WIA StandardsKOEN

WIA Deep Sea Exploration Standard Guide

A guide to the WIA-ENE-040 standard

Contents

Chapter 1The Deep Sea as an Operating Environment — Depth Zones, Pressure, Acoustics and PlatformsEvery field in a data standard exists because something in the physical world forces it to. A deep-sea message carries a calibration date on every temperature… Chapter 2Why a Standard — Scope, Architecture and Governance of WIA-ENE-040Chapter 1 described the deep sea as a place: its depth zones, its pressure, the way sound carries and the vehicles that go there. This chapter turns to the… Chapter 3Phase 1 Data Format — Message Envelope, Measurement Packets, Binary Encoding and ArchivesPhase 1 of WIA-ENE-040 is the part of the standard that everything else leans on. The Phase 2 API returns Phase 1 messages, the Phase 3 acoustic stack carries… Chapter 4The Science Record Model — Expedition, Dive, Observation, Sample, Vent and Survey RecordsChapter 3 dealt with the operations layer: messages that a vehicle emits while it works, each wrapped in the Phase 1 envelope and stamped with a sequence… Chapter 5The APIs — Operations API, Records API, SDK and CLIChapters 3 and 4 defined what WIA-ENE-040 data looks like at rest: the Phase 1 message envelope and the science records (expeditions, dives, observations… Chapter 6Phase 3 — The Underwater Acoustic Protocol StackChapters 3 to 5 assumed that a message, once built, somehow reaches its destination. Below the sea surface that assumption fails. Radio does not propagate more… Chapter 7Phase 4 Integration — Research Networks, Repositories, Cloud and Access ControlA dive does not end when the vehicle is back on deck. Its CTD casts have to reach a national archive, its video annotations have to reach the people who… Chapter 8Testing, Conformance, Certification — and What Comes NextThe previous seven chapters described what WIA-ENE-040 asks a system to do: the Phase 1 messages and records, the Phase 2 and records APIs, the Phase 3…

About this book

Every field in a data standard exists because something in the physical world forces it to. A deep-sea message carries a calibration date on every temperature value, a separate accuracy block for position, a pressure range that reaches past one thousand bar and a binary encoding for links that move a few hundred bits per second. None of those choices makes sense until you have a feel for the environment the data comes from. This chapter builds that feel. It is deliberately physical: depth zones, hydrostatic pressure, the temperature and chemistry envelope, the vehicles that operate down there, the sensors they carry, and the acoustics that dominate both communication and seafloor mapping.

You do not need an oceanography background. High-school physics is enough, and every formula is worked through with numbers. Where the WIA-ENE-040 documents or the shipped SDK get the physics wrong, the chapter says so and shows the correct version, because an implementer who copies a wrong formula into a validator will reject good data or accept bad data for years. Readers who already know the ocean can skim sections 1.3 to 1.5 and focus on the pitfalls in 1.1 and 1.2 and the link-budget reasoning in 1.6.