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Tropicalization of $\psi $ classes

Published online by Cambridge University Press:  20 April 2026

Andreas Gross
Affiliation:
Department of Mathematics, Goethe-Universität Frankfurt , Germany; E-mail: gross@math.uni-frankfurt.de
Renzo Cavalieri*
Affiliation:
Department of Mathematics, Colorado State University , Fort Collins CO, USA
*
E-mail: renzo@colostate.edu (Corresponding author)

Abstract

Under suitable conditions on a family of logarithmic curves, we endow the tropicalization of the family with an affine structure in a neighborhood of the sections in such a way that the tropical $\psi $ classes from [6] arise as tropicalizations of algebraic $\psi $ classes.

Information

Type
Mathematical Physics
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1 An illustration that tropical cross ratios are the tropicalization of algebraic cross ratios. The top of the figure shows a cross ratio as factoring through a morphism to $\overline {\mathcal M}_{0,4}$, which is then identified with (the difference between the two spaces is the boundary structure). Tropical cross ratios are similarly obtained in the row below. Functoriality of tropicalization shows the bottom part of the figure to be the tropicalization of the top.

Figure 1

Figure 2 The setup used in showing that a function $\phi \in \operatorname {\mathrm {Aff}}_{ \Sigma _X}( \Sigma _X^\tau )$ is the restriction of a function in $\operatorname {\mathrm {Aff}}_{\Sigma _Y}( \Sigma _Y^\sigma )$. The key point is that the map $f_\gamma $ is a $\mathbb {P}^1$ bundle. In the illustration we draw $\theta = \sigma $ for lack of dimensions: $\sigma $ is the minimal cone of $\Sigma _Y$ containing $\tau $, and $\theta $ a maximal cone with such property.

Figure 2

Figure 3 Illustration for the second part of the argument in Proposition 3.8. Here by lack of dimensions we have drawn $\sigma = \gamma $. Observe that $\tilde {\gamma } \subset \gamma $, and the cones $\theta $ and $\theta '$ are the two-dimensional triangles bounded by the black edges.

Figure 3

Figure 4 The primitive ray generators for the cone complex $\Sigma $, depicted in red, are embedded into via the chosen generators of H, and into via the generators of $\overline {H}$. The two balanced fans are related by a linear function. The failure of normality of H detects the fact that the embedding of $\Sigma $ as a plane balanced fan is not as linearly independent as possible.

Figure 4

Figure 5 The subdivision of the edge e in $G_\star $.

Figure 5

Figure 6 The tropicalization of a line bundle on a toroidal space with a unique boundary divisor H. As suggested by the orientation of the picture, we call x a linear coordinate for the ray $\rho _H$ and y the coordinate for the ray $\rho _Z$ dual to the zero section $Z\cong X$.

Figure 6

Figure 7 A topological cartoon of the admissible covers parameterized by the general points of $\mathrm {src}^\ast (D_2)$. The blue points are the marked points that get forgotten by the map $r_2$, which we did not label to avoid cluttering the figure. There are three possible ways to order the pairs of blue points, giving rise to three irreducible components.

Figure 7

Figure 8 The topological types of tropical covers corresponding to the rays and two-dimensional cones of $\overline {Adm}^{{\mathtt {trop}}}_{1\to 0}((3), (2,1)^4)$. Types are labeled as in their description in Section 6.2. The color coding is meant to facilitate the understanding of the structure of the cone complex of tropical admissible covers, represented in Figure 9.

Figure 8

Table 1 The factors computing the weights of two-dimensional cones in $\overline {Adm}^{{\mathtt {trop}}}_{1\to 0}((3), (2,1)^4)$.

Figure 9

Figure 9 The restriction of the map $\mathtt {br}^{trop}$ to the inverse image of the shaded region. In blue are the nonzero slopes of the piecewise linear function representing $\frac {1}{3}\psi _1^{\mathtt {trop}}$ and of its pullback to the space of tropical admissible covers. The rays and faces of the space of tropical admissible covers are color coded by the type of cones as in Figure 8.

Figure 10

Figure 10 The type of admissible covers contributing to the computation of the degree of the map $\varphi _1^{{\mathtt {trop}}}$. We have colored the ends that are remembered, as well as the edges whose lengths are relevant for the computation of the degree.

Figure 11

Figure 11 The type of admissible covers contributing to the computation of the degree of the map $\varphi _2^{{\mathtt {trop}}}$. We have colored the ends that are remembered, as well as the edges whose lengths are relevant for the computation of the degree.