Aerosol

J. T. Sullivan (GSFC), L. Twigg (SSAI), and G. Sumnicht (SSAI) — The STROZ lidar retrieves ozone vertical profiles in the stratosphere from 10 to 50 km. Temperature to ~80 km and aerosols (at 355 nm) to 35 km also are measured. The instrument has also been modified to measure water vapor from near the ground to ~15 km. When not participating in campaigns, the instrument conducts measurements at the NASA Goddard Space Flight Center in Greenbelt, MD. The STROZ lidar participated in the ozone and water vapor comparisons during the WAVES 2008 and 2009 campaigns. Data through 2001 is archived in the name of the previous PI – McGee.

J. T. Sullivan (GSFC), L. Twigg (SSAI), and G. Sumnicht (SSAI) — The STROZ lidar retrieves ozone vertical profiles in the stratosphere from 10 to 50 km. Temperature to ~80 km and aerosols (at 355 nm) to 35 km also are measured. The instrument has also been modified to measure water vapor from near the ground to ~10 km. As a mobile intercomparator, it has participated in ozone intercomparisons at OHP for July–August 1992 and for June–July 1997. Teh 1992 and 1997 data is archived in the name of the previous PI – McGee.

J. T. Sullivan (GSFC), L. Twigg (SSAI), and G. Sumnicht (SSAI) — The STROZ lidar retrieves ozone vertical profiles in the stratosphere from 10 to 50 km. Temperature to ~80 km and aerosols (at 355 nm) to 35 km also are measured. The instrument has also been modified to measure water vapor from near the ground to ~15 km. As a mobile intercomparator, it has participated in an ozone and temperature intercomparisons at Hohenpeissenberg in October 2005. The 2025 data is archived in the name of the previous PI – McGee.

J. T. Sullivan (GSFC), L. Twigg (SSAI), and G. Sumnicht (SSAI) — The STROZ lidar retrieves ozone vertical profiles in the stratosphere from 10 to 50 km. Temperature to ~80 km and aerosols (at 355 nm) to 35 km also are measured. The instrument has also been modified to measure water vapor from near the ground to ~15 km. As a mobile intercomparator, it has participated in an ozone intercomparison at Sodankylä during March–April 2006 and in February 2007. The 2026-2007 data is archived in the name of the previous PI – McGee.

J. Rosen (U. Wyoming) and N. Larsen (DMI) – Backscatter measurements of aerosol profiles available for January 1992 – December 1998.

J. T. Sullivan (GSFC), L. Twigg (SSAI), and G. Sumnicht (SSAI) — The STROZ lidar retrieves ozone vertical profiles in the stratosphere from 10 to 50 km. Temperature to ~80 km and aerosols (at 355 nm) to 35 km also are measured. The instrument has also been modified to measure water vapor from near the ground to ~10 km. As a mobile intercomparator, it has participated in an ozone intercomparison in Ny Ålesund in September 1997 and January–February 1998. The 1997-1998 data is archived in the name of the previous PI – McGee.

J. Rosen (U. Wyoming) — Backscatter measurements from 1990 to 1991.

J. Rosen (U. Wyoming) — Dustsonde measurements of aerosol profiles from 1972 to 1980.

M. Snels (ISAC-CNR), F. Cairo (ISAC-CNR), and G. Di Donfrancesco (ENEA) — Database extends back to 1990. Measurements were made from February through October. Data from 1990 to 2002 are archived under previous PI (Adriani). Operations discontinued in October 2010. Relocation to Dome C planned for 2014.

J. Rosen (U. Wyoming) — Dustsonde measurements of aerosol profiles from 1973 to 1979.