Talk:Thunderstorm

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Good articleThunderstorm has been listed as one of the Natural sciences good articles under the good article criteria. If you can improve it further, please do so. If it no longer meets these criteria, you can reassess it.
Article milestones
DateProcessResult
October 6, 2006Good article nomineeListed
October 26, 2006Good article reassessmentDelisted
October 12, 2009Good article nomineeListed
Current status: Good article

Copy edit donation from Severe weather

Thunderclouds also have a wide distribution of occurrences. These forms of clouds are able to form under the circumstance where warm, moist air collides with cool air fronts.[1] Thunderclouds undergoes two stages of development: Cumulus and Mature.[2] During the stage of Cumulus, the heat generated from the Sun's radiation warms up the Earth's crust and the air close towards it. The warming of the air cause an updraft to form, allowing the warmed air to rise as warm air is less dense than normal oxygen. If the updraft contains water molecules, the rising of the updraft would cause the water molecules to condense forming a Cumulus cloud(there is less heat presented in higher attitudes). The continuation of condensation of the water molecules would allow the Cumulus cloud to reach greater volume.

Cumulonimbus cloud. The Cumulonimbus cloud is the basic foundation of a thundercloud.[4]

This information was removed from the severe weather page, but may be of use to your article. Respectfully Bullock 18:56, 28 May 2010 (UTC)[reply]

References

  1. ^ Cite error: The named reference nssl.noaa.gov was invoked but never defined (see the help page).
  2. ^ "Thunderstorm Formation". Windows Team. September, 2000. Retrieved 28 July 2009. {{cite web}}: Check date values in: |date= (help)
  3. ^ "Cumulus Stage". Windows Team. September, 2000. Retrieved 28 July 2009. {{cite web}}: Check date values in: |date= (help)
  4. ^ "Mature Stage". Windows Team. September, 2000. Retrieved 28 July 2009. {{cite web}}: Check date values in: |date= (help)