To calculate the electric field of a sphere we can use Gaussian law
Ф = ∫ E. dA = / ε₀
In this case we must use a Gaussian surface of spherical shape, since the radii of the sphere and the electric field line have been parallel, consequently the scalar product is reduced to an algebraic product.
The error of a sphere is
A = 4π π r²
E (4π r³) = / εo (1)
to find the charge inside the sera we use the concept of density
Ocean currents act as conveyer belts of warm and cold water, sending heat toward the polar regions and helping tropical areas cool off, thus influencing both weather and climate.