1989
DOI: 10.1016/0169-8095(89)90033-1
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Lidar observation of time and spatial variations of backscattering coefficient near the stratiform cloud base

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Cited by 2 publications
(3 citation statements)
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“…The smaller particles, if less than 10^m in size, would give a smaller backscatter at 10.6 microns which could give an apparently lower cloud top. Figure 5 shows the cloud-base distribution with altitude measured by Kolev et al (1993) in their ECLIPS (Phase II) experiment, given as the numbers of occurrences between various height ranges. Two cloud groups are noted, one at 700 to 1200 m and another at 2000 to 2600 m. These two groups are related to the thermodynamics of the atmospheric boundary layer and to the formation of fair-weather cumulus at the higher altitudes.…”
Section: Retrieval Of Cloud Base a Definition Of Cloud Basementioning
confidence: 99%
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“…The smaller particles, if less than 10^m in size, would give a smaller backscatter at 10.6 microns which could give an apparently lower cloud top. Figure 5 shows the cloud-base distribution with altitude measured by Kolev et al (1993) in their ECLIPS (Phase II) experiment, given as the numbers of occurrences between various height ranges. Two cloud groups are noted, one at 700 to 1200 m and another at 2000 to 2600 m. These two groups are related to the thermodynamics of the atmospheric boundary layer and to the formation of fair-weather cumulus at the higher altitudes.…”
Section: Retrieval Of Cloud Base a Definition Of Cloud Basementioning
confidence: 99%
“…5. Frequency histograms of the number of cases of retrieved cloud base at different altitudes for stratocumulus and cumulus clouds (Kolev et al 1993).…”
Section: Retrieval Of Extinction Coefficientmentioning
confidence: 99%
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