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Figure 2: This Θ -S A diagram can be used to illustrate relationships between temperature, salinity, and density for different water masses.
- Ocean Acidification
When CO 2 dissolves in seawater to produce aqueous CO 2 (CO...
- Ocean Acidification
Definition. 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.
Two of the most important characteristics of seawater are temperature and salinity – together they control its density, which is the major factor governing the vertical movement of ocean waters.
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.
These example scripts create T-S diagrams based on global or CESM/POP-defined ocean basins employing a scattergram format with temperature on the ordinate (Y axis) and salinity on the abscissa (X axis).
A temperature-salinity (T-S) diagram is used to examine how temperature, salinity, and density change with depth, and to identify the vertical structure of the water column, including the water masses it contains. Water temperature is on the y-axis, and salinity appears on the x-axis.
Temperature and salinity control seawater's density. The weight of seawater determines whether it sinks or floats, helping to drive deep ocean circulation. At the sea surface, wind and waves move seawater — and the heat it carries — around our globe.
