Salinity and temperature are interconnected in aquatic environments, as both factors influence water density and circulation. Generally, warmer water can hold more dissolved salts, leading to higher salinity levels in warmer regions. Conversely, as temperature decreases, water becomes denser and can lead to lower salinity, especially in polar regions where freshwater from melting ice can dilute seawater. However, the relationship can vary based on specific environmental conditions and locations.
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