Variation of "g" with height:
Consider the body which is at height h from the surface of earth whose radius is considered to be R .
Let the mass of earth be M .
so,
acceleration due to gravity acted on a body at surface of earth = GM / R 2
or, g = GM / R 2 ............ ... ... ... (i)
again,
acceleration due to gravity acted on a body at the height h above the surface of earth = GM / (R+h)2
or, g ' = GM / (R+h) 2 ... ... ... ... ... (ii)
Now, dividing (i) by (ii), we get,
g/g ' = (GM / R 2 ) / (GM / (R + h) 2 )
or, g/g ' = (GM x (R+h) 2 ) / (GM x R 2 )
or, g/g ' = (R+h) 2 / R 2
or, g/g ' = (R/R + h/R) 2
or, g/g ' = (1+h/R) 2
or g ' = g(1+h/R) -2
Now, expanding binomially, we get,
or, g ' = g(1- 2h/R)
Variation of g with depth:
Consider the body at the depth of x from the surface of earth whose mass is considered to be M and radius to be R .
But at this situation body will experience acceleration due to gravity only by that mass in which it is standing. Let that mass is considered to be M ' . Similarly radius will be (R-x).
Now, acceleration due to gravity at the surface of earth = GM / R 2
or, g = GM / R 2 ... ... ... ... ... ... ... ... (i)
Similarly, acceleration due to gravity below the depth of x from surface of earth = GM ' / (R-x) 2
or, g ' = GM ' / (R-x) 2 ... ... ... ... ... ... (ii)
Dividing (ii) by (i), we get,
g '/ g =( GM ' / (R-x) 2 ) / (GM / R 2 )
or, g '/ g = M ' R 2 / (M (R-x) 2 )... ... ... ... (iii)
Now, Density of earth ( ρ ) = M/V
ρ = M/ (4/3 π R 3 )
M = ρ x (4/3 π R 3 ) ... ... ... ... (iv)
Density of earth below x meter from the surface of earth (ρ) = M '/V '
ρ = M ' / (4/3 π (R - x) 3 )
M ' = ρ x (4/3 π (R - x) 3 ) ... ... ... (v)
Putting (iv) and (v) in (iii), we get,
g '/ g = (ρ x (4/3 π (R - x) 3 ) x R 2 )/ ( ρ x (4/3 π R 3 ) (R-x) 2 )
or, g ' = g(1- x/R)
The regular variation in the heart rate due to the changes in the rate and depth of breathing is called arrhythmias.
I saw nothing. This question can be handled better by someone who was there and actually saw it.
The ocean floor is very much like dry terrain; it has mountains and valleys, so the depth is not constant all over earth.
The illusion of depth on a flat surface.
The formula for depth in terms of pressure is given by: depth = (pressure)/(density*g), where pressure is the pressure at the depth, density is the density of the fluid, and g is the acceleration due to gravity. This formula is derived from the hydrostatic pressure equation.
If you are taking the variation of 'g' with altitude, then its weight is lesser, not greater, at the beginning of the descent. But for small heights, The variation of g is negligible, so its weight remains the same
The ocean floor is very much like dry terrain; it has mountains and valleys, so the depth is not constant all over earth.
His Sonata in G Opus 14 No.2 has a theme and variation in the Second Movement
In a two-way ANOVA in depth, the relate in an equation the total variation, , where i=1,2,…,a, j=1,2,…,b and k=1,2,...,n; the explained variation by the "treatment" or first factor is , the explained variation by the "block" or second factor is and the unexplained variation . SST=SSA+SSB+ SS(AB) + SSE Degrees of freedom N-1 a-1 b-1 (a-1)(b-1) N-ab N=nab  
Some variation of brown/grey/black, depending on the amounts and depth of the purple colour.
Some variation of brown/grey/black, depending on the amounts and depth of the purple colour.
it depends on the vapour pressure of the liquid