ASPB and CIMSS Weekly Report
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ASPB AND CIMSS WEEKLY HIGHLIGHTS FOR THE WEEK ENDING MAY 25, 2013

IN THE PRESS:

ITEMS FOR THE ADMINISTRATOR:

ITEMS FOR THE ASSISTANT ADMINISTRATOR:

ITEMS FOR THE OFFICE DIRECTOR, STAR:

RAQMS supports Wyoming Exceptional Event Demonstration: On May 21, 2013, the State of Wyoming Department of Environmental Quality/Air Quality Division released a document entitled “Exceptional Event Demonstration Package for the Environmental Protection Agency Thunder Basin, Wyoming Ozone Standard Exceedance June 6, 2012” (http://deq.state.wy.us/aqd/Exceptional%20Events/June_6_2012ThunderBasin/June_6_2012_SI_Package.pdf) for public comment. In the exceptional event demonstration, results from Real-time Air Quality Modeling System (RAQMS) ozone analyses and Lagrangian trajectory analysis were used determine the genesis of a stratospheric intrusion (SI) event observed by the NASA Ames Alpha Jet Atmospheric eXperiment (AJAX, http://geo.arc.nasa.gov/ajax/ajax_index.html) over California on June 5, 2012 that led to surface ozone exceedances on June 6, 2012 at the Thunder Basin ozone monitor in NE Wyoming. Following the public comment period, this document will be submitted to the US Environmental Protection Agency (US EPA) to demonstrate that the surface ozone exceedances where due to an exceptional event associated with a stratospheric intrusion (SI). According to the US EPA, exceptional events are unusual or naturally occurring events that can affect air quality but are not reasonably controllable using techniques that tribal, state or local air agencies may implement in order to attain and maintain the National Ambient Air Quality Standards. (R.B. Pierce, E/RA2, 608-890-1892, brad.pierce@ssec.wisc.edu)

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Figure caption: RAQMS 4km ozone (O3, ppbv, upper left panel) map and 122W cross-section (ppbv, lower left panel) on 5 June 2012 at 11 am MST. The AJAX flight track is shown in black. Note the tropopause fold indicated by the tongue of high ozone extending from the lower stratosphere into the mid-troposphere. Upper right panel shows a map of 7-day averaged (May 30-June 5, 2012) AIRS total column O3 (DU) with back trajectory history (white) and origin (white with blue edges) at 11 am MST on May 30, 2012 for AJAX Flight 47 SI encounter. Lower right panel shows RAQMS 150W O3 (ppbv) and zonal wind (m/s) cross-section with origin of AJAX Flight 47 SI encounter (blue dots) at 11 am MST on May 30, 2012. 

CSPP/IMAPP User's Group Meeting, Madison WI: The first Community Satellite Processing Package (CSPP) and International MODIS/AIRS Processing Package (IMAPP) Users’ Group Meeting was held in Madison, Wisconsin, 21-23 May 2013. The goal of the meeting was to bring together the worldwide community of CSPP and IMAPP users to discuss issues relevant to reception, processing, and applications of data acquired by direct broadcast from the Suomi NPP, Terra, and Aqua satellites. Bob Aune gave a presentation on improvements to the IMAPP Direct Broadcast CIMSS Regional Assimilation System (DBCRAS). Andy Heidinger and Nick Bearson briefed on the CSPP implementation of the NESDIS Clouds from AVHRR Extended (CLAVR-x) processing system. Many other Cooperative Institute for Meteorological Satellite Studies (CIMSS), Space Science and Engineering Center (SSEC), and NOAA personnel participated, along with attendees from Sweden, UK, France, Germany, Mexico, and Australia. CSPP is supported by the JPSS program. (R. Aune, E/RA2, 608-262-1071; A. Heidinger, E/RA2, 608-263-6757, andrew.heidinger@noaa.gov, Nick Bearson, CIMSS, nick.bearson@ssec.wisc.edu)

Third Meeting of the Polar Space Task Group: The third meeting of the World Meteorological Organization's (WMO) Polar Space Task Group (PSTG) was held at Centre National d’Etudes Spatiales (CNES) in Paris, France, 22-23 May 2013. The PSTG was established for the purpose of space agency planning, processing, and archiving of satellite products covering, or relevant to, the polar regions. All major space agencies have representatives on the PSTG. Jeff Key, PSTG Vice Chair, participated remotely due NOAA travel cuts. (J. Key, E/RA2, 608-263-2605, jkey@ssec.wisc.edu)

ITEMS FOR THE DIVISION CHIEF, CoRP:

Satellite Imagery from Moore, Oklahoma EF5 Tornado Event: Geostationary Operational Environmental Satellite (GOES), Visible Infrared Imager Radiometer Suite (VIIRS), and Moderate Resolution Imaging Spectroradiometer (MODIS) images from the Moore, Oklahoma EF5 tornado event on May 20, 2013 were posted on the Cooperative Institute for Meteorological Satellite Studies (CIMSS) Satellite Blog (http://cimss.ssec.wisc.edu/goes/blog/archives/12984). (S. Bachmeier, CIMSS, 608-263-3958)


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Figure caption: 1-km resolution MODIS 0.65 µm visible channel visible and 11.0 µm InfraRed (IR) images at 19:36 UTC (about a half hour before the tornado moved through Moore, Oklahoma) displayed signatures of vigorous convective overshooting tops, with cloud-top IR brightness temperatures as cold as -76º C.

GOES-13 Outage and Switch to GOES-14: Geostationary Operational Environmental Satellite (GOES)-13 suffered an anomaly when the satellite was no longer pointed toward the Earth for as a yet unknown reason. The anomaly started at 03:38 UTC on 22 May. At 04:29 UTC, GOES-West (GOES-15) began a 30-minute full disk scan schedule. After being taken out of on-orbit storage, GOES-14 began imaging early on 23 May. The Cooperative Institute for Meteorological Satellite Studies (CIMSS) Satellite Blog contains more information on the GOES-13 outage (http://cimss.ssec.wisc.edu/goes/blog/archives/13031) and on GOES-14 beginning service as GOES-East (http://cimss.ssec.wisc.edu/goes/blog/archives/13063). Processing at CIMSS is now using GOES-14 as the Eastern satellite (http://cimss.ssec.wisc.edu/goes/rt/sounder-dpi.php.) (T. Schmit, E/RA2, 608-263-0291, tim.j.schmit@noaa.gov; S. Bachmeier, CIMSS, 608-263-3958; S. Lindstrom, CIMSS, J. Nelson, CIMSS, 608-263-6013)

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Figure caption: GOES-13 Imager of the 11 um infrared window band for two times (03:15 and 03:32 UTC) on May 22, 2013. The large navigation offset is apparent in the right-hand panel, which is the last good image from GOES-13 before the major anomaly. The yellow line shows the approximate amount of the navigation error (~200 km).

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