Simon Carn 1, Matt DeLand 2, Nick Gorkavyi 2, Eric Hughes 3 and Nick Krotkov 4
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1 Simon Carn 1, Matt DeLand 2, Nick Gorkavyi 2, Eric Hughes 3 and Nick Krotkov 4 1. Michigan Technological University, Houghton, MI 2. Science Systems and Applications, Inc., Lanham, MD 20706, USA 3. University of Maryland, College Park, MD, USA 4. Code 614, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA Goddard Space Flight Center
2 UV satellite instruments currently in orbit Instrument Satellite(s) Overpass Nadir footprint area (km 2 ) Data coverage Polar orbiters (LEO) Ozone Monitoring Instrument (OMI) Aura 1:45 pm 312 (13 24) Sep present Global Ozone Monitoring Experiment-2 (GOME-2) MetOp-A/B 9:30 am 3200 (40x80) Oct present Ozone Mapper and Profiler Suite (OMPS) Suomi NPP 1:30 pm Standard: 2500 (50 50) Zoom: 100 (10 10) Apr present L 1 Lagrange Point Earth Polychromatic Imaging Camera (EPIC) DSCOVR Full disk every ~90 mins 576 (24 24) From late 2015 (Geostationary UV sensors planned for later this decade)
3 Current OMI measurements OMI measurements of Manam (PNG) eruption on July 31, 2015 OMI spatial coverage since 2008 affected by row anomaly data gap global coverage achieved every 2 days Good data in useable parts of swath UV satellite products: SO 2 column amount Sensitive to tropospheric and stratospheric SO 2 UV Aerosol Index (UVAI) Semi-quantitative indication of ash presence Sensitive to any UV-absorbing aerosol (ash, smoke, dust)
4 Suomi-NPP/OMPS Sensors Limb Profiler (LP): Aerosol and Ozone profiles 3 OMPS instruments Nadir Mapper (NM; OMI) Nadir Profiler (NP) Limb Profiler (LP) 13:30 LT ascending node OMPS LP: Looks aft, following nadir view by ~7 minutes 3 vertical slits with 250 km spacing Spectral range: nm ~2 km vertical resolution; surface to ~105 km altitude Nadir Mapper (NM): swath similar to OMI NP OMPS-NM spatial zoom mode: 10x10 km Launched October 2011
5 Aura (2004-) OMI - SO 2, NO 2, BrO TES - SO 2 MLS - strat. SO 2, HCl CloudSat (2006-) CPR (radar) precipitation, hydrometeors Aqua (2002-) MODIS - SO 2, ash, sulfate AIRS - UTLS SO 2, ash Volcanic CO 2? The A-Train OMPS, VIIRS, CrIS - SO 2, ash CALIPSO (2006-) CALIOP (lidar) - cloud altitude, aerosol phase
6 OMPS-LP Aerosol Scattering Index (ASI) Calbuco (Chile) plume on April 26, 2013 Aerosol Scattering Index (ASI) æ ASI = ln I 0 ç è I 0 = observed radiance I R = modeled Rayleigh radiance ASI is not a retrieval, but a semi-quantitative Indication of aerosol/cloud presence Scattering angle effects important I R ö ø
7 OMPS (zoom): Ojos del Salado plume June 13, 2015 Ojos del Salado OMPS-NM zoom mode observations of Ojos del Salado plume on June 13, 2015 No global OMPS-LP data during OMPS-NM zoom mode operation (bandwidth) Clear OMPS UVAI signal No coincident OMI UVAI anomaly (spatial resolution effect?) No OMPS or OMI SO 2 signal Volcanic eruption source unlikely
8 OMPS-NM SO 2 Calbuco (Chile), Apr 22 May 20, 2015
9 OMPS-NM UVAI Calbuco (Chile), April 24, slits
10 OMPS-NM SO 2 Calbuco (Chile), April 24, slits
11 Aqua/MODIS showing Calbuco ash April 24, 2015
12 CALIPSO + OMPS-NM Calbuco (Chile), April 24, 2015
13 CALIPSO + OMPS-LP Calbuco (Chile), April 24, 2015 ASI = Aerosol Scattering Index at 674 nm Background = CALIOP; contours = OMPS-LP
14 OMPS-NM SO 2 Calbuco (Chile), April 26, 2015 Calbuco 3 slits OMPS-LP slits and CALIPSO tracks
15 OMPS-NM UVAI Calbuco (Chile), April 26, 2015 Calbuco 3 slits OMPS-LP slits and CALIPSO tracks
16 Aqua/MODIS showing Calbuco ash April 26, 2015
17 CALIOP backscatter and OMPS-LP ASI (to east) ASI = Aerosol Scattering Index at 674 nm Background = CALIOP; contours = OMPS-LP
18 CALIOP backscatter and OMPS-LP ASI (to west) ASI = Aerosol Scattering Index at 674 nm Background = CALIOP; contours = OMPS-LP
19 CALIOP backscatter and OMPS-NM
20 OMPS Direct Broadcast data for the North Atlantic Finnish Meteorological Institute (FMI)
21 OMPS Direct Broadcast data for the North Pacific Alaska Geographic Information Network of Alaska (GINA) Kamchatka Aleutians
22 Detection of NO 2 in volcanic eruption plumes OMI detected NO 2 in 2011 Grimsvötn and 2008 Okmok volcanic clouds Grimsvötn May 22, 2011 NO 2 known to be generated by lightning in thunderstorms Signal of plume electrification at overpass time Indicates air (N 2 ) entrainment Okmok Jul 12, 2008 Both the Grimsvötn and Okmok eruptions featured distinct vertical separation of gas (SO 2 ) and ash Plan to analyze NO 2 data for other explosive eruptions and coincident WWLLN lightning detections
23 Deep Space Climate Observatory (DSCOVR) at L 1 Simulation of EPIC views of May 2006 Soufriere Hills volcanic cloud Earth Polychromatic Imaging Camera (EPIC) ~90 min temporal resolution Spatial resolution similar to OMI at sub-satellite point SO 2, UVAI and volcanic ash retrievals planned
24 Summary OMI still providing high quality data outside data gaps OMPS-NM zoom mode (Saturdays) provides increased sensitivity to volcanic ash and SO 2 Ojos del Salado resuspended ash plume detected in UVAI; no SO 2 Future OMPS instruments on JPSS may be 100% zoom mode OMPS-LP: useful new tool for analysis of volcanic plumes Additional plume altitude information between CALIOP overpasses Aerosol type information? Aerosol scattering signal in LP profiles even in young plumes Lightning-generated NO 2 detected in some eruption plumes Additional technique for eruption detection Indicative of strong convection and plume electrification at satellite overpass time DSCOVR/EPIC soon to be operational at L 1 Volcanic SO 2 and UVAI data with ~90-minute temporal resolution
25 Ash spectral refractive indices in the UV-visible Carn and Krotkov (2015)
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