Q.What is salinity of sea water?
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Start your 14-day free trial to unlock the full solution →Salinity is the total amount of dissolved salts in sea water, usually measured in grams per kilogram (parts per thousand), and it is the single most important chemical property of the ocean.
Think of sea water not as plain water with a pinch of salt, but as a complex chemical broth. Every litre of ocean water carries roughly 35 grams of dissolved substances — mostly sodium and chloride, but also magnesium, calcium, potassium, and a host of trace elements. Salinity is simply the measure of that total dissolved salt content. Oceanographers express it as parts per thousand (‰), so normal open-ocean water has a salinity of about 35‰, meaning 35 grams of salt per 1,000 grams of water.
The idea is straightforward, but the practice is subtle. Salinity isn't about tasting the water or watching it evaporate; it's a precise scientific quantity. When we say the ocean is salty, we're really saying that dissolved ions — charged particles from weathered rocks on land, carried by rivers into the sea — have accumulated over millions of years. The ocean is Earth's great salt sink, and salinity is the ledger of that accumulation.
What makes salinity fascinating is that it isn't uniform. The open ocean averages around 35‰, but that number shifts with geography and climate. Near the equator, heavy rainfall and river discharge dilute the surface water, pulling salinity down. In the subtropics, where evaporation outpaces precipitation, salinity climbs — the Red Sea and Persian Gulf, for instance, are famously saltier than the global average. At the poles, melting ice adds fresh water, lowering salinity again. So salinity is a dynamic map, not a fixed number.
The salt in the sea isn't just table salt (sodium chloride). It's a mixture of many dissolved compounds, though sodium and chloride together make up about 85% of the total dissolved solids.
The processes that change salinity are beautifully simple in principle. Evaporation removes pure water, leaving salts behind — so salinity rises. Precipitation, river runoff, and melting ice add fresh water — so salinity falls. Freezing of sea water also concentrates the remaining liquid, because ice crystals exclude salt. These are the four great movers of salinity: evaporation, precipitation, runoff, and freezing. In the deep ocean, away from these surface effects, salinity is remarkably stable, hovering near 34.5‰ to 35‰ almost everywhere. …
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