Ei Nino refers to the change in climate across the Pacific Ocean. Although it normally occurs every two to seven years. The Ei Nino phenomenon has taken place more often in the past three decades. Ei Nino have an effect on climate and weather around the globe. A single phase can last for about one and a half years and is often followed by an opposite climate pattern called, La Nina.
The term Ei Nino means “Christ child” and was first used by Peruvian. They discovered that in some years there were fewer fish around Christmas time.
In normal years, cold water comes from the Antarctic region and flows along the eastern coast of South America. A high-pressure area develops, warms the water on the surface and pushes it in a westward direction. In the western Pacific, the air becomes warmer. A low-pressure area forms and leads to tropical rainfall in Indonesia and northern Australia. Because of this climate cycle cold water rises from deeper regions of the South American coast to replace the warmer water on the surface. This part of the ocean belongs to the richest fishing regions of the world because fish can find more than enough to the richest fishing regions of the world because fish can find more than enough food.
During a typical Ei Nino phase, the air pressure is higher than normal in the western Pacific and lower than normal on the water does not have the nutrients that fish need to survive. They stay in the colder regions near the Antarctic. Other animals that feed on fish to fish also suffer so that the whole food chain is affected. In addition, more rainfall comes to a normally dry area and occasional flooding also occurs. On the other side, eastern Australia and Indonesia are hit by unusual periods of dry weather. Climate experts have seen more tropical storms in the central Pacific during an Ei Nino year.
Ei Nino does not only affect the climate of the Pacific regions but has an impact on global climate. Climatologists claim that frequent occurrences of Ei Nino are another sign of global warming.
Ei Nino refers to the change in climate across the Pacific Ocean. Although it normally occurs every two to seven years. The Ei Nino phenomenon has taken place more often in the past three decades. Ei Nino have an effect on climate and weather around the globe. A single phase can last for about one and a half years and is often followed by an opposite climate pattern called, La Nina.The term Ei Nino means “Christ child” and was first used by Peruvian. They discovered that in some years there were fewer fish around Christmas time.In normal years, cold water comes from the Antarctic region and flows along the eastern coast of South America. A high-pressure area develops, warms the water on the surface and pushes it in a westward direction. In the western Pacific, the air becomes warmer. A low-pressure area forms and leads to tropical rainfall in Indonesia and northern Australia. Because of this climate cycle cold water rises from deeper regions of the South American coast to replace the warmer water on the surface. This part of the ocean belongs to the richest fishing regions of the world because fish can find more than enough to the richest fishing regions of the world because fish can find more than enough food.During a typical Ei Nino phase, the air pressure is higher than normal in the western Pacific and lower than normal on the water does not have the nutrients that fish need to survive. They stay in the colder regions near the Antarctic. Other animals that feed on fish to fish also suffer so that the whole food chain is affected. In addition, more rainfall comes to a normally dry area and occasional flooding also occurs. On the other side, eastern Australia and Indonesia are hit by unusual periods of dry weather. Climate experts have seen more tropical storms in the central Pacific during an Ei Nino year.Ei Nino does not only affect the climate of the Pacific regions but has an impact on global climate. Climatologists claim that frequent occurrences of Ei Nino are another sign of global warming.
การแปล กรุณารอสักครู่..
