Ignoring air resistance . . .H = 1/2 G t2t = sqrt(2H/G) = sqrt(2 x 363 / 32.2) = 4.75 seconds (rounded)
If the ball was dropped from a roof and hit the ground 3.03 seconds later, then when it hit the groundits velocity was 29.694 meters (97.42 feet) per second (rounded) downward.
a radar uses a "parabolic" dish to capture the radio waves and because the shape is concave the waves hit the centre of the dish, the receiver is placed away from the centres facing the dish where the waves are reflected to it. The classic example is satellite dish receivers
On Earth gravity equals 9.8 m/s^2. If you multiply that by 8 seconds you get: 78.4m/s
Speed / Distance=Time 2283.6211MPH/60KM= 61.25219859267292 seconds
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The number of times waves hit the shore can vary depending on factors such as wave frequency, amplitude, and shoreline structure. In general, waves continuously hit the shore in a rhythmic pattern due to the movement of water caused by wind and tides.
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It depends on the wind direction. The waves may be straight on to the shore, or hit the shore at an angle.
Waves hit the shore many times per minute, but it varies so greatly. The wind changing can result in a change of this number. Any storms out in the ocean can change it as well.
Long-shore currents are generated when waves approach the coast at an angle, causing water to move parallel to the shore. When waves hit the shore head on, there is less tendency for water to move laterally along the coast, resulting in weaker or non-existent long-shore currents.
Long-shore currents don't form in places where waves hit the shore head-on because the sand is moving in a zigzag pattern, making it at an angle.
When waves hit the shore, energy is transferred to the beach. This energy causes erosion by moving and depositing sand along the coast. Additionally, wave action can also bring nutrients and minerals to the beach, which can support the local ecosystem.
Longshore currents are driven by the angle at which waves approach the shore. When waves hit the shore head-on, rather than at an angle, there is no net transport of water along the shoreline to generate a longshore current. The wave energy is dissipated directly onto the shore, preventing the development of a longshore current.
people for fish hit the correl and the waves cary it to the shore and beach it
Large pebbles near the shore are typically deposited by wave action. As waves hit the shore, they can pick up and transport larger rocks and pebbles, eventually depositing them closer to the shore. The size of the pebbles also helps to protect the shore from erosion by dissipating the energy of the waves.
1 wave / 8 seconds = 0.125 waves per second