Intuition The one core idea
A smooth surface, seen up close, looks like a flat tilted sheet — and that sheet is completely described by just its height at a point plus how steeply it climbs in two perpendicular directions. This whole topic is about writing that flat sheet as an equation and using it to guess nearby heights.
This page assumes nothing . Before you can read the parent note Tangent Planes , every symbol it uses is built here from the ground up, in an order where each one leans only on the ones before it.
Everything happens in three-dimensional space . We label a point by three numbers.
( x , y , z )
Three numbers that pin down one point in space:
x — how far right (or left if negative),
y — how far forward (or back),
z — how far up (or down).
The picture : three number-lines (axes) meeting at right angles at the origin ( 0 , 0 , 0 ) . The x - and y -axes make the flat ground ; the z -axis stands straight up.
Why the topic needs it: a surface is a shape floating in this space, and the tangent plane is another shape in the same space. Without axes we can't say where anything is.
f ( x , y ) — a height machine
f is a rule that takes two inputs x and y (a spot on the ground) and returns one number — a height. We read "f ( x , y ) " as "f of x and y ".
The picture : stand on the ground at spot ( x , y ) , look straight up, and f ( x , y ) tells you how high the roof is above you.
Worked example Reading the notation
If f ( x , y ) = x 2 + y 2 , then f ( 1 , 2 ) means "put x = 1 and y = 2 in": 1 2 + 2 2 = 5 .
Why the topic needs it: the surface is the function. The whole game is approximating f near one spot.
Intuition From a rule to a shape
If we plot the point ( x , y , f ( x , y )) for every ground spot ( x , y ) , all those points together form a surface — a curved sheet hovering over the ground. Writing z = f ( x , y ) just says "let the height coordinate z equal the machine's output".
The bowl in the figure is z = x 2 + y 2 . Directly above the ground spot ( a , b ) sits the surface point ( a , b , f ( a , b )) — the yellow dot. That dot is where our flat sheet will touch.
( a , b ) — the spot we zoom into
a and b are just fixed numbers : the particular ground spot where we build our flat sheet. x and y stay variable — they roam around near ( a , b ) .
x − a and y − b — the step away
x − a = how far right of the base point you've walked. y − b = how far forward. Together they are your small step from ( a , b ) to a nearby spot ( x , y ) .
The picture : an arrow on the ground from the fixed dot ( a , b ) to a nearby dot ( x , y ) ; its rightward part is x − a , its forward part is y − b .
x with x − a
The slopes will multiply the step x − a , never x itself. If you're standing at the base point, x − a = 0 and the plane must give exactly f ( a , b ) — that only works with the offset.
Why the topic needs it: "linear approximation" means height at base plus slope × step . The step is precisely ( x − a , y − b ) .
Before two dimensions, recall the one-dimensional idea from Tangent line and linear approximation (single variable) : the slope of a curve y = f ( x ) is "rise over run" of its tangent line — how fast height changes as you step right.
tool for slope on a surface
On a surface you can walk in infinitely many directions, each with its own steepness. The cleverest trick is to freeze one variable so the surface becomes a plain 1D curve — then use ordinary slope. That frozen-slice slope is a partial derivative .
Definition Partial derivatives
f x and f y
f x ( a , b ) ("f-sub-x"): hold y = b fixed , walk in the x -direction only, measure the slope. It answers "how steeply does the surface climb as I step right?"
f y ( a , b ) : hold x = a fixed, walk in the y -direction, measure the slope. "How steeply as I step forward?"
The picture : slice the surface with a vertical wall. The wall parallel to the x -axis cuts out a curve whose tangent-line slope is f x ; the wall parallel to the y -axis gives f y .
Worked example Computing a partial
For f ( x , y ) = x 2 + y 2 : to get f x , treat y as a constant and differentiate in x only: f x = 2 x . Treating x as constant: f y = 2 y . At ( 1 , 2 ) : f x = 2 , f y = 4 .
Why the topic needs it: the tangent plane must tilt exactly like the surface. Its two tilts are f x and f y . Full machinery lives in Partial derivatives .
Definition A non-vertical plane
A flat, tilted sheet with no folds. Any such sheet can be written
z = z 0 + A ( x − a ) + B ( y − b )
where z 0 is its height above the base point, A is its rightward tilt, B its forward tilt.
The picture : a stiff sheet of cardboard pinned at height z 0 over ( a , b ) , tilted by A side-to-side and B front-to-back.
Read the symbols: at the base point x − a = 0 and y − b = 0 , so z = z 0 — the sheet passes through height z 0 . Step one unit right (x − a = 1 ) and z rises by A : that's why A is the rightward slope.
Why the topic needs it: this is the raw shape of the answer. The parent note fills in z 0 = f ( a , b ) , A = f x , B = f y to make it the tangent plane.
Once we plug z 0 = f ( a , b ) , A = f x ( a , b ) , B = f y ( a , b ) into the plane of section 5, the right-hand side gets its own name.
L ( x , y ) — the linear approximation
L ( x , y ) is a name for the height of the flat sheet above the ground spot ( x , y ) :
L ( x , y ) = f ( a , b ) + f x ( a , b ) ( x − a ) + f y ( a , b ) ( y − b ) .
Reading it: "L " stands for linear — the formula has only steps to the first power, no squares, so its graph is a plane. It is the exact same right-hand side as z = z 0 + A ( x − a ) + B ( y − b ) , now with the tangent-plane values filled in.
The picture : for any ground spot ( x , y ) , L ( x , y ) is the height you read off the flat sheet (not the curved surface) directly above that spot.
Why the topic needs it: every later formula — the ≈ statement, the error, the differentiability limit — is written in terms of L . Having a single letter for "the flat-sheet height" keeps those formulas short.
≈ — "is close to"
f ( x , y ) ≈ L ( x , y ) reads "the true surface height is nearly the flat-sheet height L ( x , y ) from section 6." Not exactly equal — close, and closer the smaller your step.
Why the topic needs it: the whole point of a linear approximation is that it's a good guess, not an exact truth. The gap is the error , studied via Differentiability of multivariable functions .
Δ z — the true change
Greek capital delta Δ means "change in". Δ z = f ( x , y ) − f ( a , b ) is how much the real surface height changed as you stepped from ( a , b ) to ( x , y ) .
d x , d y , d z — the predicted step and change
d x = x − a and d y = y − b are your (small) steps. d z = f x d x + f y d y is the change the flat sheet predicts . For small steps, Δ z ≈ d z .
d z comes from — read it off the plane
The flat sheet's height is L ( x , y ) = f ( a , b ) + f x ( x − a ) + f y ( y − b ) from section 6. Its change as you step away from the base point is
L ( x , y ) − L ( a , b ) = [ f ( a , b ) + f x ( x − a ) + f y ( y − b ) ] − f ( a , b ) = f x ( x − a ) + f y ( y − b ) .
Rename x − a = d x and y − b = d y and this is d z = f x d x + f y d y . So d z isn't a new idea — it's literally "how much the plane of section 5 rose over your step." Because f ( x , y ) ≈ L ( x , y ) near the point, the true rise Δ z matches this predicted rise d z .
The picture : two heights rising above your step — the curved surface's real rise Δ z , and the flat sheet's straight-line rise d z . Near the point they almost coincide; far away they split apart.
Why the topic needs it: differentials d z are how the topic does fast error estimates (like the rectangle-area example).
( x , y ) → ( a , b ) lim — "as you creep toward the base point"
This symbol asks: what value does an expression home in on as ( x , y ) slides ever closer to ( a , b ) from any direction?
Intuition Why a limit, and not just "small error"
A tangent plane is only honest if its error dies faster than you approach . Here L ( x , y ) is the flat-sheet height from section 6, and f ( x , y ) − L ( x , y ) is the gap between the true surface and the sheet. We measure approach by the straight-line distance ( x − a ) 2 + ( y − b ) 2 (Pythagoras on the ground step). The test
lim ( x , y ) → ( a , b ) ( x − a ) 2 + ( y − b ) 2 f ( x , y ) − L ( x , y ) = 0
says the error is tiny even compared to how far you've stepped . That is the exact meaning of differentiable .
Why the topic needs it: this is the fine print guaranteeing the plane truly "hugs" the surface — the subject of Differentiability of multivariable functions .
⟨ p , q , r ⟩
An arrow in space described by three components: p right, q forward, r up. The angle-brackets ⟨ ⟩ just group them.
Definition Dot product and perpendicularity
For two vectors ⟨ p , q , r ⟩ and ⟨ u , v , w ⟩ , the dot product is the single number p u + q v + r w . Its key fact: two vectors are perpendicular (at right angles) exactly when their dot product is 0 .
n
"Normal" means perpendicular — sticking straight out of the surface like a flagpole from a hillside. The tangent plane is everything at right angles to n .
The picture : the flat sheet lying on the surface, with one arrow n poking straight up out of it.
n = ⟨ f x , f y , − 1 ⟩ — check it's perpendicular
The plane contains two natural direction-arrows built from the slopes:
step 1 right, and the height climbs by f x : the arrow t x = ⟨ 1 , 0 , f x ⟩ ;
step 1 forward, height climbs by f y : the arrow t y = ⟨ 0 , 1 , f y ⟩ .
A vector normal to the plane must be perpendicular to both . Dot n with each:
n ⋅ t x = f x ( 1 ) + f y ( 0 ) + ( − 1 ) f x = f x − f x = 0 ,
n ⋅ t y = f x ( 0 ) + f y ( 1 ) + ( − 1 ) f y = f y − f y = 0.
Both dot products vanish, so n = ⟨ f x , f y , − 1 ⟩ really does stick out perpendicular to the sheet. The − 1 in the last slot is what cancels the height-climb terms.
Why the topic needs it: it gives a second, elegant way to write the plane, and it connects to The gradient vector and Directional derivatives .
base point a b and steps x-a y-b
plane form height plus tilts
partial derivatives fx fy
approx symbol and deltas dz
TANGENT PLANE TOPIC 4.4.5
Can you answer each without peeking? Reveal to check.
What do the three numbers in ( x , y , z ) measure? How far right, forward, and up a point sits from the origin.
What does f ( x , y ) return, and what does it picture? A single height above the ground spot ( x , y ) — the roof height over that spot.
What shape is z = f ( x , y ) ? A curved surface, made of all points ( x , y , f ( x , y )) floating over the ground.
What are x − a and y − b ? The rightward and forward parts of your small step away from the fixed base point ( a , b ) .
In plain words, what is f x ( a , b ) ? The slope of the surface as you step in the x -direction with y held fixed at b .
How do you compute f x from a formula? Differentiate treating y as a constant.
Why write a plane as z = z 0 + A ( x − a ) + B ( y − b ) ? It automatically passes through height z 0 at ( a , b ) , and A , B are its two tilts.
What is L ( x , y ) ? A name for the flat-sheet height: L ( x , y ) = f ( a , b ) + f x ( a , b ) ( x − a ) + f y ( a , b ) ( y − b ) .
Difference between Δ z and d z ? Δ z is the true surface height-change; d z is the flat sheet's predicted change, i.e. L 's change over the step.
Where does d z = f x d x + f y d y come from? It's L ( x , y ) − L ( a , b ) with d x = x − a , d y = y − b — the plane's own rise over the step.
What does the differentiability limit say in words? The error f − L shrinks faster than your distance to the base point.
Why is n = ⟨ f x , f y , − 1 ⟩ normal to the surface? Its dot product with both in-plane arrows ⟨ 1 , 0 , f x ⟩ and ⟨ 0 , 1 , f y ⟩ is 0 , so it is perpendicular to the whole sheet.
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