Domains of Maritime Circulation
Oceanic masses and rivers are the two major components of maritime circulation. Oceanic masses account for 71% of the terrestrial surface. The four major oceans relevant to maritime circulation are: the Pacific (165 millions square km), the Atlantic (82 million square km), Indian (73 million square km) and the Mediterranean (2.5 million square km). Although the Pacific is by far the largest ocean, it is not the most significant as far as maritime circulation is concerned. It supports about 15% of the global maritime trade and only a small portion of it is used for commercial transportation purposes. The northernmost parts of the Atlantic as well as the southernmost parts of the Atlantic, Indian and Pacific oceans are not much used mainly because of hazardous conditions (mainly ice) and their remoteness to the centers of economic activity.
Even if maritime transportation has experienced remarkable improvements in its safety and reliability, maritime routes are still hindered by dominant winds, currents and general weather patterns. The North Atlantic and the North Pacific (50 to 60 degrees north) are subject to heavy wave activity during the winter that sometimes impairs navigation, and may cause ships to follow routes at lower latitudes, thereby increasing the route lengths. During the summer monsoon season (April to October), navigation may become more hazardous on the Indian Ocean and the South China Sea.
Rivers may not be useful for commercial navigation if their orientations do not correspond to the directions of transport demand. Thus, many of the major rivers of Russia flow north-south, while the main trade and passenger flows are east-west. Shallow draught and extensive obstacles, such as rapids, may also limit navigation. However, many rivers, such as the Rhine or the Chang Jiang, are significant arteries for water transport because they provide access from the oceans to inland markets. Geographically, maritime activities can be divided in two major categories: