Sumatra squall lines

Sumatra Squall Lines (SSL) also known simply as Sumatras are squall lines that develop over Sumatra at night when viewed from Singapore and Malaysia. These squalls develop most often between April and November and are steered east towards the west coast of Peninsular Malaysia and Singapore by the southwesterly winds of the monsoons. The squall usually arrives during the pre dawn and early morning with strong wind gusts and thundery showers.[1][2][3]

Theory

During the southwest monsoon, southwesterly winds pass over the mountains of Sumatra and creates mountain waves on the leeward side of the mountain thus creating an unstable atmosphere. As the atmosphere becomes highly unstable, the thunderstorms begin to merge into each other forming a squall line. This squall line is then steered by the southwesterly winds causing the storm to move northeastwards and moving into the Straits of Malacca. When this squall line moves offshore to the Straits of Malacca, it is usually night and thus, warmer air rising over the Straits of Malacca would cause the squall line to intensify. As the abundance of moisture over the Straits of Malacca condenses, it releases huge amounts of latent heat of condensation and this helps the squall line maintain its strength and intensify even more. This squall line then moves towards the coast of Peninsular Malaysia or Singapore. As this squall line moves inland, it is deprived of latent heat of condensation and hence, dissipates rapidly.

gollark: With no particular incentive to except that the "friend" might not like it otherwise?
gollark: So companies are supposed to just give goods to their "friends"...?
gollark: To some extent, but it's fuzzier, and how is that meant to work for *factories* or whatever?
gollark: And it's (very roughly) gotten by providing stuff people want, so organizations which can do that can pay more than ones which can't.
gollark: And "who can pay most" is simple and objective.

References

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.