communications (Polar Cap Absorption [PCA] event). Lower frequency waves that would normally reflect off the low altitude ( D- or E-region) ionospheric layers now do so at lower altitudes thereby changing dramatically their propagation paths. PCA events are particularly devastating to radio communications because they can last for days depending on the sizes and locations of the magnetic disturbances on the Sun that produce them. The commercial airline industry requires knowledge of possible PCA events for operational planning for polar routes.

12 AMS, Jan 2011 Current Launch Schedule 1 USAF/NOAA/Europe Polar Programs 1 After Mary Kicza – National Academies Committee on Earth Science, 07 July 2010

13 AMS, Jan 2011 Summary New Operational SWx Sensor (SEM-N) Space Environment Monitor – Next (SEM-N) is the follow- on operational space weather sensor for the DoD / NOAA Sensor under development for a 2018 launch – some capability improvements over current operational sensors Various SEM-N data products will be available for the SWx operational communities

14 AMS, Jan 2011 QUESTIONS?