Ch 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.
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).
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.
The Bay of Fundy in Canada experiences the highest tides in the world, with a tidal range of 15-16 meters. This occurs due to the funnelling effect of the bay's shape and the resonance of water sloshing back and forth.
Tidal energy can be harnessed by building dams across estuaries. India has high potential for tidal energy in the Gulf of Khambhat, Gulf of Kutch, and the Sundarbans region.
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.
The West Wind Drift (Antarctic Circumpolar Current) is the only ocean current that flows completely around the globe without encountering any landmass barrier, driven by strong westerly winds.