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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />- 117 - <br /> <br /> <br />4.2.15 Capped Columns (CPla) <br /> <br />Our aircraft observations indicate that capped columns usually form by <br /> <br />cold region columns falling through a region of active plate growth. The <br /> <br />columnar portions of the crystals are typical cold region columns with length <br /> <br />to width ratios of about three. Ground observations also indicated that the <br /> <br />columnar part of the crystal was stubby. Air observations shololed these <br /> <br />crystals had lengths up to 800 lJm. The end plates were often only partially <br /> <br />replicated. <br /> <br />The nature of the capped part of the column was variable. Usually both <br /> <br />ends were capped, but in some cases only one end of the column was capped. The <br /> <br /> <br />end plates were not, in general, equal in diameter. Occasionally, riminp was <br /> <br /> <br />observed on these crystals and often the end plates collected other particles, <br /> <br /> <br />both planar and columnar types. The accretion of particles at the end plates <br /> <br /> <br />indicates that the column changed its original orientation to fall with the <br /> <br /> <br />larger end plate leading. According to Ono (1969) this occurs when the <br /> <br /> <br />diameter of the end plate exceeds the length of the column. <br /> <br /> <br />The air observations indicated that capped columns were usually present <br /> <br /> <br />as individual crystals, althOUgh occasionally they were observed in aggregates. <br /> <br /> <br />However, at the ground, the capped columns were usually parts of aggregates. <br /> <br />Capped columns were observed to suffer fragmentation in the air and this <br /> <br /> <br />usually involved the end plates. <br /> <br /> <br />4.2.16 Frozen Drops <br /> <br /> <br />Air and ground observations indicated that frozen drops seldom made a <br /> <br /> <br />large contribution to the total concentration of ice particles in the air. <br /> <br /> <br />Those which were present were generally spherical in shape, although sometimes <br />