THEY ARE THE MOST COMMON CLOUD, THEY ARE THIN AND WISPY

MID LEVEL CLOUDS AND NORMALLY APPEAR AS GRAY PUFFY MASSES

FORM A DARK GRAY, WET LOOKING LAYER

ASSOCIATED WITH HEAVY RAIN SNOW HAIL AND LIGHTING, THE ANVIL POINTS TO THE WAY ITS GOING

CONDENSED TAIL LEFT BEHIND JET AIRCRAFTS, DUE TO JET EXHAUST

APPEAR LIKE SMALL ROUNDED WHITE PUFFS IN LONG ROWS, INDICATING FAIR BUT COLD WEATHER

GRAY OR BLUE-GRAY MID LEVEL CLOUDS COMPOSED OF ICE CRYSTALS

ARE UNIFORM GRAYISH CLOUDS THAT OFTEN COVER THE ENTIRE SKY

RAIN RARELY OCCURS, HOWEVER THEY CAN TURN INTO NIMBOSTRATUS CLOUDS

BASE OF A CUMULONIMBUS CLOUD AND FROM WHICH TORNADOES SOMETIMES FORM FROM

LOW HORIZONTAL CLOUD FORMATION, APPEARING AS AN ACCESSORY TO A CUMULONIMBUS

SMALL RAGGED CLOUD FRAGMENTS THAT ARE USUALLY FOUND UNDER AN AMBIENT CLOUD BASE

LOW HANGING BULGES THAT DROP FROM CUMULONIMBUS CLOUDS

IS COMPOSED OF BILLIONS OF TINY WATER DROPLETS FLOATING IN THE AIR.

IS A LARGE GAP USUALLY CIRCULAR OR ELLIPTICAL THAT APPEAR IN CIRROCUMULUS OR ALTOCUMULUS

WAVE WIND PATTERN CREATED BY MOUNTAINS THAT LOOK LIKE DISCS OR SAUCERS