Dust Vortex in the Taklimakan Desert by Himawari-8 High Frequency and Resolution Observation

Keiya Yumimoto, Mizuo Kajino, Taichu Y. Tanaka, Itsushi Uno

Research output: Contribution to journalArticle

Abstract

The Taklimakan Desert is known to be one of the world’s major sources of aeolian dust particles. Continuous images with 10-min temporal and 2-km spatial resolutions from a new-generation geostationary meteorological satellite captured the lifecycle (generation, evolution and outflow) of a previously unrecognized type of Taklimakan dust storm. The dust storm showed an anti-clockwise spiral structure and a clear core and behaved like a “dust vortex”. From image analysis, the horizontal scale and temporal lifetime of the dust vortex were estimated to be 600 km and 36 hours, respectively. We found that a strong pressure trough (cut-off low), along with a cold air mass located on the northwestern side of the Taklimakan Desert and the high mountains surrounding the Taklimakan Desert, played important roles in the formation and evolution of the dust vortex.

Original languageEnglish
Article number1209
JournalScientific reports
Volume9
Issue number1
DOIs
Publication statusPublished - Dec 1 2019

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Dust
Observation
Air
Pressure

All Science Journal Classification (ASJC) codes

  • General

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Dust Vortex in the Taklimakan Desert by Himawari-8 High Frequency and Resolution Observation. / Yumimoto, Keiya; Kajino, Mizuo; Tanaka, Taichu Y.; Uno, Itsushi.

In: Scientific reports, Vol. 9, No. 1, 1209, 01.12.2019.

Research output: Contribution to journalArticle

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