GACHE / Greenland monitoring study

Greenland Arctic Coral Health Estimator

This work is an estimator for how these deep-sea reefs are performing in today's oceans. We look to estimate the health of these reefs without expensive deep-sea rovers, but instead using sample data & larger ocean health data to answer the question: Can environmental acidification, temperature increase, and surface-level microplastic exposure be used as a predictor of vulnerability in Greenland cold-water coral ecosystems?

Outputs support comparative analysis and should not be interpreted as field observations.

Microplastics in Greenland waters

142 particles/m³

West Greenland surface-water samples, 2019

Study source

Acidification in Greenland fjords

Ωarag 0.28–3.11

West Greenland fjord observations; values below 1 are corrosive

Study source

Ocean temperature near Greenland

Live satellite SST

DMI imagery is updated several times daily

View current SST

Greenland reef outlook

Estimated cold-water coral health over time

Each chart places its environmental driver on the left axis and the GACHE health estimate on the right. The health line now combines the temperature, acidification, and microplastic timelines using a nonlinear multi-stressor risk response.

Model v2: normalized logistic health = logistic(2.9 − cumulative risk), where risk combines thresholded thermal, acidification, and microplastic exposures plus their pairwise interactions. This structure follows coral prediction work that uses nonlinear thermal stress and multi-stressor effects; the Greenland-specific weights are transparent calibration assumptions, not field-fitted coefficients. NOAA heat-stress modelling and multi-stressor Bayesian-network study.

Stressor selection is grounded in cold-water coral experiments showing reduced skeletal growth under microplastic exposure and altered calcification under unfavorable acidification conditions. Microplastic experiment and NOAA cold-water coral acidification study.

Figure 01

Surface temperature → deep-reef temperature

NOAA surface observations are translated to an estimated 886–932 m reef-water temperature using a damped depth-transfer proxy.

Observed surface values: NOAA OISST. Reef-depth temperature context: Meyer et al..

The health line includes all three stressor trajectories. 2026 onward is a linear warming scenario, not an NOAA forecast.

Figure 02

Microplastic contamination

Sparse reported water-column observations from Greenland waters are shown with an illustrative 6% annual continuation scenario.

NOAA Arctic Report Card and West Greenland 2019 observations.

The health line includes all three stressor trajectories. Sampling methods and particle-size thresholds differ between studies; points are not a harmonized monitoring record.

Figure 03

Ocean acidification

A Greenland Sea upper-ocean pH trend is reconstructed from the published 1981–2019 measured decline rate.

Trend source: Acidification of the Nordic Seas (Greenland Sea, 0–200 m).

The health line includes all three stressor trajectories. 2020 onward extends the observed −0.00219 pH/year trend; it is a scenario, not a climate-model forecast.

Figure 04 / Station environmental relationship

Environmental conditions and estimated station health

Each dot is one station. Its health index is calculated with GACHE Model v2: surface temperature is converted to a deep-reef proxy, then combined with ocean pH and microplastic density in a nonlinear multi-stressor response. The line is an OLS fit through those station scores.

Figure 05 / Reference context

Arctic estimate and tropical reef context

This is not a like-for-like health ranking: GACHE's Arctic value is a modelled 0–100 index, while the tropical value is measured global live hard-coral cover. It is shown to give the estimate ecological context.

Global tropical live hard-coral cover was 29.5% in 2019, after an estimated 14% loss since 2009. Source: GCRMN Status of Coral Reefs of the World.