High Resolution Dynamics Limb Sounder observations of polar stratospheric clouds and subvisible cirrus

  • Steven Massie
  • , John Gille
  • , Rashid Khosravi
  • , Hyunah Lee
  • , Douglas Kinnison
  • , Gene Francis
  • , Bruno Nardi
  • , Thomas Eden
  • , Cheryl Craig
  • , Chris Halvorson
  • , Michael Coffey
  • , Daniel Packman
  • , Charles Cavanaugh
  • , James Craft
  • , Vincil Dean
  • , David Ellis
  • , John Barnett
  • , Christopher Hepplewhite
  • , Alyn Lambert
  • , Gloria Manney
  • Anthony Strawa, Marion Legg

Research output: Contribution to journalArticlepeer-review

22 Scopus citations

Abstract

The High Resolution Dynamics Limb Sounder (HIRDLS) cloud detection and cloud top determination algorithm is described and applied to 2005-2007 HIRDLS radiance profiles. Statistical averages of HIRDLS and correlative cloud data are highly correlated. The 1998-2005 Halogen Occultation Experiment (HALOE) and HIRDLS time averaged cloud top pressures have a correlation coefficient of 0.87 and 0.93 in the tropics and midlatitudes, respectively. Time series of the temperature T < 195 K hemispherical area, on the 450 K potential temperature surface, and the total number of polar stratospheric clouds observed by the HIRDLS experiment in January and February 2005 have a correlation coefficient of 0.92. HALOE and HIRDLS normalized distributions of cloud counts, expressed as a function of outgoing longwave radiation (OLR), have a correlation coefficient of 0.99. Tropical averages of 1998-2005 HALOE and HIRDLS cloud occurrence frequencies at 82 and 100 hPa are within 25% of each other, and the morphology of latitude-longitude contour maps of cloud frequency are similar. Colocated Stratospheric Aerosol and Gas Experiment (SAGE III) and HIRDLS cloud top pressure values in 2005 have a correlation coefficient of 0.85 when the distance between observations is less than 100 kin and the time difference is less than 6 h. Correlations between colocated GE III and HIRDLS cloud top pressures improve as space and time differences decrease.

Original languageEnglish
Article numberD24S31
JournalJournal of Geophysical Research
Volume112
Issue number24
DOIs
StatePublished - Dec 27 2007

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