Ocean and wind currents above the equator flow in a clockwise pattern, while those south of the equator flow in a counterclockwise pattern. But all the winds and currents meet at the equator and flow east to west forming the trade winds and equatorial currents.
Deserts can be found both in the interior of continents or along the coasts. Australia, Asia, Africa and a number of other continents have interior deserts. The Atacama Desert of South America and the Namib Desert of Africa are coastal deserts.
Western coasts of continents are usually colder because of the cold ocean currents that flow along them. These currents bring colder water from higher latitudes, lowering the overall temperature of the coastal areas. Additionally, the prevailing winds blowing from the west carry cool, moist air from the ocean, further contributing to the cooler temperatures along western coasts.
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Urban areas, river valleys, and coastal plains.
Cold water currents along the western coasts of continents tend to keep the coastal areas cooler compared to the eastern coasts. They can also result in upwelling of nutrient-rich waters, supporting diverse marine ecosystems and fisheries. These currents can also influence the climate by moderating temperatures and affecting local weather patterns.
Thorium is found in abundance along the western coast of India, particularly in the coastal regions of Kerala and Tamil Nadu. The Monazite sands along this coastline are rich in thorium deposits.
The Western Ghats separate the Deccan Plateau from the coastal areas along the Arabian Sea, while the Eastern Ghats separate the Deccan Plateau from the coastal areas along the Bay of Bengal in India. These mountain ranges run parallel to the western and eastern coasts, respectively, and influence the climate and ecology of the regions they divide.
Yes, waves are a major force of erosion along coasts. The continuous impact of waves against the coastline wears away rock and sediment, leading to the erosion of coastal landforms. This erosion can result in the formation of cliffs, sea caves, and other coastal features.
The western coasts of continents tend to be warmer than the eastern coasts because of ocean currents. In the Northern Hemisphere, warm ocean currents move from the equator towards the poles along western coastlines, raising temperatures. Meanwhile, cold ocean currents flow from the poles towards the equator along eastern coastlines, bringing cooler temperatures.
The western coastal areas of Peru are deserts primarily due to the cold Humboldt Current, which flows along the coast and cools the air, reducing its moisture-holding capacity. Additionally, the Andes Mountains block moist air from reaching the coast, creating a rain shadow effect that further limits precipitation. These climatic conditions result in arid landscapes characterized by minimal rainfall and desert vegetation.
because the ocean currents circulate heat as well as moisture along the coasts, therefore, all of the major deserts that we see, are well away from the major oceans
Brown pelicans live along the southern and western sea coasts of North America.