Aerosol

O. Schrems and F. Immler (AWI) – Mobile Aerosol Raman Lidar (MARL), participated; campaign data were obtained at Prestwick from September to October 2000.

O. Schrems and F. Immler (AWI) – Mobile Aerosol Raman Lidar (MARL), participated; campaign data were obtained at the Meteorological Observatory in Lindenberg, Germany from April to October 2003.

J. Rosen (U. Wyoming) and N. Larsen (DMI) – Backscatter profile measurements available for January 1995 and January 1996.

J. Rosen (U. Wyoming) and V. Khattatov (CAO) – Backscatter measurements of aerosol profiles available for November–December 1993.

J. Rosen (U. Wyoming) and V. Yushkov (CAO) – Backscatter measurements of aerosol profiles available for March 1999 and January 2000.

J. T. Sullivan (GSFC), G. Sumnicht (SSAI), and L. Twigg (SSAI) — The Aerosol and Temperature Lidar (AT Lidar) has been rebuilt, and now includes water vapor to ~15 km, temperature in the troposphere using rotational Raman backscatter, stratospheric temperature up to ~80 km, and aerosol parameters using elastic and Raman backscatter up to ~35 km. When not participating in campaigns, the instrument conducts measurements at the NASA Goddard Space Flight Center in Greenbelt, MD. The AT lidar participated in the WAVES 2006, 2007, 2008 and 2009 campaigns conducted in Beltsville, MD. Data through 2009 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 ozone intercomparisons at the Table Mountain Facility February/March 1992, February/March 1997, June 2004, June 2005, October 2009 (MOHAVE), and February–March 2011. Data through 2011 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 ozone intercomparisons at Lauder October–December 1992, March–October 1994, April 1995, September–December 2001, April 2002, June–July 2011, and April 2012. Data through 2012 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 and temperature intercomparisons at Mauna Loa from June 1995–February 1996, August 2002, November 2012–August 2013, and January 2014. The 1995-1996 data is archived in the name of the previous PI – McGee.

J. T. Sullivan (GSFC), G. Sumnicht (SSAI), and L. Twigg (SSAI) — The Aerosol and Temperature Lidar (AT Lidar) has been rebuilt, and now includes water vapor to >10 km, temperature in the troposphere using rotational Raman backscatter, stratospheric temperature up to ~80 km, and aerosol parameters using elastic and Raman backscatter up to ~35 km. It has participated in ozone intercomparisons at the Table Mountain Facility in June 2005 and in water vapor intercomparisons during the MOHAVE campaign of October 2006, 2007, and 2009. Data through 2009 is archived in the name of the previous PI – McGee.