Example Science Applications of SABER Processed Data.

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Example Science Applications of SABER Processed Data Slide 2 NLTE SABER zonal mean temperature July 4, 2002 showing double mesopause structure NLTE temperature shows double mesopause structure NLTE LTE LTE temperature shows little double mesopause structure (Mertens et al, 2003) Slide 3 SABER data show presence of mesospheric chemical heating on June 4, 2002 20 K/day 5 K/day Chemical heating present every day of yaw period analyzed for May July, 2002 H + O 3 O + O + M O + O 2 + M Slide 4 SABER (m,f) Spectra at ~71 km show quasi-2-day wave (Garcia, 2003) Large 2-day wave amplitudes are seen around summer solstice Variance is present along a line of constant phase speed; largest for m = 3, 4 near 0.5 cpd c ~ 70 m/s Jan-Feb 2002 at 36 SJun-Jul 2002 at 36 N c~70 ms - 1 Slide 5 SABER quasi-2-day wave amplitude for 2002 and 2003 (Garcia, 2004) =3, June 15-July 14, 2002 =3, June 14-July 14, 2003 =4, June 15-July 14, 2002 =4, June 14-July 14, 2003 Slide 6 October November 2003 Solar Storm Slide 7 NO VER before storm October 12, 2003 NO VER near storm peak October 31, 2003 Oct Nov, 2003 solar storm shows large effect on NO emission at 125 km Slide 8 Slide 9 Slide 10 Slide 11 Slide 12 Slide 13 Slide 14 Slide 15 Slide 16 Slide 17 Slide 18 Slide 19 Slide 20 Slide 21 Slide 22 Slide 23 Slide 24 Slide 25 Slide 26 Slide 27 Slide 28 Slide 29 Slide 30 Slide 31 Slide 32 Slide 33 Slide 34 Slide 35 Slide 36 Slide 37 NO mixing ratio profiles measured by HALOE on the UARS Platform Slide 38 HALOE daily zonal mean thermosphric NO profiles Oct 2003 Slide 39 HALOE daily zonal mean thermosphric NO profiles Nov 2003 Slide 40 NO VER time series at 125 km compared with X-ray, electron and proton fluxes from GOES and TIMED/SEE, Ap Index Slide 41 SABER Avg NO VER 125 km 70 o N - 80 o N Daily averaged NO VERs at 125 km, 70 o N - 80 o N, and Ap index Ap Index Corr. Coeff. 73% Slide 42 SABER 125 km northern hemisphere NO VERs on October 30 2003 with magnetic coordinates Slide 43 NO VERs at 110 km prior to solar storms NO VERs at 110 km, April 18, 2002, near peak of solar storm SABER NO Volume Emission Rates during the April, 2002 and October, 2003 Solar Storms NO VERs at 110 km, October 31, 2003, near peak of solar storm Slide 44 SH (45 o S 84 o S) maximum NO radiance (in color, red high) and temperature (contours) altitude versus time SH NO radiance and Tk versus time (top) and 40km O 3 and NO polar plots (bottom) - June 1 to August 31, 2003 Ozone mixing ratio (left), NO radiance (left) and potential vorticity contours at 40 km on August 23, 2003 O3O3 NO O 3 loss coupled with implied NO descent Slide 45 SABER 4.3- m Channel Solar Storm response compares well with GUVI LBH-2 SABER GUVI April 18, 2002 Slide 46 Comparison of SABER NO 5.3 m Energy Loss Rates for April, 2002 and October, 2003 solar storms October, 2003 82 o N April, 2002 82 o S Peak energy loss rates are comparable for the two storms Slide 47 Energy loss rate comparison for SABER NO 5.3 m And calculated TIME-GCM/ASPEN [O] at 63 m NO is dominant thermostat emitter in thermosphere storm NO [O] April, 2002 solar storm for 77.5 o S Slide 48 SABER Temperature Tidal Structures Slide 49 SABER CO 2 15- m Emission Shows Signature of Diurnal Tide Typical equatorial ascending / descending radiance profiles and difference (21 Mar 2002) Equatorial radiance s over 34 days (~8.8 hr LT ) - Vertical wavelength 22-25 km - Phase fronts descend with LT at ~ 22 km/day) - Consistent with interpretation as diurnal tide Slide 50 Slide 51 Slide 52 Slide 53 Slide 54 Slide 55 Slide 56 Slide 57 SABER Summary Slide 58 SABER Performance Summary The SABER instrument performance in orbit is excellent Routine periodic turn - off needed to remove detector/filter focal plane ice but effect is small now. Of no consequence for data processing Field-of-View effects addressed using orbital data and FOV knowledge is well in-hand Temperature data quality is excellent and agrees well with correlative data NLTE temperature ZM cross section shows clear double mesopause structure Diurnal tide and Quasi 2-day wave signatures present Mesosphere chemical heating present on all days analyzed NO radiances show strong effects due to solar storms large NO changes and major cooling Strong NO VER correlation with Ap index and enhancements align with magnetic coordinates. Evidence of NO descent to upper stratosphere with accompanying ozone loss.