Tropical projective space

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Conventional visualization of the tropical projective plane, with projection of the real coordinate axes.

In tropical geometry, a tropical projective space is the tropical analog of the classic projective space.

Definition

Given a module M over the tropical semiring T, its projectivization is the usual projective space of a module: the quotient space of the module (omitting the additive identity 0) under scalar multiplication, omitting multiplication by the scalar additive identity 0:[lower-alpha 1]

[math]\displaystyle{ \mathbf{T}(M) := (M \setminus \mathbf{0})/(\mathbf{T} \setminus 0). }[/math]

In the tropical setting, tropical multiplication is classical addition, with unit real number 0 (not 1); tropical addition is minimum or maximum (depending on convention), with unit extended real number (not 0),[lower-alpha 2] so it is clearer to write this using the extended real numbers, rather than the abstract algebraic units:

[math]\displaystyle{ \mathbf{T}(M) := (M \setminus \boldsymbol{\infty})/(\mathbf{T} \setminus \infty). }[/math]

Just as in the classical case, the standard n-dimensional tropical projective space is defined as the quotient of the standard (n+1)-dimensional coordinate space by scalar multiplication, with all operations defined coordinate-wise:[1]

[math]\displaystyle{ \mathbf{TP}^n := (\mathbf{T}^{n+1} \setminus \boldsymbol{\infty})/(\mathbf{T} \setminus \infty). }[/math]

Tropical multiplication corresponds to classical addition, so tropical scalar multiplication by c corresponds to adding c to all coordinates. Thus two elements of [math]\displaystyle{ \mathbf T^{n+1} \setminus \boldsymbol{\infty} }[/math] are identified if their coordinates differ by the same additive amount c:

[math]\displaystyle{ (x_0, \dots, x_n) \sim (y_0, \dots, y_n) \iff (x_0 + c, \dots, x_n + c) = (y_0, \dots, y_n). }[/math]

Notes

  1. As usual, scalar multiplication of any vector by 0 yields the identity for vector addition 0, so these must be omitted or all vectors will be identified.
  2. can be interpreted as either positive or negative infinity, depending on convention.

References

  1. Mikhalkin 2006, p. 6, example 3.10.
  • Richter-Gebert, Jürgen; Sturmfels, Bernd; Theobald, Thorsten (2003). "First steps in tropical geometry". arXiv:math/0306366.
  • Mikhalkin, Grigory (2006). "Tropical Geometry and its applications". arXiv:math/0601041.