Consider an area on the earth's surface. On the sides which face the wind, air will flow into the area, while on the other sides air will flow out. If, however, the wind is not uniform, more air may flow in than flows out, and the amount of air in the area will tend to increase: this process is called convergence. The air cannot, however, go on accumulating and excess will have to flow out over the top, thus leading to a rising air current, and perhaps to clouds and rain. The contrary case is called divergence.