It takes the average reader 15 hours and 18 minutes to read Ocean Circulation and Climate by Nikolai Maximenko
Assuming a reading speed of 250 words per minute. Learn more
This chapter summarizes the history of and recent progress in observations of surface circulation of the ocean. The description is biased toward Lagrangian drifting buoys and satellite altimetry that, in the authors’ opinion, have revolutionized our understanding of ocean surface currents by providing a high resolution, continuous global view of mesoscale ocean “weather.” We outline the current state of the observing system and characterize geostrophic surface circulation, Ekman currents, and effects of centrifugal force and nonlinear interaction between geostrophic and Ekman currents. This general description is complemented by regional examples, detailing processes in the California Current System, off Senegal, and the Kuroshio interaction with the East and South China Seas. Applications to various tasks, in which surface currents play important role, are illustrated by model simulations of motions of marine debris, including debris generated by the 2011 tsunami in Japan. The chapter concludes with a brief discussion of the next tasks needed to improve understanding of the dynamics of the surface ocean circulation.
Ocean Circulation and Climate by Nikolai Maximenko is 904 pages long, and a total of 229,616 words.
This makes it 305% the length of the average book. It also has 281% more words than the average book.
The average oral reading speed is 183 words per minute. This means it takes 20 hours and 54 minutes to read Ocean Circulation and Climate aloud.
Ocean Circulation and Climate is suitable for students ages 12 and up.
Note that there may be other factors that effect this rating besides length that are not factored in on this page. This may include things like complex language or sensitive topics not suitable for students of certain ages.
When deciding what to show young students always use your best judgement and consult a professional.
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