I have a question about the intuition behind Grothendieck's proposed notion of so called "Tame topology" in his Esquisse d’un programme. Grothendieck insisted that theory should admit “dévissage of stratified structures", see e.g. here or here arXiv:1603.03016.
Question: How should one think on intuitive level of this “dévissage of stratified structures"?
The philosophy behind of the concept of usual dévissage I'm familar with deals roughly with deciding when say for a fixed space $X$ and $C(X)$ be an additive category of "nice" objects naturally attached to $X$ (eg is $X$ a scheme, $C(X)$ could be the cat of coherent $O_X$-modules), and $A \subset \text{ob}C(X)$ subset of the objects of $C(X)$ satisfying (context depending additional properties; archetypical property would be eg the $2$-of-$3$-property ) and devissage results are dealing with metastatements when $A$ actually equals $C(X)$.
Now, which intuition one should have for "dévissage of stratified structures"? Say we have a stratified space ( in reasonble sense) $\emptyset =X_{-1} \subset X_0 \subset X_1 \subset ... \subset X_n =X$ and want to build up inductively the knowledge about $X$ from it's strata pieces step by step. So say wlog $X=X_1$ and we "understand" already the pieces $X_0$ and $X_1 - X_0$.
So far I understand the idea & goal of "dévissage of stratified structures" should be results of type to deduce from information from the pieces $X_0$ and $X_1 - X_0$ something about $X (=X_1)$.
But what kind of "information" about $X$ one expects to deduce via this "stratified dévissage"? Say, how would such archetypical metastatement from "dévissage of stratified structures" look like?
Is it of "strong" form (= full amount of information about $X$) in the sense that of we understand $X_0$ and $X_1 - X_0$ + these pieces satisfy certain "dévissage condition" which one might interpret as kind of "glueing data", then it suffice to reconstruct $X$ "totally" up to isomorphy type (that's why "strong" form; the picture I have in mind is eg the Morse theory)
Or does this stratified dévissage works as "weak" form, so in similar vein to the business with $C(X)$ as above? Namely, it not focussed on "reconstructing completely" $X$ as in strong form from strata pieces $X_0$ and $X_1 - X_0$, but just some weaker data functorially associated with $X$ incarnating metastaments more of following kind:
Say we have again as before $C(X)$ (resp. $C(X_0)$ and $C(X_1 - X_0)$) be an additive category of "nice" objects naturally attached to $X$ (resp to $X_0$ and $X_1 - X_0$) and canonical maps $C(X_0) \to C(X) \to C(X_1 - X_0) $ (...so in most reasonable cases $C$ comes functorially, so as presheaf; think of functoriality of $K$-theory with Grothendieck groups).
And my naively guess is that this "weak form" of Grothendieck's "devissage of stratified structures" deals with questions when objects in $C(X)$ can be constructed from objects from $C(X_0)$ and $C(X_1 - X_0)$, so extension problem in terms of homological algebra.
So my question boils down to which form (strong vs weak) Grothendieck refers by "dévissage of stratified structures" in his "Esquisse d’un programme"?