Tom Woods LASP/CU tom.woods@lasp.colorado.edu LASP/CU: Frank Eparvier, Don Woodraska, Gary Rottman HAO/NCAR: Stan Solomon, Ray Roble, Giuliana de Toma NRL: Judith Lean SpaceWx: Kent Tobiska GI/UAF: Scott Bailey TIMED SEE SORCE SWG July 2002 - 1 TIMED Mission ♦ TIMED primary science goals are to understand : • energy transfer into and out of the Mesosphere and Lower Thermosphere/Ionosphere (MLTI) region of the Earth's atmosphere, and • basic structure (i.e., pressure, temperature, and winds) of the MLTI region between 60 and 180 km ♦ ♦ TIMED launched on Dec. 7, 2001 Normal operations began on Jan. 22, 2002 Thermosphere Ionosphere Mesosphere Energetics Dynamics TIMED SEE SORCE SWG July 2002 - 2 TIMED Instruments Overview ♦ All instruments measure atmospheric composition, density, and temperature (even SEE using solar occultations) ♦ SABER • Cooling-IR ♦ TIDI • Winds-Visible ♦ GUVI • Aurora-FUV ♦ SEE • Solar-EUV TIMED SEE SORCE SWG July 2002 - 3 Before TIMED ♦ Some previous missions have also studied the MLTI region: • Atmospheric Explorer (AE-C, AE-E) - 1973-1981: composition, winds, plasma, solar EUV • Solar Mesospheric Explorer (SME) - 1981-1989: composition, solar UV • Upper Atmosphere Research Satellite (UARS) - 1991-present: composition, winds, solar UV, plasma • Student Nitric Oxide Explorer (SNOE) - 1998-present: NO, aurora, solar XUV ♦ TIMED improvements include: • • • • • • ♦ Measurement of IR cooling by SABER Measurement of CO 2 by SABER Four telescopes for measuring winds by TIDI GUVI has 25 km spatial resolution for aurora dynamics Better spectral resolution and coverage for solar EUV irradiance by SEE Use of improved technology / calibrations by all instruments AIM SMEX is future explorer that will focus on PMCs TIMED SEE SORCE SWG July 2002 - 4 Solar EUV Experiment (SEE) Science Objectives ♦ Study the solar radiation input to the mesosphere, lower thermosphere, and ionosphere (MLTI) • • Accurately determine the solar vacuum ultraviolet (VUV: below 200 nm) irradiance Study the impact of solar changes on Earth’s upper atmosphere utilizing atmospheric models Photochemistry Examples Heating Atmospheric Layers Creation of Ionosphere + O → O + e ν EUV − XUV Ozone Creation O2 → O → O 3 ν FUV Thermosphere EUV-FUV 90 Mesosphere O2 Ozone Destruction O3 → O 2 + O ν MUV Solar Input FUV 50 Stratosphere 20 km Troposphere 200 MUV NUV-Vis-IR 1000 °K 250 Temperature PLUS other effects on Climate Surface Oceans Temperature (°K) QuickTime™ and a Photo - JPEG decompressor are needed to see this picture. Corona SOHO EIT He II 30.4 nm 500,000 15,000 Transition Region Chromosphere 6,000 Photosphere 4,000 ♦ Improve the understanding of solar VUV variability - XUV EUV Identify and quantify the sources of solar VUV variability Develop better models of the solar VUV irradiance FUV TIMED SEE SORCE SWG July 2002 - 5 EGS Measures the Solar EUV-FUV ♦ EUV Grating Spectrograph (EGS) • Normal Incidence, 1/4 m Rowland Circle Spectrograph - 26-195 nm range − ∆λ = 0.4 nm - (0.167 nm/pixel) EUV FUV Example EGS Measurement • Redundant channel used weekly for tracking degradation Lyman-α Filter Calibration accuracy < 10% Measurement precision < 2% Charge Amp 64 x 1024 CODACON Detector Flat Field (Hg) Lamp Vacuum Door Detector HVPS Slit Selector TIMED SEE Optical Cube Solar Aspect Sensor (SAS) SORCE SWG July 2002 - 6 XPS Measures the Solar XUV Calibration accuracy < 20% Measurement precision < 1% ♦ XUV Photometer System (XPS) • 8 XUV Si photodiodes - 0.1-27 nm − ∆λ ~ 7 nm Example XPS Measurement • 1 Lyman-α (121.6 nm) photometer • 3 bare (Vis) Si photodiodes - measure FS filter transmission • 8 position filter wheel - 1 clear aperture per diode - 2 fused silica filters per diode - 5 blank apertures per diode 12 PhotoDiode Detectors Amplifiers & VFCs Interface Board Filter Wheel Mechanism Filter Wheel Control Electronics LVPS XPS - Generic Channel Interface Filter Wheel (inside purge cover) Photodiode Electronics Section +28V XPS To MU Solar Radiation Filter Wheel Control Electronics TIMED SEE SORCE SWG July 2002 - 7 SEE is Healthy and Working Well ♦ Obtain ~100 solar measurements per week • Each solar measurement is ~20 10-second integrations • A solar observation is performed each orbit ♦ Perform ~3 EGS detector flatfield calibrations per week SEE has been in normal operations (daily measurements) since Jan. 22, 2002 • On-board Hg lamp is flatfield source ♦ ♦ ♦ Make redundant channel (calibration) solar observation once a week for tracking degradation Occultation experiments are possible for about 2 weeks per yaw around period Plan an underflight rocket calibration once a year 12 hr Example for SEE Observations Detector Flatfields Solar Observations • First calibration rocket was launched on Feb. 8, 2002 TIMED SEE SORCE SWG July 2002 - 8 Status of SEE Data Processing ♦ SEE data products are being generated daily • Version 4 is current version ♦ SEE XPS Level 2 data products are available now • SEE data and S/W: http://lasp.colorado.edu/see/ - daily average, instrument resolution (~7 nm), atmospheric absorption corrected, degradation corrected, normalized to 1 AU - NetCDF format: use IDL read_netcdf.pro to read SEE data products - Quick-look: use IDL plotxps_ts.pro to plot time series for 1 channel ♦ SEE EGS data products should be available in late July - EGS re-processing (version 5) includes underflight rocket calibration results, in-flight FOV and 2nd order maps, and flatfield lamp degradation - EGS irradiance results shown today are mostly version 4 data, which don’t have the latest calibrations incorporated yet TIMED SEE SORCE SWG July 2002 - 9 XPS Validations with SNOE: 2-7 nm 2-7 nm SNOE Rocket SNOE 2-7 nm irradiances are higher than SEE 2-7 nm values by ~30%. SEE However, earlier SNOE 2-7 nm measurements, as compared to F10.7, are more consistent with SEE. TIMED SEE SORCE SWG July 2002 - 10 XPS Validations with SNOE: 17-20 nm 17-20 nm SNOE Rocket SNOE 17-20 nm irradiances agree very well with the SEE 17-20 nm values. SEE SEE confirms the important SNOE result that the solar XUV irradiance below 20 nm is about 4 times more than the historical values [Hinteregger et al., 1981]. TIMED SEE SORCE SWG July 2002 - 11 Atmosphere Confirms Higher XUV Irradiances Modeling of TIMED GUVI Dayglow [Stan Solomon, Spring AGU 2002] Model with Reference XUV Model with SEE XUV TIMED GUVI Measurement Daily average, near equator, SZA ~ 50°, F10.7=257 TIMED SEE SORCE SWG July 2002 - 12 EGS Validation with UARS: 120-195 nm ♦ Initial comparison showed differences of ~30% EGS Version 4 • ~20% was systematic offset - thought to be due to pre-launch degradation of SEE EGS • ~10% was reduced by including new calibration parameters (FOV, degradation) ♦ SEE EGS Version 5 has minor differences between SOLSTICE • Feb. 2002 rocket calibration confirms the UARS SOLSTICE irradiance levels • EGS Version 5 data include the latest parameters for FOV, 2nd Order, and rocket/SOLSTICE calibration TIMED SEE EGS Version 5 EGS Version 4 SORCE SWG July 2002 - 13 TIMED-SORCE Validation Plans ♦ SORCE XPS • 0-35 nm overlap between SORCE XPS and SEE XPS/EGS ♦ SORCE SOLSTICE - FUV (G channel) • 115-195 nm overlap between SOLSTICE and EGS ♦ ♦ ♦ Weekly redundant channel measurements by both SORCE and SEE instruments Annual rocket calibration experiments for SEE Important solar Lyman-α irradiance will be well measured by SORCE and SEE • 6 different measurements: SEE XPS, SEE EGS x 2, SORCE XPS, SORCE SOLSTICE x 2 • 3 different measurements from annual rocket experiment TIMED SEE SORCE SWG July 2002 - 14 TIMED Fills the “EUV Hole” Satellite Measurements of the Daily Solar Spectral Irradiance SORCE SBUV NPOES UARS SME SOLRAD EUV Hole SOHO GOES XRS TIMED SEE SDO GOES AE TIMED AEROS Future FUV Hole ? SNOE SORCE SWG July 2002 - 15 TIMED Mission Began at Solar Maximum ♦ ♦ TIMED was just in time for solar maximum Solar cycle 23 may already be dropping towards solar minimum conditions “EUV Hole” Has Been Filled Prior to the SOHO measurements, the solar EUV/XUV irradiances had not been measured on a daily basis since 1980 by the AE-E satellite. Dick Donnelly had dubbed this problem as the “EUV Hole”. The TIMED SEE instrument is the first instrument to measure the solar irradiance over the full EUV spectral range (0-120 nm) on a daily basis and thus ending the EUV Hole. SOHO EIT He II 30.4 nm Solar Min Max XUV During Solar Cycle 23 TIMED SEE SORCE SWG July 2002 - 16 SEE Measures Solar Variability XPS Time Series Version 4 Data XPS data include lots of X-ray flares EGS Time Series Current V4 EGS data still require several calibration corrections Updated FOV Maps Degradation Correction Rocket Calibration Update These corrections have been updated for the XPS Version 4 data, but these corrections, being more complicated for EGS, will be included in EGS Version 5. TIMED SEE SORCE SWG July 2002 - 17 Special Study is Large Flare on April 21 TRACE 1 hour later • X1.5 class flare at ~2 UT • C8 class flare at ~18 UT LOG Scale SOHO EIT X-rays and coronal lines show most variation • X-ray increased by factor of 8 • Longer wavelengths enhanced much less (< 40%) TIMED SEE SORCE SWG July 2002 - 18 Solar Rotation (27-day) Variations ♦ ♦ ♦ Fairly strong 27-day variation seen in late April EGS degradation is not included yet as evident for the brighter lines in EGS Trend is similar to “reference” variation but significant differences, such as for H continuum (80-90 nm) and XUV (< 30 nm), need to be studied in more detail at other time periods Pre-TIMED reference 27-day variation that is based on UARS, SNOE, rockets, and AE-E results [Woods and Rottman, in Comparative Aeronomy, 2002] XPS EGS TIMED SEE SORCE SWG July 2002 - 19 SEE’s Occultation Will Yield O, O 2, and N2 Densities Normal Solar Occultation SEE occultation experiments are possible about 2 weeks per yaw around period Unit Optical Depth for Solar Min. Condition Raw SEE data is used for this example (no corrections for dark, scattered light, etc.) TIMED SEE SORCE SWG July 2002 - 20 SEE Team’s Future Science Effort ♦ Validating the absolute solar irradiance values • Comparisons with SOHO, SNOE, and UARS measurements • Comparisons with SORCE XPS and SOLSTICE measurements ♦ ♦ Characterizing the solar UV variations as function of wavelength and over different time scales Modeling the atmospheric response to the measured solar variations • Photoelectron response studies using FAST photoelectron data and the ‘glow’ model (Stan Solomon, Scott Bailey, Frank Eparvier) • Atmospheric response studies using TIME-GCM (Ray Roble, Stan Solomon) ♦ Modeling the solar variation • Study active feature evolution using SOHO, TRACE, and PSPT images (Judith Lean, Tom Woods, Giuliana de Toma, Dick White) • Improve models of the solar irradiance (NRLEUV: Judith Lean, SOLAR2000: Kent Tobiska, SunRise: Dick White, Peter Fox) TIMED SEE SORCE SWG July 2002 - 21