Fast-moving, cool air masses often sweep from east to west across North Africa in the winter, sending surges of dry air over the Atlantic Ocean. When this dry air encounters moister and more stable air masses over the water, the clash can yield distinctive and beautiful patterns in the clouds.
On February 18, 2013, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured this view of a thin layer of marine stratocumulus clouds off the coast of western Africa.
The air mass moving west pushed a wave of cool, dry air ahead of it, much like the bow wave of water that moves ahead of a boat in calm water. When that wave of air met the mass of moist air over the ocean, it pushed the moist air up. As that air rose, it cooled at the peak of the wave, forming a linear wave cloud. As the wave propagated forward, it rose to a slightly lower peak, and so on and so forth, until it eventually dissipated. The series of clouds that formed at the high-altitude peaks produced the rippling pattern seen in the clouds. This type of atmospheric disturbance is known as an undular bore. The air to the east of the bore is almost completely cloud-free because dry air would have eroded any clouds in that area.
The Cape Verde islands had their own noticeable effect on the clouds to the south. Air masses passing over the volcanic islands split into streams, then come back together—a process that creates off-centered areas of low pressure like whirlpools. These low-pressure areas produce thread-like swirls in the clouds downstream of the islands. These are known as Von Karman vortices. The cloud layer is fairly thin in this image, so the vortices are less distinct than they are in other satellite images of the phenomenon.
The island itself is almost too small see in this image, but it serves as the starting point for the clouds that flow toward the northeast in a giant V shape. Amsterdam Island is a volcanic summit, the northernmost volcano on the Antarctic tectonic plate.