HIGH CLOUDS HIGH LEVEL TYPE THE HIGH LEVEL ETAGE CIRROSTRATUS ICE CRYSTALS PRESENT BRIGHT WHITE APPEARANCE EXCEPT SUNRISE THE REFLECTION THE CLOUD BASES ORANGE YELLOW SUNLIGHT SCATTERED THE ATMOSPHERE THE MOST BEAUTIFUL CLOUD CIRRUS DETACHED WHITE PATCHES FIBROUS CIRRUS CLOUDS ALMOST CRYSTALS GENERAL VERY SMALL SPARSENESS DENSE PATCHES TUFTS LARGE ENOUGH ACQUIRE TERMINAL VELOCITY TRAILS VERTICAL EXTENT DISTINGUISHED THE ABSENCE CLOUD ELEMENTS DISCONTINUOUS STRUCTURE CONTINUOUS SHEETS LAYER SHADING ELEMENTS MERGED MORE OR LESS WIDTH LESS THAN ONE SMOOTH DO NOT COLLECTIVELY GREATER ALTOCUMULUS DEGREE AN ANGLE ABOVE THE HORIZON PRESENTS WHITISH VEIL TOTALLY COVERING GENERALLY HALO SMALLNESS FACT MODERATE ACCOUNT THE OUTLINE THE SUN ALTOSTRATUS THINNESS SHOW HALO PHENOMENA NEVER ENOUGH PREVENT ON THE GROUND CASTING SHADOWS WHEN THE SUN COPYRIGHT TEXAS METEOROLOGY DEPARTMENT MARION