Answer:
The answer is 12.5 m/s
v=the square root of 2 x(gh)
or v = the square root of 2 x (9.8 x 8)
Explanation:
until he stops to talk to his neighbor, what is his average velocity? (Round your answer to the nearest tenth of a meter
per second.)
Ben's average velocity is m/s.
Answer:
I'm terrible at explaining so here's a screenshot
- Ripper
Explanation:
destructive
negligible
interference is not involved in the creation of beats
Answer: constructive
Explanation:
Two waves having slightly different frequencies when interfere constructively produce beats. Superposition of these two waves results in addition of amplitudes of the two waves. The amplitude of the resultant wave vibrates or beats.
Beat frequency is given by the absolute difference between the frequencies of the two waves.
b = |f₂ - f₁| = f₂ - f₁ or f₂ + f₁
B.) 40 feet
C.) 42 feet
D.) 45 feet
Answer:
The height of the ball when it hits t = 3 seconds will be 42 feet.
Explanation:
The user above me provides a very helpful explanation, so I am only writing this in his/her/their honor for his/her/their work :D
h = -16t² + 60t + 6
h = (-16)(3 s)² + (60)(3) + 6 = 42
ocean floor
ocean surface
thermocline
Deep ocean currents primarily flow along the ocean floor, driven by variations in water density. The halocline and thermocline are transitional layers in the ocean, but do not direct deep current flow.
Deep currents in the ocean predominantly flow along the ocean floor. These are also known as deep-ocean or abyssal currents. Unlike surface currents, which are mainly driven by wind, deep ocean currents are driven by variations in water density, which involves factors such as differences in temperature and salinity. The halocline and thermocline refer to transitional layers within the ocean where salinity and temperature change rapidly, respectively. However, they do not necessarily direct the flow of deep currents.
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