1979•Journal of applied meteorologyOpen access

In SituAircraft Verification of the Quality of Satellite Cloud Winds over Oceanic Regions

A. Fritz Hasler, William C. Skillman, WILLIAM E. SHENK, Joseph Steranka

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Abstract

A 5-year aircraft experiment to verify the quality of satellite cloud winds over oceans using in situ aircraft Inertial Navigation System wind measurements has been completed. The final results show that satellite measured cumulus cloud motions Vcloud are very good estimators of the cloud-base wind VCBW (900–950 mb) for trade wind and subtropical high regions. The average magnitude of the vector differences between the cloud motion and the cloud-base wind ranged from 0.9 to 1.7 m s−1 [ 0.9 m s−1 ≤ | Vcloud−VCBW| ≤1.7 m s−1. For cumulus clouds near frontal regions, the cloud motion agreed best with the mean cloud layer wind VMCLW [|Vcloud−VMCLW|. For a very limited sample, cirrus cloud motions also most closely followed the mean wind in the cloud layer [|Vcloud−VMCLW| = 1.7 m s−1].

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What this paper is about

A 5-year aircraft experiment to verify the quality of satellite cloud winds over oceans using in situ aircraft Inertial Navigation System wind measurements has been completed. The final results show that satellite measured cumulus cloud motions Vcloud are very good estimators of the cloud-base wind VCBW (900–950 mb) for trade wind and subtropical high regions. The average magnitude of the vector differences between the cloud motion and the cloud-base wind ranged from 0.9 to 1.7 m s−1 [ 0.9 m s−1 ≤ | Vcloud−VCBW| ≤1.7 m s−1. For cumulus clouds near frontal regions, the cloud motion agreed best with the mean cloud layer wind VMCLW [|Vcloud−VMCLW|. For a very limited sample, cirrus cloud motions also most closely followed the mean wind in the cloud layer [|Vcloud−VMCLW| = 1.7 m s−1].

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Available abstract

A 5-year aircraft experiment to verify the quality of satellite cloud winds over oceans using in situ aircraft Inertial Navigation System wind measurements has been completed. The final results show that satellite measured cumulus cloud motions Vcloud are very good estimators of the cloud-base wind VCBW (900–950 mb) for trade wind and subtropical high regions. The average magnitude of the vector differences between the cloud motion and the cloud-base wind ranged from 0.9 to 1.7 m s−1 [ 0.9 m s−1 ≤ | Vcloud−VCBW| ≤1.7 m s−1. For cumulus clouds near frontal regions, the cloud motion agreed best with the mean cloud layer wind VMCLW [|Vcloud−VMCLW|. For a very limited sample, cirrus cloud motions also most closely followed the mean wind in the cloud layer [|Vcloud−VMCLW| = 1.7 m s−1].

Key concepts: Environmental science, Cloud computing, Satellite, Cloud height, Cirrus, Meteorology, Wind profiler, Liquid water content

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