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Density is usually calculated using a mathematical function of temperature, salinity, and pressure, sometimes called an equation of state. For many years the internationally accepted...
- Ocean Acidification
[CO 3 2-] saturation is a weak function of temperature and...
- Ocean Acidification
1. Salinity, along with temperature, determines the density of seawater, and hence its vertical flow patterns in thermohaline circulation. 2. Salinity records the physical processes affecting a water mass when it was last at the surface. a. precipitation/evaporation – salts excluded from vapor b. freezing/thawing – salts excluded from ice 3.
T-S diagrams are graphic representations of two main properties of water masses: Temperature and salinity. Usually, the salinity is plotted on the X-axis and the temperature on the Y-axis. Those two properties are the main factors of a third one, the density. The latter is thus also represented on the graph by addition of curves of equal ...
A T-S diagram shows lines of equal density, or isopycnals, for various combinations of temperature and salinity (Figure 9.8.3). You can then plot the values of temperature and salinity on the diagram, and use their point of intersection to calculate the density of the water.
15 Φεβ 2021 · Monthly Isopycnal & Mixed-layer Ocean Climatology (MIMOC): Animations show pycnocline (temperature and salinity) data of different parts of the world. The NASA animations provide views of how salinity, temperature, and density change over the course of a year.
A T-S diagram is a graph showing the relationship between temperature and salinity as observed together at, for example, specified depths in a water column. Isopleths of constant density are often also drawn on the same diagram as a useful additional interpretation aid.
9 Δεκ 2021 · As the density of seawater, which controls the ocean circulation and distributions of various biogeochemical tracers, is determined by both temperature and salinity, it is important to understand the linkage between the two variables.
