As a general rule, sound frequencies lower than 10 Hz tend to penetrate deep into the seabed, whereas frequencies above 1 MHz are absorbed very quickly by the water, limiting their useful range. This frequency-dependent absorption necessitates careful selection of operating frequencies for different applications: low frequencies for long-range communication and detection (e.g., SONAR, whale monitoring), and high frequencies for high-resolution imaging of nearby objects (e.g., medical ultrasound, fish finders). Additionally, seasonal and regional variations in water temperature, salinity, and suspended particle concentration can significantly alter sound propagation characteristics, requiring adaptive approaches in underwater acoustic systems.