Enter an event-first sea under archived climate context.
Some bodies are carried away. Some keep a local loop. Some remain in the boundary layer.
This is not a daily playback map. It is a spatial responder: event tracer templates remain first, while replay date, episode, and climate frame lightly modulate the surrounding sea.
Not a spreadsheet. Each event is read as a tidal strip: who is pulled into the main current, who keeps a loop, and who stays in the boundary layer.
Read the deformation of the shared field: one body dissolves into the current, one gathers water into a local vortex, and one unsettles the boundary layer.
2020-03-18 / Three different ways to remain in the same sea.
Energy is taken by the dominant current, tech still folds into a local loop, and commodity holds a boundary-layer trace rather than a clean absorption.
XOM
TSLA
CL=F
Local bodies do not float on black emptiness. They sit inside nested seas: a slow global ocean, sector currents, and the local bodies whose transport we are reading.
A broad reference sea beneath the event field: a way to read shared movement before local residuals separate.
Proxy comparison fields rendered as directional pulls for reading. The directions orient relation; they are not measured force vectors.
Current state in the field, not an asset category.
This is where the page finally sinks beneath the theater surface. Metrics, canonical residuals, best fields, null competition, and all-asset notes belong here, not in the entrance screen.
The deep layer is where the compressed reading reconnects to the audit machinery: explicit best field, canonical deep residual, and the observational boundary around null competition.
Each available body is summarised from the generated event set: how often it is absorbed, partly retained, or left in a boundary reading.