Ocean - Oceanic Climate Variables

This page illustrates a subset of the 50 Essential Climate Variables identified by the Global Climate Observing System (GCOS) for worldwide monitoring. GCOS is an international network of people and observing systems that gather data for monitoring global climate. Panels of experts helped identify which climate observations should be made on an ongoing basis, and agreed upon principles and guidelines for the best ways to make them. You can read more about how essential climate variables are used to support climate research and policy and find links to vetted data sets on the Global Observing Systems Information Center (GOSIC) site »

 

Surface Ocean Variables


Sea Surface Temperature

Aqua satellite

Aqua satellite
Image source: NASA

Sea Surface Temperature (SST) is defined as the skin temperature (top 2 mm) of the ocean. Historically, ships measured sea surface temperature directly, and later, buoys were fitted with thermometers to check the temperature of surface waters. Instruments on satellites now remotely measure SST for the whole world every day.

More information: Sea Surface Temperature - NASA
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Ocean Color

Aqua satellite

Aqua satellite
Image source: NASA

The color of the ocean can be strongly influenced by the presence of microscopic algae (phytoplankton) that contain chlorophyll. When populations of phytoplankton have the right combination of nutrients, sunlight, and water temperatures, they can explode into "blooms" large enough to be visible from space. Additionally, phenomena such as suspended sediments and solutions of dissolved natural materials can affect ocean color. Instruments on satellites measure ocean color from space.

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Phytoplankton

plankton sample net

Plankton sample net
Image source: NASA

Phytoplankton are tiny plants (algae) that float freely in the ocean. They are often accompanied by zooplankton, or microscopic animals. These microscopic organisms form the base of the global oceanic food chain. Through photosynthesis, scientists estimate that marine phytoplankton produce about half of the world's oxygen. Scientists measure phytoplankton abundance by straining staining marine water samples through very fine mesh nets.

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Sea State

Wave crashing

Wave crashing over vessel in a large swell.
Image source: NOAA

Sea state is the general condition of the sea with respect to the wind, swell, and waves at a given time and location. Skilled observers, instruments on ocean buoys, or satellite instruments can measure sea state. The Douglas Sea Scale is the 10-point classification system for sea state.

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Sea Ice

IceSat satellite

IceSat satellite
Image source: NASA

Sea ice is frozen seawater that forms at the ocean's surface in the polar regions. As salty ocean water freezes, some of the salt is expelled, and the brine below it becomes saltier and more dense. Sea ice extent is defined as the area where at least 15% of the surface is covered with ice. Sea ice extent changes with the seasons in both hemispheres. Satellite instruments measure sea ice extent. Submarines and remotely operated vehicles are used to monitor the thickness of sea ice.

More information: Sea Ice monitoring - NOAA
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Sea Surface Salinity

Argo float

Argo float being deployed
Image source: ARGO

Ocean salinity is the mass of salt per unit volume of water: it is normally reported in units of grams of salt per 1000 grams of water. Changes in salinity are due variations in the rate of evaporation and amount of precipitation over the ocean. River runoff and ice melt also influence ocean salinity by adding fresh water. Salinity affects the density of seawater and therefore, along with temperature, is a major controller of ocean circulation. Historically, ships gathered samples of water to measure salinity, or instruments on buoys measured salinity by passing a current through the water. Now, instruments on satellites can measure salinity remotely.

More information: Sea Surface Salinity - NASA
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Sea Surface Height

Jason 2 satellite

Artist's rendition of Jason 2 satellite
Image source: Wikipedia

Just as Earth's land has high and low areas, the surface of the sea is not flat either. Factors that cause "hills and valleys" on the ocean's surface include gravity, tides, ocean temperatures, winds, and currents. Satellite instruments use sophisticated mathematical equations to make precise measurements of the height of the sea's surface. Monitoring sea surface height is useful for understanding weather and climate phenomena such as El Niño events.

More information: Sea Surface Height - NASA
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Ocean Currents

Ocean current bouy

Ocean current bouy being deployed
Image source: NOAA

Water in the ocean is constantly in motion from waves, tides, and currents. Ocean currents are the result of winds, density differences, and and the rotation of planet. The simplest method of measuring a surface ocean current is to use a float and record the time it takes to travel a given distance. Observers on ships once used this method to measure ocean currents. Today, instruments on drifting and anchored buoys measure the speed of ocean currents. Satellite instruments are also used to measure the motion of the ocean.

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Sub-Surface Ocean Variables


Atlas bouy

Atlas bouy
Image source: NOAA

Temperature, Ocean Heat Content and Flux, CO2, Winds, Currents, Sea Level, Sea Ice Extent

The global ocean has an enormous capacity to store and distribute heat around the planet. The high heat capacity of water helps to moderate swings in our climate on both long- and short-term time scales. Differences in temperature and density of water in the deep ocean are two key properties driving ocean currents. Sub-surface ocean temperature, salinity, and stored CO2 can affect the health of ecosystems and fisheries. Drifters, moored ocean buoys, and instruments on ships are the primary methods used to track changes in sub-surface ocean temperatures.

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