2008
DOI: 10.1002/cjg2.1241
|View full text |Cite
|
Sign up to set email alerts
|

Dynamic Relationships Between the Horizontal Helicity and the Sandstorm

Abstract: Using the recorded data of upper wind and surface wind at 08 h and 20 h everyday from 2002 to 2006, we calculated the horizontal helicity from surface to 500 hPa. The results show that the more negative the horizontal helicity is, the higher the wind velocities from the surface to 500 hPa are and the stronger the westerly wind is. Consequently, the shear strength of the vertical air flow increases and the convergent vertical air flow thus enhances, which resulting in the formation of extremely severe dust stor… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...

Citation Types

0
0
0

Publication Types

Select...

Relationship

0
0

Authors

Journals

citations
Cited by 0 publications
references
References 6 publications
0
0
0
Order By: Relevance

No citations

Set email alert for when this publication receives citations?