| 11. | The top of a nimbostratus deck is usually in the middle level of the troposphere.
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| 12. | Nimbostratus cloud droplets can also be quite large, up to 0.015 mm radius.
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| 13. | If the precipitation increases in persistence and intensity, the altostratus cloud may thicken into nimbostratus.
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| 14. | They comprise two or three genera depending on the system of height classification being used : nimbostratus.
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| 15. | These are the nimbostratus clouds, and the cumulonimbus clouds, and are classified as pannus clouds.
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| 16. | This sometimes leads to the continued exclusion of nimbostratus from the group of vertical clouds by some independent meteorologists.
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| 17. | Lightning from an embedded cumulonimbus cloud may interact with the nimbostratus but only in the immediate area around it.
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| 18. | Altostratus tends to form ahead of a warm or occluded front, the altostratus gradually thickening into rain bearing nimbostratus.
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| 19. | The occurrence of cumulonimbus and nimbostratus together is uncommon, and usually only nimbostratus is found at a warm front.
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| 20. | The occurrence of cumulonimbus and nimbostratus together is uncommon, and usually only nimbostratus is found at a warm front.
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