What is the Water Column: A Complete Breakdown

Have you ever dreamt of diving deep underneath the water where the marine splendors and aquatic enigmas await? Get ready for Brace yourselves for a deep-sea adventure as we untangle the mysterious riddle of the water column—a vertical maritime space teeming with life, enigmas, and wonders beneath the mighty tides!

Now the million-dollar question is: what is the water column? grab your snorkel, put on your wingsuit, and Let’s unravel the answer to this question by plunging deep into the sea! it’s going to be a splash-tastic adventure!

What is The Water Column: The Definition

In oceanography, the water column is a concept used to define the chemical and physical attributes of seawater at various depths for a specific geographical point. While the chemical characteristics can be dissolved nutrient salts, or oxygen and pH levels, salinity, temperature, and light penetration of seawater fall under the physical characteristics. The water column helps you get a complete view of the vertical profiles of these parameters at set points, within a water body.

From the well-lit water surface to the seafloor as deep as 11 km underwater – the water column can take you on a ride to the awe-inspiring underwater realm.

This habitat is still an enigma that entices ocean enthusiasts to take a deep plunge and unveil the unknowns it’s wrapping inside – and what if you get the chance to say hello to a mermaid?

Why Is Water Columns Studies Important

Do you want to dive deep into the different features of the blue oceans? Studying the water column can help.

This is because, with the water column study, you get a framework to describe the key physical and chemical makeup of the ocean at different depths. And we all know how these parameters regulate the lives of the marine organisms – our ocean pals.

Environmental conditions change at each layer of the water column. At the sunlit surface, living organisms can rely on photosynthesis. And as we go further, and darker, it gets colder – at great depths, temperature can be as low as 2°C and pressure as high as (1 bar per 10 m). Only underwater superstars like deep-Sea Anglerfish – who are capable of adapting to such a pressure-packed environment can survive here; for example deep-Sea Anglerfish.  Knowing these key gradients – pressure, temperature, and light is critical to deciphering the interconnection between the species living at different layers of the water column. It also facilitates research on biodiversity and marine ecosystems.

Again, the vertical structure of the water column has a profound impact on the key oceanographic processes – nutrient cycle, climate changes, thermohaline circulation and ocean currents.

  • The vertical structure of the water column determines how key nutrients -nitrogen, phosphorus, carbon, etc. will be available and distributed across the ocean path. The importance of these nutrients in the lives of our ocean buddies is beyond description.
  • Again, the vertical distribution of salinity and temperature in the water column, by generating density variation between the layers in the water column, drives thermohaline circulation. Simply put, it refers to the global oceanic overturning where salinity and temperature causes currents to move accordingly. It plays a critical role in determining climate patterns, heat and organism distribution and nutrient transport. Any change in the vertical structure of the water column can cause changes in density gradients, thus affecting the stability of these vital processes.

This is why a water column study is essential to understand how living organisms adapt to large-scale water circulation in the unending sea.

All this knowledge is critical to getting an in-depth insight into the dynamics of the marine ecosystem, preserving biodiversity, and keeping our marine buddies jumping in a swag in the whimsical aquatic environment!

Layers of the Water Column

The water column can be divided into five layers based on the physical and ecological factors:

Figure: Water Column layers

  • The sunlight zone (epipelagic): It is the ocean layer where sunlight reaches to support photosynthesis. A bustling community of aquatic life – from phytoplankton to sea mammals – thrives in this sunkissed ocean playground. The epipelagic zone extends from the sunlit surface to a depth of around 200 m (650 feet) underwater. Algae – one of the dwellers in this well-lit zone – supplies almost all maritime creatures with food. They are the ultimate kitchen king throwing party for sea creatures. Even better, algae also produce around 50% of the atmospheric oxygen. Organisms that live in the epipelagic zone may come into contact with the sea surface.
  • The Twilight zone (mesopelagic): The mesopelagic region starts from the point where the epipelagic zone ends and expands down to the point where water penetrates very low amounts of sunlight. Larger than the pelagic zone, the mesopelagic zone can reach as deep as 3,300 feet underwater. The mesopelagic zone is much larger than the epipelagic one. A swarming habitat of sea life, mesopelagic zone is where most hippest vertebras of the world, such as the mighty bristlemouth fish, throw underwater salad parties! You will also find invertebrates and other fishes in this zone but they move to the epipelagic region to feed at night when darkness shrouds the underwater environment. In the dark depths of the mesopelagic zone unfold the larger-than-life mysteries that the ocean conceals.
  • The Midnight Zone (bathypelagic): Down to the mesopelagic zone is the bathypelagic zone that expands down to 13,100 feet. The largest ecosystem on the mother planet, the bathypelagic region is 15 times the extent of the epipelagic zone and is completely out of reach of sunlight. Organisms such as jellyfish, cephalopods, etc., are adapted to withstand extreme cold, and pressure. However, some organisms in this zone light up the underwater surroundings using bioluminescence to hunt their prey or find a mate.
  • The Abyssal Zone (abyssopelagic): The abyssopelagic zone better known as the abyss can be found between 9,842 to 21,325 feet underneath seawater. One of the darkest layers in the water column, in the abyss, sunlight doesn’t penetrate at all. s. Deep-sea corals, giant isopods, and grenadier fish are found in this zone. It’s indeed a deep-ocean masquerade where grenadiers, giant isopods or deep-sea corals thrive, defying the extreme environment.
  • Hadopelagic Zone (trenches): The deepest layer in the water column that can be only in certain places. The depth of the hadal zone can range between 6000 to 36000 feet.

Human Impact on the Water Column

Different anthropogenic causes are degrading the quality of seawater. For example:

  • Pollution: Pollutants generated by anthropogenic causes – municipality runoff, agricultural runoff, industrial wastes, etc., can significantly degrade marine ecosystems. For example if not contained properly, harmful industrial solvents such as methylene chloride, tetrachloroethane, trichloroethene, etc., can run off to the water. These weighty, long chain organic compounds are insoluble and hence, accumulate in the surfaces under the sea. Needless to mention, some of these chemicals are better known for causing cancer in humans. so they sink to an impermeable bottom layer in the ground (like bedrock) and accumulate. Many solvents are known cancer-causing compounds.
  • Overfishing: According to studies, we have already eaten up 90% of the world’s stock of top marine predators – tuna, shark, swordfish, etc. These maritime creatures are already at the verge of extinction. Depleting these fishes can affect the entire ecosystem and marine food web while also degrading habitats. Depletion of these predators means there would be significant change in the population of their prey. Overfishing also affects the population of phytoplankton and other organisms fish feast on. All these upset the balance in marine ecosystems, thereby affecting biodiversity, nutrient cycling and the world’s overall ecological health.
Patsy Todd