[FIG. 00 / SURFACE]
00 — SURFACE · THE SEA, ANNOTATED

바다는 읽는 것이다. The sea is to be read.

bada.quest reframes the harbor as an instrument panel. Tide charts become progress bars, buoys become icons, shipping lanes become navigation paths. This is a tutorial, not a travelogue.

LAT
37.5000°N
LON
129.1000°E
WIND
04 KT · SW
SWELL
0.6 M
FIG. 00.A — HARBOR / DUSK
Harbor at dusk A flat cream-toned line illustration of a harbor with cranes, lighthouse and a low skyline. A — LIGHTHOUSE B — BUOY 04
[FIG. 01 / TIDE]
01 — TIDE · HOW TO READ A TIDE CHART

A tide is a slow breath.

Twice each day the sea inhales and exhales against the pier. The chart below traces twelve hours of that breath. Hover any vertex to see the exact reading.

FIG. 01.A — TIDE / 12H | UNIT: M | SAMPLE: 30M
12-hour tide curve A sinusoidal tide curve from 06:00 to 18:00 with vertices at 30-minute intervals. 3.0 2.0 1.0 0.0 06:00 09:00 12:00 15:00 18:00 NOW
VERTEX
01.A Vertices sampled every 30 minutes. Hover a node to read its height in meters.
NOTE / 01

Read the slope, not the value.

A single number tells you nothing. The slope between two readings tells you whether the tide is rising or falling, and how fast. The curve's steepest segments mark the strongest currents.

NOTE / 02

Mark the turn.

The flat moments — high water, low water — are not pauses. They are the instant when momentum reverses. A trained eye watches the second derivative.

NOTE / 03

Cross-reference the moon.

Spring tides arrive near new and full moons; neap tides near the quarters. A tide table without a lunar column is missing half the story.

[FIG. 02 / CURRENT]
02 — CURRENT · SURFACE VS SUBSURFACE

Two oceans share one surface.

The wind moves the upper meter. Density and rotation move the rest. A swimmer feels only the first; a fish lives in the second.

02.A — SURFACE

Wind-driven, fast, fickle.

  • DRIVERWIND
  • DEPTH0–1 M
  • SPEED~3% OF WIND
  • SHIFTHOURLY
02.B — SUBSURFACE

Density-driven, slow, steady.

  • DRIVERT & S
  • DEPTH1–4000 M
  • SPEED0.05 M/S
  • SHIFTSEASONAL
FIG. 02.C — FLOW VECTORS | SAMPLE: 12
SURFACE ↑ WIND-DRIVEN DEEP ↓ DENSITY-DRIVEN
02.C Vector field sketches surface (top) versus deep (bottom) flow at noon.
[FIG. 03 / SONAR]
03 — SONAR · LISTENING TO DEPTH

A ping is a question.

The hull asks. The seabed answers in time. Multiply the round trip by half the speed of sound in water, and you have measured the dark.

FIG. 03.A — SONAR / 6S | FREQ: 38 KHZ |
N S W E 40 M 80 M 120 M 160 M
03.A Single ping every six seconds. The radial axis is depth in meters; contacts are buoys, vessels, and reflective seabed features.
DEPTH / SEABED
142.3M
TEMP / SURFACE
14.6°C
SALINITY
34.2PSU
VESSEL TRAFFIC
07✕ / 5KM
[FIG. 04 / LOGBOOK]
04 — LOGBOOK · RETURN TO PIER

Sign the watch.

Leave a line in the harbormaster's logbook and we will write back when the next chart is published. No promises beyond the tide.

ENTRY — 0481 | --:--:-- KST | OBSERVER
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