Global Ocean Accounts Partnership Secretariat · GOAP Technical Guidance on Ocean Accounting · circular

Physical Condition Measurement

Responsible officer: Dr Jordan GacutanDrafting: AI-assisted drafting from GOAP Secretariat source materials; source list to be published at the close of consultation.
GOAP Technical Guidance

Version 0.8.1 · 1 September 2026Draft for consultation — not final guidance and not to be cited as adopted
CC BY-NC 4.0

Framework position: TG-4.8 sits in the data methods layer. It provides the measurement protocols and variable selection guidance for physical state variables that feed upstream into the ecosystem condition indicators described in TG-2.1 and TG-2.8, and from there into asset accounts compiled under TG-3.1. Users compiling condition accounts should read this Circular alongside TG-4.9 Biological Condition Measurement, which covers the biotic counterpart to the abiotic variables described here.

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Framework Position

TG-4.8 sits within Section 4 (Data Methods). It owns the abiotic condition variable — ECT Classes A1 and A2 — from selection through measurement protocol, data source and tier, reference condition, and rescaling to a dimensionless 0—1 score against that documented reference, with its uncertainty. It does not own what is built from those scores. Combining variables into an ECT-class or overall condition index is TG-2.1 Aggregate Biophysical Indicators of Environmental State; the SEEA EA Table 5.2 condition account is TG-3.1 Asset Accounts Section 3.5.2. Biotic variables are TG-4.9 Biological Condition Measurement.

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This Circular provides guidance on measuring the physical condition of ocean and coastal ecosystems for use in SEEA EA ecosystem condition accounts. On completing this Circular, users will be able to select appropriate physical state variables, establish reference conditions, rescale variables to dimensionless condition indicators on a 0—1 scale, and integrate physical condition data into the asset account structure defined in TG-3.1 Asset Accounts.

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Physical condition measurement addresses the abiotic subset of ecosystem condition (temperature, salinity, dissolved oxygen, pH, turbidity, nutrients, and light attenuation), corresponding to ECT Classes A1 and A2 as defined in SEEA EA Table 5.1. This Circular does not cover biological condition variables (covered by TG-4.9) or the compilation of condition account tables (covered by TG-3.1).

Users should be familiar with the following circulars before working through this guidance:

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  • TG-0.1 General Introduction to Ocean Accounts — for the overall structure and purpose of ocean accounts
  • TG-0.6 Glossary of Key Terms — for canonical definitions of “condition variable”, “condition indicator”, and “reference condition”
  • TG-0.7 Quality Assurance Principles — for data quality, metadata, and uncertainty documentation requirements
  • TG-4.1 Remote Sensing and Geospatial Data — for satellite sensor selection, pre-processing, and spatial data handling
  • TG-4.5 Integrating Research Data into Official Statistics — for admitting in-situ oceanographic survey and monitoring data, including quality thresholds, spatial interpolation, and cross-validation
  • TG-4.4 Citizen Science and Community-Based Monitoring — for citizen science and community-based monitoring data in data-poor contexts
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Physical condition measurement is anchored in SEEA EA Chapter 5, which establishes the Ecosystem Condition Typology (ECT), the concept of reference condition, and the rescaling of state variables to dimensionless condition indicators on a 0—1 scale. Physical condition captures the abiotic state of the ocean environment. The SEEA EA Ecosystem Condition Typology (Table 5.1) groups condition characteristics into three groups and six classes — Group A (abiotic) with classes A1 and A2, Group B (biotic) with classes B1 to B3, and Group C (landscape) with class C1. Abiotic condition is the two classes of Group A:

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  • ECT Class A1 — Physical state characteristics: the thermal, hydrodynamic and optical properties of the water column (temperature, salinity, water clarity, stratification).
  • ECT Class A2 — Chemical state characteristics: the chemical composition of the water column (pH and aragonite saturation, dissolved oxygen, dissolved inorganic nutrients).

Class labels follow SEEA EA Table 5.1 exactly. TG-3.1 Asset Accounts Section 3.5.2 uses the same six classes, and a variable must carry the same class label in both circulars.

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Physical condition is distinct from biological condition (TG-4.9 Biological Condition Measurement): physical variables measure the abiotic habitat envelope within which organisms live, whilst biological variables capture the biotic response of living organisms to that environment. Both are components of ecosystem condition as defined by SEEA EA Chapter 5 and both feed into asset accounts (TG-3.1 Asset Accounts).

Reference condition is the baseline against which current state is compared. SEEA EA paras 5.65—5.75 and Appendix A5.2 establish four approaches, and this framework is canonical for both physical and biological condition accounts (TG-4.9 cross-refers here).

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Fixed reference condition for time-series accounts. For time-series accounting, the reference condition value for each indicator must be fixed at the start of the series and held constant across all subsequent periods. Revisions are permitted only at a formally documented major methodological review and require complete re-compilation of the historical series from the new baseline. Document the reference-condition vintage (year established) in account metadata. New accounting units introduced mid-series establish their own baseline at first measurement, and are flagged as a new series start.

Ecosystem-specific physical priorities vary by habitat type:

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For detailed habitat-specific guidance, see TG-6.1 Coral Reef Ecosystem Accounting, TG-6.2 Mangrove and Coastal Wetland Accounting, TG-6.3 Seagrass Ecosystem Accounting, and TG-6.5 Pelagic and Open Ocean Accounting.

Indicators are selected according to four criteria set out in SEEA EA paras 5.22—5.27. Table 3.2.1 below summarises these criteria.

Recommended physical condition indicators by ECT class

ECT Class A1 — Physical state characteristics

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  • Sea Surface Temperature (SST): primary indicator of thermal stress and climate forcing. Unit: °C. Reference condition: long-term climatological mean (e.g., the 1985—2012 NOAA Coral Reef Watch CoralTemp climatology). Where the full 1985—2012 period is unavailable nationally, use the longest consistent national record as the reference baseline, document the period explicitly in metadata, and note the departure from the global standard baseline. Rescaling: temperature anomaly relative to baseline. The condition indicator decreases as anomaly increases above the reference variability range. For coral reef accounting units: threshold-based rescaling using the Maximum Monthly Mean (MMM) climatology is the preferred approach. When sea surface temperature exceeds the MMM, Degree Heating Weeks (DHW) begin to accumulate, and DHW ≥ 8°C-weeks corresponds to significant bleaching risk. The MMM/DHW method is the global operational standard for bleaching heat-stress monitoring.

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NOAA Coral Reef Watch provides ready-to-use global 5-km DHW and MMM products. The same indices can equally be derived from Copernicus Marine Service (CMEMS) or ESA Climate Change Initiative (CCI) SST inputs where an alternative provider is preferred.

  • Salinity: indicator for estuarine and coastal boundary zones. Unit: practical salinity units (PSU). Reference condition: long-term climatological mean from WOA or ARGO programme for the accounting unit.
  • Water clarity / light attenuation (Kd490): relevant for seagrass and coral light requirements. Unit: m⁻¹. Reference condition: site-specific long-term mean from satellite ocean colour products. Condition indicator decreases as Kd490 increases beyond the reference level (higher attenuation = reduced light penetration = poorer condition).
  • Mixed layer depth (MLD): indicator of ocean stratification and vertical mixing, relevant for pelagic and open-ocean accounting units. Unit: metres. Reference condition: long-term climatological mean MLD from ARGO programme or CMEMS reanalysis.

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    Shoaling of MLD beyond the climatological range indicates increased stratification, which constrains nutrient upwelling and affects productivity. Condition indicator decreases as MLD shoals beyond the climatological reference range. Source: ARGO programme density profiles; CMEMS physical reanalysis products. See TG-6.5 Pelagic and Open Ocean Accounting for guidance on MLD in pelagic condition accounts.

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    ECT Class A2 — Chemical state characteristics

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    • Ocean pH / aragonite saturation (Ω): indicator of ocean acidification state. Unit: pH units (dimensionless Ω). Reference condition: pre-industrial pH (~8.18) or a regional multi-decadal baseline from SOCAT/GLODAP. Condition indicator decreases as pH declines or Ω falls below the aragonite saturation threshold (Ω = 1), below which shell-forming organisms cannot maintain calcified structures.
    • Dissolved oxygen (DO): indicator of habitat viability and eutrophication stress. Unit: mg/L or % saturation. Hypoxia threshold: <2 mg/L (below which most marine fauna cannot persist). Reference condition: site-specific or regional historical baseline.
    • Dissolved inorganic nutrients (NO₃, PO₄): eutrophication indicators for coastal zones. Unit: μmol/L. Reference condition: oligotrophic background level for the relevant ocean region. Condition indicator decreases as nutrient concentrations exceed reference levels.
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    Tiered indicator selection approach

    Indicator selection follows a three-tier framework based on data availability. The tiering draws on the graduated capacity framework described in TG-0.7 Quality Assurance Principles. Table 3.2.2 below summarises the three tiers.

    Rescaling and aggregation pathway

    The transition from raw measurement to reported condition indicator follows three steps, consistent with SEEA EA paras 5.44—5.58. Figure 4.8.1 traces the pathway from a raw ECT Class A1 or A2 variable, through quality control and benchmarking against the reference condition, to a rescaled and aggregated SEEA EA Table 5.2 condition account row. Table 3.2.3 below summarises these steps.

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    · Figure 4.8.1

    Pathway from an ECT Class A or B variable through quality check, reference benchmarking, rescaling, and aggregation to a SEEA EA Table 5.2 row. Four reference-condition approaches; regulatory or management target is least preferred.

    TG-4.8 -- Physical condition indicator construction pathway The physical condition measurement pathway runs left-to-right. A raw Ecosystem Condition Typology (ECT) Class A or B variable is combined with a reference condition drawn from one of four approaches -- historical benchmark, reference site, modelled potential, or a regulatory / management target (flagged least preferred) -- at a fan-in junction. The combined signal is rescaled to a unitless 0--1 condition index, then aggregated across indicators, and the result is entered as a row in the SEEA EA Table 5.2 ecosystem condition account. Nodes are coloured by data role: raw input (cyan/secondary), compilation or transformation step (emerald/process), and account output (teal/anchor). Condition indicator construction pathway Reference condition (choose one approach) Historical Pre-disturbance benchmark value Reference site Least-disturbed analogous site Modelled Simulated potential condition estimate Regulatory target Policy-defined (MPA recovery, GBF Target 3) least preferred Raw ECT variable Class A or B indicator from monitoring data Quality check IOC-UNESCO/IODE QA/QC screen Rescale to 0--1 index Dimensionless condition score vs reference Aggregate Weighted mean across ECT characteristic groups SEEA EA Table 5.2 row Condition account entry for reporting input passed index score reference (V_ref) Raw input Quality gate Compilation / transformation Account output (SEEA EA)

    Source TG-4.8, §3.1--3.5 (conceptual framework, indicator selection, measurement & integration); ECT Class A/B structure per SEEA EA 2024 Table 5.1; reference-condition approaches per SEEA EA 2024 §§5.65--5.75 and Appendix A5.2.

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    In-situ measurement

    CTD (conductivity-temperature-depth) casts provide vertical profiles of temperature, salinity, and (where equipped) dissolved oxygen and fluorescence. Moored buoys record continuous surface and sub-surface time series. ARGO profiling floats provide open-ocean profiles to 2,000 m depth with near-real-time transmission. Repeat hydrography programmes (WOCE/GO-SHIP sections) supply basin-scale reference data for calibration.

    For coastal and estuarine zones, national tide gauge networks, fixed moored sensors, and periodic survey cruises provide the primary in-situ data. Water sampling for nutrient and pH analysis should follow IOC-UNESCO/IODE standard operating procedures, including certified reference materials for pH (NOAA-distributed CRMs) and oxygen (Winkler titration).

    Remote sensing

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    Satellite-derived SST (MODIS Aqua, AVHRR, Sentinel-3 SLSTR) provides daily global coverage with approximately 1 km spatial resolution. Ocean colour products (MODIS Aqua, SeaWiFS, Sentinel-3 OLCI) deliver Kd490 and turbidity estimates at 300 m — 4 km resolution. Gap-filling via optimal interpolation (OI) is standard for SST products (NOAA OISST, CMEMS, GHRSST Level 4). See TG-4.1 Remote Sensing and Geospatial Data for sensor selection and pre-processing protocols.

    Tiered minimum time requirements

    Table 3.3.1 below summarises the minimum time-coverage requirements for each tier.

    Abiotic SOP references

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    The standards listed in Table 3.3.2 are the canonical SOPs for the abiotic variables enumerated in Section 3.2. Compiling agencies should record the cited standard (and its version/year) in metadata for each variable per TG-0.7 Quality Assurance Principles. Documented departures from the SOP (sampling depth, replication, gear substitution) should be recorded alongside the measurement. Satellite-derived alternatives are listed in the remote-sensing subsection above and in Table 3.4.

    Quality control and data-poor contexts

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    Apply IOC-UNESCO/IODE QA procedures (anomaly flagging, measurement precision, gap-filling documentation) within the TG-0.7 framework. All stations georeferenced to WGS84. Annual composites are the minimum for accounts. Where national in-situ programmes are limited, global reanalysis (CMEMS, ERA5-ocean, WOA) is a viable Tier 3 alternative. Document source, version, and known biases, especially in shallow coastal and enclosed seas. Supplement with TG-4.4 Citizen Science data where coverage is sparse.

    3.4 Data Requirements and Sources

    The following matrix specifies the minimum data requirements for each recommended physical condition indicator:

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    Key institutional data sources: Copernicus Marine Service (CMEMS), NOAA CoastWatch, NOAA Coral Reef Watch, IMOS (Australia), ICES Data Centre, IOC-UNESCO IODE, national oceanographic institutes, national meteorological services, Argo Data Assembly Centres (GDAC).

    Known data limitations:

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    • Sparse in-situ coverage in developing-country EEZs creates reliance on Tier 2—3 products with higher uncertainty.
    • Satellite retrievals are degraded by cloud cover, sun glint, river plumes, and coastal adjacency effects within approximately 1 km of the shoreline.
    • Reanalysis products may not resolve sub-mesoscale processes in enclosed seas, shallow bays, or areas of strong tidal forcing.
    • BGC-ARGO pH and oxygen profiles are sparse in coastal and shelf regions, whilst WOD/GLODAP cover is more complete in the open ocean.
    • MLD estimates from density profiles are sensitive to the threshold criterion applied (density or temperature criterion), and the criterion used must be documented for reproducibility.
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    Compiling agencies should document data source, product version, spatial resolution, and temporal coverage for every variable in the condition account metadata. See TG-4.6 Data Harmonisation and Interoperability for guidance on integrating data from multiple sources.

    3.5 Reporting and Integration

    Reporting format

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    Each physical condition variable is delivered with the following fields: ECT class, variable name, unit of measurement, reference condition value, current condition value, and rescaled condition indicator (0—1 scale). Arranging those fields as rows of the SEEA EA Table 5.2 condition account is done in TG-3.1 Asset Accounts Section 3.5.2; combining variables into an ECT-class or overall condition index is TG-2.1 Aggregate Biophysical Indicators of Environmental State. This Circular is responsible for the variable and its rescaling to a 0—1 score against a documented reference, not for the aggregate or the account.

    Rescaling formula

    For variables where higher values indicate better condition (e.g., dissolved oxygen, aragonite saturation):

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    CI = (V — V_min) / (V_ref — V_min)

    For variables where lower values indicate better condition (e.g., temperature anomaly, nutrient loading, turbidity):

    CI = 1 — [(V — V_min) / (V_max — V_min)]

    Where:

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    • CI = condition indicator (0—1 scale; 1 = at or above reference condition; 0 = fully degraded or absent)
    • V = observed variable value for the accounting period
    • V_ref = reference condition value (the value of the variable under the chosen reference condition)
    • V_min = minimum observed value or ecologically meaningful lower bound (e.g., 0 mg/L for dissolved oxygen; Ωaragonite = 0; pH = 7.75). Examples by variable: dissolved oxygen V_min = 0 mg/L; Ωaragonite V_min = 0; pH V_min = 7.75; temperature anomaly V_min = 0. Compiling agencies must document the V_min and V_max values applied for each variable, and deliver them alongside the variable.
    • V_max = maximum observed value or ecologically meaningful upper bound (used in negative-condition formula only)
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    For binary threshold indicators (e.g., DO hypoxia): CI = 1 if V ≥ threshold (2 mg/L), and CI = 0 if V < threshold (step rescaling). Figure 4.8.2 works a numerical example of these formulas: continuous-variable rescaling (an SST anomaly on a coral reef unit) and threshold (step) rescaling (dissolved oxygen about the hypoxia threshold). Its third panel shows, for orientation only, where the delivered scores go — the ECT-class aggregate and the Table 5.2 rows are compiled under TG-2.1 and TG-3.1 respectively, not here.

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    · Figure 4.8.2

    Panels A and B show the rescaling this Circular performs: continuous rescaling and threshold rescaling. Panel C shows where the resulting scores go -- ECT Class A aggregation and SEEA EA Table 5.2 rows, both compiled elsewhere. Observed values and weights are illustrative.

    TG-4.8 -- Worked example: from raw variable to condition account row A three-part worked example. Panel A (continuous-variable rescaling) carries a sea surface temperature anomaly for a coral-reef accounting unit through the SEEA EA negative-condition formula: an observed annual mean of 30.2 degrees Celsius against a maximum-monthly-mean reference of 29.0 gives a +1.2 anomaly, which with bounds V_min 0 and V_max +2.0 rescales to a condition indicator of 0.40 on the 0--1 scale. Panel B (threshold rescaling) shows the binary step rule for dissolved-oxygen hypoxia: condition equals 1 when oxygen is at or above the 2 milligrams-per-litre threshold and 0 when below, illustrated by an oxygenated case of 5.4 and a hypoxic case of 1.3. Panel C (where the scores go) shows, for orientation, the downstream use of the delivered scores: three ECT Class A indicators combined by weighted mean to a class condition index of 0.63 under TG-2.1, and the variables recorded as SEEA EA Table 5.2 condition-account rows under TG-3.1 Section 3.5.2. Neither step is compiled in TG-4.8. Worked example: from raw variable to condition account row A. Continuous-variable rescaling What it represents: turning one raw measurement into a dimensionless 0--1 condition score against a reference. Worked variable: sea surface temperature, coral-reef unit. Inputs Observed SST = 30.2 °C Reference (MMM) = 29.0 °C → anomaly V = +1.2 °C V_min = 0 °C (at MMM) V_max = +2.0 °C (reef-collapse) Rescale -- negative-condition form (§3.5) CI = 1 - (V - V_min) / (V_max - V_min) = 1 - (1.2 - 0) / (2.0 - 0) = 1 - 0.60 Lower SST is better → negative form. Condition indicator (CI) CI = 0.40 0 1 0--1 condition scale B. Threshold (step) rescaling What it represents: pass/fail variables that score 1 above an ecological threshold and 0 below it. Worked variable: dissolved oxygen, hypoxia. Rule -- step rescaling (§3.5) CI = 1 if DO ≥ 2 mg/L CI = 0 if DO < 2 mg/L Case 1 -- oxygenated DO = 5.4 mg/L 5.4 ≥ 2 → CI = 1.00 Case 2 -- hypoxic DO = 1.3 mg/L 1.3 < 2 → CI = 0.00 C. Where the delivered scores go Downstream use, shown for orientation: indicator scores are combined into an ECT-class index under TG-2.1 and recorded as SEEA EA condition account rows under TG-3.1 Sec. 3.5.2. Aggregate ECT Class A (weighted mean) SST anomaly CI 0.40 w 0.40 pH / arag. CI 0.72 w 0.30 turbidity CI 0.85 w 0.30 Class A condition index = 0.63 = 0.40×0.40 + 0.72×0.30 + 0.85×0.30 SEEA EA Table 5.2 -- ECT Class A condition rows Variable Unit V_ref Current CI Sea surface temperature °C 29.0 30.2 0.40 Dissolved oxygen mg/L ≥ 2 5.4 1.00 ECT Class A index 0.63 Reference baselines and ecological thresholds follow published literature (see caption). Observed values, and the pH and turbidity scores in Panel C, are illustrative. Raw input Compilation / transformation Threshold rule Below threshold Account output (SEEA EA)

    Source TG-4.8 §3.5 (rescaling, bounds, binary threshold); TG-2.1 (aggregation); TG-3.1 §3.5.2 (condition account); SEEA EA 2024 §§5.44--5.58 and Table 5.2. Baselines: Liu et al. 2014 (MMM/DHW); IPCC 2018 / Frieler et al. 2013 (+2°C); Diaz & Rosenberg 2008 / Vaquer-Sunyer & Duarte 2008 (2 mg/L hypoxia).

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    Where current condition exceeds the reference baseline (CI > 1 in the positive-condition formula), CI is delivered as 1.0 and the raw calculated value is recorded in the accompanying metadata. A CI above 1 can arise where recent conservation gains have improved condition above the historical reference.

    Integration with biological condition

    Physical variables establish the abiotic habitat envelope for TG-4.9 indicators. Joint reporting of SST, DO, turbidity, and pH enables attribution analysis (e.g., distinguishing thermal stress from direct anthropogenic impact).

    Uncertainty reporting

    Each indicator requires measurement-uncertainty, representativeness, and model-uncertainty components, plus the data tier (1—3) and gap-filling method. Metadata documentation follows TG-0.7.

    Authors: [To be confirmed]

    Reviewers: [To be confirmed]

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    Cite this report

    Physical Condition Measurement

    Physical Condition Measurement (2026) (GOAP Technical Guidance on Ocean Accounting, TG-4.8, v0.8.1). GOAP Secretariat. https://guidance.oceanaccounts.org/circulars/section-4/4-8-physical-condition-measurement/

    guidance.oceanaccounts.org/circulars/section-4/4-8-physical-condition-measurement

    © 2026 Global Ocean Accounts Partnership Secretariat · CC BY-NC 4.0 · The report, its PDF and this deck are built from the same source.

    GOAP Technical GuidanceVersion 0.8.1 · 1 September 2026