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low rates of evaporation.
an area with high rates of evaporation
If the salinity of surface ocean water is high in a particular place, it suggests that there is high evaporation rates in that area. As water evaporates, it leaves behind salt, increasing the salinity of the remaining water.
All deserts have low precipitation and high evaporation rates.
The highest salinity levels are typically found in enclosed bodies of water with high evaporation rates, such as the Dead Sea and the Great Salt Lake. These areas have limited freshwater inflow and high concentrations of dissolved salts, resulting in extremely high salinity levels.
deserts
Both have low precipitation and high evaporation rates.
The deserts biome is an example where evaporation rates often exceed precipitation rates. These regions receive limited rainfall, resulting in higher evaporation due to the intense heat and lack of moisture in the air.
High evaporation rates in the subtropics typically lead to increased salinity in surface ocean waters, not lower. As water evaporates, salts and other dissolved substances remain, concentrating in the remaining water. However, in some regions where precipitation or river influx balances or exceeds evaporation, salinity may be moderated. Overall, the general trend in subtropical regions is for evaporation to increase salinity.
The most evaporation occurs in warm regions with high temperatures and abundant sunlight. Areas like deserts, tropical rainforests, and near large bodies of water experience high rates of evaporation due to the conditions that favor the process.
RAiSE diVidENd RAtES. . .A+
Deserts and tundras receive the same amount of rainfall, but they differ in temperature and evaporation rates. Deserts are hot and experience high rates of evaporation, leading to arid conditions, whereas tundras are cold with lower evaporation rates, resulting in waterlogged conditions. This difference in climate impacts the vegetation and overall landscape of each biome.