University of Hertfordshire

From the same journal

By the same authors

  • A. Ansmann
  • Matthias Tesche
  • D. Althausen
  • D. Mueller
  • P. Seifert
  • V. Freudenthaler
  • B. Heese
  • M. Wiegner
  • G. Pisani
  • P. Knippertz
  • O. Dubovik
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Original languageEnglish
Article numberD04210
Number of pages16
JournalJournal of Geophysical Research: Atmospheres
Publication statusPublished - 27 Feb 2008


Multiwavelength lidar, Sun photometer, and radiosonde observations were conducted at Ouarzazate ( 30.9 degrees N, 6.9 degrees W, 1133 m above sea level, asl), Morocco, in the framework of the Saharan Mineral Dust Experiment (SAMUM) in May-June 2006. The field site is close to the Saharan desert. Information on the depolarization ratio, backscatter and extinction coefficients, and lidar ratio of the dust particles, estimates of the available concentration of atmospheric ice nuclei at cloud level, profiles of temperature, humidity, and the horizontal wind vector as well as backward trajectory analysis are used to study cases of cloud formation in the dust with focus on heterogeneous ice formation. Surprisingly, most of the altocumulus clouds that form at the top of the Saharan dust layer, which reaches into heights of 4-7 km asl and has layer top temperatures of -8 degrees C to -18 degrees C, do not show any ice formation. According to the lidar observations the presence of a high number of ice nuclei (1-20 cm(-3)) does not automatically result in the obvious generation of ice particles, but the observations indicate that cloud top temperatures must typically reach values as low as -20 degrees C before significant ice production starts. Another main finding is that liquid clouds are obviously required before ice crystals form via heterogeneous freezing mechanisms, and, as a consequence, that deposition freezing is not an important ice nucleation process. An interesting case with cloud seeding in the free troposphere above the dust layer is presented in addition. Small water clouds formed at about -30 degrees C and produced ice virga. These virga reached water cloud layers several kilometers below the initiating cloud cells and caused strong ice production in these clouds at temperatures as high as -12 degrees C to -15 degrees C.

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