Tropicalization of Abstract Curves

  1. Conventions
  2. Tropical Curves
    1. Algorithm
    2. A Q\mathbb Q-tropical curve associated to (C,D)(C,D)
    3. Parameterized Tropical Curves

Today Abhishek Koparde spoke on the tropicalization of abstract curves. These are some rough notes taken during the talk.

Main reference: Tropical geometry and correspondence theorems via toric stacks. Link to Abhishek's notes: not yet obtained.

Conventions

KK is algebraicaly closed, RR is a complex DVR with residue field kk and fraction field FF. We let F\overline F be the separable closure of FF and vv is a normalized valuation on F\overline F so that v(F)=Zv(F^*) = \mathbb Z.

Graphs are finite connected with the usual notations.

Curves are denoted by (C,D)(C,D), are assumed to be complete with marked points (q1,...,qD)(q_1,...,q_{|D|}) over F\overline F, and (CRL,DRL)(C_{R_L}, D_{R_L}) is the nodal model (FLFF \subset L\subset \overline F is an intermediate field extension). CRLSpecRLC_{R_L} \to \operatorname{Spec} R_{L} is a proper curve and L/FL/F is finite separable. DRLD_{R_L} is a finite set of RLR_L points and the total space CRLC_{R_L} is normal. (CRL,DRL)×SpecRLSpeck(C_{R_L},D_{R_L}) \times_{\operatorname{Spec} R_{L}} \operatorname{Spec} k is nodal and (CRL,DRL)×SpecRLSpecF(C,D)(C_{R_L}, D_{R_L})\times_{\operatorname{Spec}_{R_L}} \operatorname{Spec} \overline F \cong (C,D).

Tropical Curves

A tropical curve Γ\Gamma is a topological graph with a complete (possibly degenerate) metric. (Note that a degenerate metric is one where d(x,y)=0d(x,y) = 0 does not necessarily imply that x=yx = y. I think this is sometimes called a pseudo-metric.)

These axioms describe a general tropical curve. We say

Algorithm

The following modifications made to a general tropical graph will not change the genus:

Claim: Let Γ\Gamma be an irreducible tropical curve satisfying g(Γ)+V(Γ)+122g(\Gamma) + \frac{|V^\infty(\Gamma)| + 1}{2} \geq 2. Then there exists a unique stable tropical curve Γst\Gamma^{st} such that V(Γ)=V(Γst)V^\infty(\Gamma) = V^\infty(\Gamma^{st}) and Γ\Gamma can be obtained from Γst\Gamma^{st} and Γ\Gamma can be obtained from Γst\Gamma^{st} by using finitely many of the above steps. We call Γst\Gamma^{st} the stabilization of Γ\Gamma.

A Q\mathbb Q-tropical curve associated to (C,D)(C,D)

Consider a curve (C,D)(C,D) and remember that (CRL,DRL)(C_{R_L},D_{R_L}) is the nodal model and CRL×SpecRLSpeckC_{R_L} \times_{\operatorname{Spec} R_L} \operatorname{Spec} k is the fiber over the base. Irreducible components will correspond to finite vertices, nodes will correspond to edges between finite vertices and DRLsD_{R_L}'s which specialize to CVC_V will correspond to infinite edges. This should determine a tropical curve, and we call this tropical curve the tropicalization of the curve.

At this point Abhishek included a picture of a sphere identified with a torus at a point corresponding a tropical curve with two finite vertices, one finite edge and three infinite edge. One finite vertex has valence 3 and the other has valence 2. In particular, this means the tropicalization is not stable.

There was some ambiguity about what it means to say "(C,D)(C,D) is stable". At first, we thought it might mean that there exists a nodal model (CRL,DRL)(C_{R_L},D_{R_L}) such that its special fiber is stable, but this is true of any curve because of the stable reduction theorem, so it must be something else.

Parameterized Tropical Curves

Let NN be a lattice, NR=NRN_\mathbb R = N\otimes \mathbb R. A parameterized tropical curve is a pair (Γ,hΓ)(\Gamma, h_\Gamma) where hΓ:V(Γ)NRh_\Gamma:V(\Gamma) \to N_\mathbb R is a map such that hΓ(v)Nh_\Gamma(v) \in N for vV(Γ)v\in V^\infty(\Gamma) and

1e(hΓ(v)hΓ(v))N.\begin{aligned} \frac{1}{|e|}(h_\Gamma(v) - h_\Gamma(v')) \in N. \end{aligned}

We also require that it satisfies the balancing condition:

vVf(Γ)    vVf(Γ),eEvv(Γ)1e(hΓ(v)hΓ(v)) + vV(Γ),eEv,v(Γ)hΓ(v) = 0.\begin{aligned} v \in V^f(\Gamma) \implies \sum_{v'\in V^f(\Gamma), e\in E_{vv'}(\Gamma)} \frac{1}{|e|}(h_\Gamma(v) - h_\Gamma(v')) ~+~ \sum_{v' \in V^\infty(\Gamma), e\in E_{v,v'}(\Gamma)} h_\Gamma(v') ~=~ 0. \end{aligned}

If hΓ(v)NQh_\Gamma(v) \in N_\mathbb Q for all vv then we say Γ\Gamma is a NQN_\mathbb Q-parameterized Q\mathbb Q-tropical curve. For the duration of today we'll attempt to justify the balancing condition.

Suppose that you have a map f:CDTN,Ff:C\setminus D \to T_{N, \overline F} and let (CRL,DRL)(C_{R_L}, D_{R_L}) be a nodal model. Here TN,FT_{N,\overline F} is the algebraic torus of dimension equal to the rank of NN. There's a diagram that I'd like to draw but can't because of tikzcd support in markdown, but its rows look like CDTN,FC\setminus D \to T_{N,\overline F} and CRLDRLTN,RLC_{R_L}\setminus D_{R_L} \to T_{N,R_L}.

In this picture, given a character χm\chi^m on TN,RLT_{N,R_L}, I can pull back to obtain a character on CRLDRLC_{R_L}\setminus D_{R_L}. I can evaluate the order of this on an irreducible component VV of CC, and arrive at the following definition for hΓh_\Gamma:

hΓ(V):=1eordVf(χm). h_\Gamma(V) := \frac{1}{|e|} \operatorname{ord}_{V} f^*(\chi^m).

The character χm\chi^m is a linear function of mm for some mM=Nm\in M = N^\vee, so in particular, 1eordVf(χm)NQ\frac{1}{|e|} \operatorname{ord}_{V} f^*(\chi^m) \in N_\mathbb Q. Furthermore,

ordVf(χm+m)=ordVf(χm)+ordVf(χm), \operatorname{ord}_{V} f^*(\chi^{m + m'}) = \operatorname{ord}_{V} f^*(\chi^m) + \operatorname{ord}_{V} f^*(\chi^{m'}),

so this definition of hΓ(V)h_\Gamma(V) is linear. We also need that 1e(hΓ(v)hΓ(v))NQ\frac{1}{|e|}(h_\Gamma(v) - h_\Gamma(v')) \in N_\mathbb Q for any bounded edge vv.

We completed the proof that hΓh_\Gamma does indeed satisfy the balancing condition, but I wasn't able to get all of it down. Please see the end of Abhishek's notes.

©Isaac Martin. Last modified: January 15, 2024.