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The strong winds whip up dust materials, eventually forming dust storms (Qian et al. 2002).
Locally, near-surface meteorological conditions and underlying surface conditions determine the availability of dust materials, the speed of surface friction wind, and the threshold wind speed for blowing up dust materials.
Paved roads, stabilized or treated (e.g., watered) surfaces with limited loose dust materials are the lowest emitting surfaces.
Local near-surface meteorological elements and underlying surface conditions also contribute to the emergence of dust storms by affecting the access to dust materials (Shao and Dong 2006).
Increased temperatures enhance photosynthesis, leading to more biomass accumulation, which increases surface roughness and the wind speed needed to blow up dust materials.
It is highly possible that some dust materials other than ices are responsible for the flat MIR extinction towards the GC and elsewhere.
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Mr. Brownlee (shown above flashing a victory sign upon the successful arrival of star dust material) makes his report in this one-hour special.
The dust charge depends on the grain sizes, plasma parameters and the dust material.
This is because with the same size, a porous grain contains less dust material than its solid counterpart.
This leads one to believe that the carrier should be a single sort of dust material with universal properties in various sources.
If this variation occurred, the dust deposition rate indicated by the 50 80 cm dust material in the dune could have been as high as 5 cm ka−1 for the period 25 16 ka.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com