Sleet is a form of frozen precipitation consisting of ice pellets. It forms when snowflakes melt as they fall through a relatively warm layer of air and then refreeze as they pass through a subsequent deep layer of sub-freezing air near the ground. The characteristics of sleet pellets are:
They are typically small, translucent or transparent ice pellets.
They usually bounce when hitting the ground or other hard surfaces and make a distinctive sound.
Regarding size:
Sleet pellets are generally defined as being 5 mm (0.2 inches) or less in diameter.
Some sources may specify a lower limit, but often the distinction is made from hail, which is larger.
Option (a) "Less than 1 mm in diameter" might describe very small ice pellets, but the typical range extends larger.
Option (b) "Between 1 mm and 5 mm in diameter" is a reasonable and commonly cited range for sleet. Many definitions consider sleet to be ice pellets specifically 5mm or less.
Option (c) "Between 5 mm and 10 mm in diameter" and (d) "Greater than 10 mm in diameter" would typically classify the precipitation as hail. Hailstones are formed by a different process (accretion of supercooled water droplets onto an ice nucleus within strong updrafts of thunderstorms) and can be much larger.
Therefore, the size range of 1 mm to 5 mm is appropriate for sleet. \[ \boxed{\text{Between 1 mm and 5 mm in diameter}} \]
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