It is known that atmospheric vortex structures causing extreme weather even
ts are of helical nature. It is suggested that the presence of helicity pro
vides for their development and longevity. Since the axial velocity compone
nt is non-zero, such vortex structures can draw in dust particles. Such par
ticles are retained by a vortex for a sufficiently long time due to its cer
tain features caused by the velocity distribution in a vortex. The retained
particles circulate in the vortex for a considerable part of its life-time
, moving together with the vortex. Such a mechanism can explain scalar tran
sfer to long distances. (C) 2000 Elsevier Science Ltd. All rights reserved.