Oceanography is also commonly referred to as marine science or marine science. Studying the ocean and trying to understand the process of the ocean is one area of science. Research conducted by oceanographers is used by government and industry. Animals and plants found in the sea are used for medical research. These researchers are trying to discover new food supplies made from sea animals and plants. Oceanography has many fields. They include: Ocean physics: It studies the physical properties of the ocean.
Oceanographers are studying the movement of water in large and small water bodies. Oceanographers can work in a variety of fields such as mining, shipping, fishing, coastal construction, weather forecasting. They may study pollution patterns, renewable energy and climate change. When oceanographers become specialized, they can be marine geologists, marine chemists, marine physicists or marine biologists. This profession requires a deep understanding of science and mathematics. Ocean engineering is a challenging task for those who like mathematics at a high level and prefer to work on the water surface rather than working underwater. The marine engineer is responsible for keeping the engine of the ship moving. They are focused on electric, hydraulic, pneumatic pumps, pipes and fuels, air conditioning and refrigeration systems. This profession involves dealing with complex mechanical systems
Rudiman was born in Washington, DC in 1943. He has a doctorate in marine geology at Columbia University (1969). After working at Columbia 's US Navy Ocean Bureau and Lamont - Doherty Earth Observatory, I moved to Virginia University in 1991 and retired in 2001 after remaining career. Professor emeritus of the department. Department of Environmental Science, Virginia University. Rudiman 's special field is paleoclimatology. He is particularly famous for his two hypotheses. One is relatively early and the other is quite late. Initially, in the work done with his student Maureen Raymo and other people in the 1980's, he noted that the structural rise of the Himalayas and the Tibetan Plateau late in the Cenozoic (about 3 million years ago) I guessed that it caused a decrease. . Increase in chemical weathering