(Note: you may need to hit 'refresh' or 'reload' if the loops do not work on your first try.)
Summary:
A dust storm, originating in Mongolia, is detected by satellite, in surface observations and modeled by NAAPS.
The dust is lifted on the 31 December 2000 and 1 January 2001.
It is quickly transported to the east over Korea and Japan where it is reported in the surface observations,
and more slowly to the SE.
6-hourly NOGAPS Dynamics, 31 December - 4 January
High surface stress (magenta-colored areas in lower-right panels) on the 31st and 1st.
Note also, the deep 500 mb trough, oriented WNW-ESE: this trough sends a tongue
of dust far to the north (see next loop).
NAAPS Aerosol Simulation:
6-hourly NAAPS China Simulation 31 December - 4 January
Lifting of dust on the 31st shows up in the lower-left panel: surface dust concentration) and the upper-left
panel (optical depth, green shades). Note the plume of dust shooting northward in the final days of the loop.
6-hourly comparison of NAAPS, TOMS AI, SeaWiFS, and surface observations
for 31 December - 4 January
In this blowup, you can see the signal in the TOMS AI and surface observations.
The event appears on the 1st, heads quickly east on the 2nd, then SE on the 3rd and 4th.
The model splits the event into a zonal northern part (westward moving) and
a more circular southern part (SE moving).
These split is also seen in the TOMS images and in the
SeaWIFS for Yellow Sea for 31 December - 4 January.
Korea and Japan appear to be particularly hard hit on the 2nd at
06Z
and
12Z.
(Note: TOMS is available once daily, so it is updated every fourth frame.)
A pall of haze over the North China Plain on the 30th and 31st, is replaced by dust on the 1st.
Dust is seen streaming off the continent as far north as Vladivostok, out over the Sea of Japan on the 2nd.
The water clouds over the Sea of Japan are typical of cold air outbreaks.
The eastward flow of dust persists on the 3rd and is seen east of Japan.