kumbangn.

/ˈkʊmbaŋ/

Forms: Also koembang.

Etymology: local Javanese koembang.

A föhn wind which blows in Java.

ΘΚΠ

the world > the earth > weather and the atmosphere > weather > wind > [noun] > hot or warm wind > hot or warm and dry > katabatic > in Java

kumbang1931

1931 A. A. Miller Climatol. v. 83 These winds have a foehn-like nature, their dry heat doing considerable damage to the more sensitive crops, especially tobacco. Such a wind is the ‘Koembang’ of Java.

1954 E. D. Laborde tr. C. Robequain Malaya, Indonesia, Borneo & Philippines ix. 187 At that time,..the lowlands between Cheribon and Tegal fairly often experience the drying effort of the south-east wind which, after crossing the Pembarisan Hills, becomes a foehn known as the kumbang.

1969 M. Sukanto in H. Arakawa Climates N. & E. Asia iv. 222 Tjirebon and Tegal (Central Djawa) are also exposed to such a wind during the dry season. In this case, the wind flows down from the western part of Mount Slamet and blows in a northern and northeastern direction. This wind is called the Kumbang.

This entry has not yet been fully updated (first published 1976; most recently modified version published online December 2020).

单词	kumbang
释义	kumbangn. /ˈkʊmbaŋ/ Forms: Also koembang. Etymology: local Javanese koembang. A föhn wind which blows in Java. ΘΚΠ the world > the earth > weather and the atmosphere > weather > wind > [noun] > hot or warm wind > hot or warm and dry > katabatic > in Java kumbang1931 1931 A. A. Miller Climatol. v. 83 These winds have a foehn-like nature, their dry heat doing considerable damage to the more sensitive crops, especially tobacco. Such a wind is the ‘Koembang’ of Java. 1954 E. D. Laborde tr. C. Robequain Malaya, Indonesia, Borneo & Philippines ix. 187 At that time,..the lowlands between Cheribon and Tegal fairly often experience the drying effort of the south-east wind which, after crossing the Pembarisan Hills, becomes a foehn known as the kumbang. 1969 M. Sukanto in H. Arakawa Climates N. & E. Asia iv. 222 Tjirebon and Tegal (Central Djawa) are also exposed to such a wind during the dry season. In this case, the wind flows down from the western part of Mount Slamet and blows in a northern and northeastern direction. This wind is called the Kumbang. This entry has not yet been fully updated (first published 1976; most recently modified version published online December 2020). < n.1931
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