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NCERTGeographyCh 14: Movements of Ocean Water
GeographyClass 11 · Fundamentals of Physical Geography
14

Movements of Ocean Water

This chapter anchors core physical oceanography concepts on the gravitational, thermal, and Coriolis-driven mechanics of waves, tides, and global ocean currents frequently tested in climate and maritime transport dynamics.

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§ 1pp. Pages 119-1200/4 checked
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Waves

UPSC frequently tests wave characteristics such as wave height, wavelength, wave period, and wave frequency. It is vital to understand that waves do not move water across the ocean, but rather transfer energy. Aspirants must master the parameters of waves: wave height is the vertical distance from trough to crest, while wavelength is the horizontal distance between two successive crests or troughs. Skip purely descriptive poetic descriptions of wave beauty; focus strictly on physical properties and factors influencing wave size like wind speed, duration, and fetch. Trap: UPSC may confuse wave speed (measured in knots) with wave frequency (number of waves passing a point per second).

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4 PYQs from this section
§ 2pp. Pages 120-1220/7 checked
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Tides

This section is a major UPSC favorite. Focus on the combined gravitational pull of the Sun and Moon, along with centrifugal force, which creates two tidal bulges daily. Grasp the distinction between Spring Tides (syzygy alignment during Full and New Moon, leading to higher high tides and lower low tides) and Neap Tides (quadrature alignment, where gravitational forces of Sun and Moon counteract each other, occurring at first and third quarters). Understand semi-diurnal, diurnal, and mixed tides based on frequency, and how tidal bores function in estuaries like the Hooghly. Trap: UPSC may falsely state that centrifugal force plays no role in tide formation, or that spring tides only occur during equinoxes.

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§ 3pp. Pages 122-1260/7 checked
High yield

Ocean Currents

The most high-yield section of this chapter. You must master the distinction between primary forces (solar heating, gravity, Coriolis force, wind) and secondary forces (temperature and salinity differences) that drive ocean currents. Memorize the spatial distribution of cold currents (e.g., Humboldt, Canaries, Benguela, West Australian) and warm currents (e.g., Gulf Stream, Kuroshio, Brazilian, Agulhas). Understand the climatic impact of these currents, specifically how cold currents contribute to the formation of coastal deserts (e.g., Atacama, Namib) and how warm-cold current mixing zones create rich fishing grounds (e.g., Grand Banks of Newfoundland) but also pose navigational hazards due to dense fog. Skip nothing here; this is highly examinable.

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