How can a gradient be though of as a function?

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If a function $f(x,y)$ would output a value in a third dimension, $z=f(x,y)$ for example. How can we treat the gradient of f as a function in x and y, when the output of the gradient is a vector in the two dimensions $x$ and $y$ which are the dimensions of the inputs. I guess my question is, is it normal for a function to map to the dimensions of its inputs?










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  • Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
    – WesleyGroupshaveFeelingsToo
    11 mins ago















up vote
4
down vote

favorite












If a function $f(x,y)$ would output a value in a third dimension, $z=f(x,y)$ for example. How can we treat the gradient of f as a function in x and y, when the output of the gradient is a vector in the two dimensions $x$ and $y$ which are the dimensions of the inputs. I guess my question is, is it normal for a function to map to the dimensions of its inputs?










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  • Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
    – WesleyGroupshaveFeelingsToo
    11 mins ago













up vote
4
down vote

favorite









up vote
4
down vote

favorite











If a function $f(x,y)$ would output a value in a third dimension, $z=f(x,y)$ for example. How can we treat the gradient of f as a function in x and y, when the output of the gradient is a vector in the two dimensions $x$ and $y$ which are the dimensions of the inputs. I guess my question is, is it normal for a function to map to the dimensions of its inputs?










share|cite|improve this question















If a function $f(x,y)$ would output a value in a third dimension, $z=f(x,y)$ for example. How can we treat the gradient of f as a function in x and y, when the output of the gradient is a vector in the two dimensions $x$ and $y$ which are the dimensions of the inputs. I guess my question is, is it normal for a function to map to the dimensions of its inputs?







multivariable-calculus functions






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edited 35 mins ago









Ethan Bolker

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asked 3 hours ago









Omar Hossam Ahmed

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  • Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
    – WesleyGroupshaveFeelingsToo
    11 mins ago

















  • Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
    – WesleyGroupshaveFeelingsToo
    11 mins ago
















Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
– WesleyGroupshaveFeelingsToo
11 mins ago





Problems in calculus often stem from physics and engineering, here we deal a lot with $mathbbR^3$ and $mathbbR^2$, so it makes sense that we visualise this by writing out a certain function in terms of $x,y,z$ we could define other basis vectors and write out some other functions for instance in terms of spherical polar coordinates, but the input is hard to visualise. We often transform to other coordinates to do integrations, for instance when we want to integrate over a sphere. The corresponding problem then transforms to some other graph in terms of these new coordinates.
– WesleyGroupshaveFeelingsToo
11 mins ago











2 Answers
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A function $F$ can be thought of as a machine that takes in inputs from one set, say $X$, and outputs elements in another set, say $Y$. A function outputs a single element for every input, and we write it $F : X rightarrow Y$.



In your case, the gradient of $f$ is just a function $nabla f : mathbbR^2 rightarrow mathbbR^2$, where for each input $(x,y)$, it outputs the element $left( fracpartial fpartial x(x,y), fracpartial fpartial y(x,y) right)$.






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    $(1)$ The gradient is a vector-valued function, this maps pairs of numbers $(x,y)$ to some other pair of numbers $(x',y')$. These pairs of numbers we call vectors and they have a very geometric interpretation: they have a length and a direction. Specifically the gradient corresponds to the direction and magnitude of steepest ascent.



    Also see:



    https://en.wikipedia.org/wiki/Vector-valued_function



    This Khan Academy link I found as well is very useful as he also thought of the same example as I did:
    https://www.khanacademy.org/math/multivariable-calculus/multivariable-derivatives/gradient-and-directional-derivatives/v/gradient-and-graphs



    $(2)$ On the contrary, when you plot a function that maps from $mathbbR^2 rightarrow mathbbR$ like $f(x,y)=x^2 +y^2$, when you want to plot this you often define a third variable $z=f(x,y)$ and you let the value of this variable be equal to the function value. I have plotted $x^2 +y^2$ in this way below:
    enter image description here



    Without introducing another axis, we can also just give different function value ranges a different colour, so a large value could be very dark and a low value could be very light or vice versa. We recognise the same function:



    enter image description here



    The difference between $(1)$ and $(2)$ is the notion of direction. The function you describe is usually a "scalar field", we only have the notion of magnitude or "value" but not of direction. Gradients will give you a so-called "vector field" as physicists often call it, we usually visualise this using VectorPlots. Below you find such a method, I've plotted the vector field $f(x,y)=(x^2+y,y^2+x )$



    enter image description here



    which has gradient $grad(f)(x,y)=(2x,2y)$



    enter image description here






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      2 Answers
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      active

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      2 Answers
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      active

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      active

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      up vote
      6
      down vote













      A function $F$ can be thought of as a machine that takes in inputs from one set, say $X$, and outputs elements in another set, say $Y$. A function outputs a single element for every input, and we write it $F : X rightarrow Y$.



      In your case, the gradient of $f$ is just a function $nabla f : mathbbR^2 rightarrow mathbbR^2$, where for each input $(x,y)$, it outputs the element $left( fracpartial fpartial x(x,y), fracpartial fpartial y(x,y) right)$.






      share|cite|improve this answer
























        up vote
        6
        down vote













        A function $F$ can be thought of as a machine that takes in inputs from one set, say $X$, and outputs elements in another set, say $Y$. A function outputs a single element for every input, and we write it $F : X rightarrow Y$.



        In your case, the gradient of $f$ is just a function $nabla f : mathbbR^2 rightarrow mathbbR^2$, where for each input $(x,y)$, it outputs the element $left( fracpartial fpartial x(x,y), fracpartial fpartial y(x,y) right)$.






        share|cite|improve this answer






















          up vote
          6
          down vote










          up vote
          6
          down vote









          A function $F$ can be thought of as a machine that takes in inputs from one set, say $X$, and outputs elements in another set, say $Y$. A function outputs a single element for every input, and we write it $F : X rightarrow Y$.



          In your case, the gradient of $f$ is just a function $nabla f : mathbbR^2 rightarrow mathbbR^2$, where for each input $(x,y)$, it outputs the element $left( fracpartial fpartial x(x,y), fracpartial fpartial y(x,y) right)$.






          share|cite|improve this answer












          A function $F$ can be thought of as a machine that takes in inputs from one set, say $X$, and outputs elements in another set, say $Y$. A function outputs a single element for every input, and we write it $F : X rightarrow Y$.



          In your case, the gradient of $f$ is just a function $nabla f : mathbbR^2 rightarrow mathbbR^2$, where for each input $(x,y)$, it outputs the element $left( fracpartial fpartial x(x,y), fracpartial fpartial y(x,y) right)$.







          share|cite|improve this answer












          share|cite|improve this answer



          share|cite|improve this answer










          answered 3 hours ago









          Sambo

          1,8652428




          1,8652428




















              up vote
              2
              down vote













              $(1)$ The gradient is a vector-valued function, this maps pairs of numbers $(x,y)$ to some other pair of numbers $(x',y')$. These pairs of numbers we call vectors and they have a very geometric interpretation: they have a length and a direction. Specifically the gradient corresponds to the direction and magnitude of steepest ascent.



              Also see:



              https://en.wikipedia.org/wiki/Vector-valued_function



              This Khan Academy link I found as well is very useful as he also thought of the same example as I did:
              https://www.khanacademy.org/math/multivariable-calculus/multivariable-derivatives/gradient-and-directional-derivatives/v/gradient-and-graphs



              $(2)$ On the contrary, when you plot a function that maps from $mathbbR^2 rightarrow mathbbR$ like $f(x,y)=x^2 +y^2$, when you want to plot this you often define a third variable $z=f(x,y)$ and you let the value of this variable be equal to the function value. I have plotted $x^2 +y^2$ in this way below:
              enter image description here



              Without introducing another axis, we can also just give different function value ranges a different colour, so a large value could be very dark and a low value could be very light or vice versa. We recognise the same function:



              enter image description here



              The difference between $(1)$ and $(2)$ is the notion of direction. The function you describe is usually a "scalar field", we only have the notion of magnitude or "value" but not of direction. Gradients will give you a so-called "vector field" as physicists often call it, we usually visualise this using VectorPlots. Below you find such a method, I've plotted the vector field $f(x,y)=(x^2+y,y^2+x )$



              enter image description here



              which has gradient $grad(f)(x,y)=(2x,2y)$



              enter image description here






              share|cite|improve this answer


























                up vote
                2
                down vote













                $(1)$ The gradient is a vector-valued function, this maps pairs of numbers $(x,y)$ to some other pair of numbers $(x',y')$. These pairs of numbers we call vectors and they have a very geometric interpretation: they have a length and a direction. Specifically the gradient corresponds to the direction and magnitude of steepest ascent.



                Also see:



                https://en.wikipedia.org/wiki/Vector-valued_function



                This Khan Academy link I found as well is very useful as he also thought of the same example as I did:
                https://www.khanacademy.org/math/multivariable-calculus/multivariable-derivatives/gradient-and-directional-derivatives/v/gradient-and-graphs



                $(2)$ On the contrary, when you plot a function that maps from $mathbbR^2 rightarrow mathbbR$ like $f(x,y)=x^2 +y^2$, when you want to plot this you often define a third variable $z=f(x,y)$ and you let the value of this variable be equal to the function value. I have plotted $x^2 +y^2$ in this way below:
                enter image description here



                Without introducing another axis, we can also just give different function value ranges a different colour, so a large value could be very dark and a low value could be very light or vice versa. We recognise the same function:



                enter image description here



                The difference between $(1)$ and $(2)$ is the notion of direction. The function you describe is usually a "scalar field", we only have the notion of magnitude or "value" but not of direction. Gradients will give you a so-called "vector field" as physicists often call it, we usually visualise this using VectorPlots. Below you find such a method, I've plotted the vector field $f(x,y)=(x^2+y,y^2+x )$



                enter image description here



                which has gradient $grad(f)(x,y)=(2x,2y)$



                enter image description here






                share|cite|improve this answer
























                  up vote
                  2
                  down vote










                  up vote
                  2
                  down vote









                  $(1)$ The gradient is a vector-valued function, this maps pairs of numbers $(x,y)$ to some other pair of numbers $(x',y')$. These pairs of numbers we call vectors and they have a very geometric interpretation: they have a length and a direction. Specifically the gradient corresponds to the direction and magnitude of steepest ascent.



                  Also see:



                  https://en.wikipedia.org/wiki/Vector-valued_function



                  This Khan Academy link I found as well is very useful as he also thought of the same example as I did:
                  https://www.khanacademy.org/math/multivariable-calculus/multivariable-derivatives/gradient-and-directional-derivatives/v/gradient-and-graphs



                  $(2)$ On the contrary, when you plot a function that maps from $mathbbR^2 rightarrow mathbbR$ like $f(x,y)=x^2 +y^2$, when you want to plot this you often define a third variable $z=f(x,y)$ and you let the value of this variable be equal to the function value. I have plotted $x^2 +y^2$ in this way below:
                  enter image description here



                  Without introducing another axis, we can also just give different function value ranges a different colour, so a large value could be very dark and a low value could be very light or vice versa. We recognise the same function:



                  enter image description here



                  The difference between $(1)$ and $(2)$ is the notion of direction. The function you describe is usually a "scalar field", we only have the notion of magnitude or "value" but not of direction. Gradients will give you a so-called "vector field" as physicists often call it, we usually visualise this using VectorPlots. Below you find such a method, I've plotted the vector field $f(x,y)=(x^2+y,y^2+x )$



                  enter image description here



                  which has gradient $grad(f)(x,y)=(2x,2y)$



                  enter image description here






                  share|cite|improve this answer














                  $(1)$ The gradient is a vector-valued function, this maps pairs of numbers $(x,y)$ to some other pair of numbers $(x',y')$. These pairs of numbers we call vectors and they have a very geometric interpretation: they have a length and a direction. Specifically the gradient corresponds to the direction and magnitude of steepest ascent.



                  Also see:



                  https://en.wikipedia.org/wiki/Vector-valued_function



                  This Khan Academy link I found as well is very useful as he also thought of the same example as I did:
                  https://www.khanacademy.org/math/multivariable-calculus/multivariable-derivatives/gradient-and-directional-derivatives/v/gradient-and-graphs



                  $(2)$ On the contrary, when you plot a function that maps from $mathbbR^2 rightarrow mathbbR$ like $f(x,y)=x^2 +y^2$, when you want to plot this you often define a third variable $z=f(x,y)$ and you let the value of this variable be equal to the function value. I have plotted $x^2 +y^2$ in this way below:
                  enter image description here



                  Without introducing another axis, we can also just give different function value ranges a different colour, so a large value could be very dark and a low value could be very light or vice versa. We recognise the same function:



                  enter image description here



                  The difference between $(1)$ and $(2)$ is the notion of direction. The function you describe is usually a "scalar field", we only have the notion of magnitude or "value" but not of direction. Gradients will give you a so-called "vector field" as physicists often call it, we usually visualise this using VectorPlots. Below you find such a method, I've plotted the vector field $f(x,y)=(x^2+y,y^2+x )$



                  enter image description here



                  which has gradient $grad(f)(x,y)=(2x,2y)$



                  enter image description here







                  share|cite|improve this answer














                  share|cite|improve this answer



                  share|cite|improve this answer








                  edited 4 mins ago

























                  answered 37 mins ago









                  WesleyGroupshaveFeelingsToo

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