Global Environmental Risks & Planetary Boundaries Monitor
Weekly strategic intelligence on Earth system risk, planetary boundary status, tipping points, and geopolitical cascades from environmental stress. Published every Saturday.
The confirmed strengthening of El Nino into a strong event for July through September 2026 raises multi-region food security and water stress risk across the Maritime Continent, southern Asia, the Car
The confirmed strengthening of El Nino into a strong event for July through September 2026 raises multi-region food security and water stress risk across the Maritime Continent, southern Asia, the Car
Sustained three-month record heat sequence (May to July 2026) combined with a lowered Amazon degradation threshold indicates the climate change and land-system change boundaries are now interacting no
The Nordic Seas Overturning Circulation strengthening is confirmed by PIK to be a symptom of AMOC weakening rather than a stabilising counter-signal, and may itself be a precursor to eventual collapse
El Niño onset in context of already-elevated baseline SST represents non-linear acceleration of climate change boundary rather than discrete crossing; super El Niño trajectory by September will compou
The June 2026 European heatwave represents a structural threshold in climate risk manifestation: formal attribution confirms the event was virtually impossible without anthropogenic forcing, and polit
The 1.5°C carbon budget exhaustion timeline of approximately 3 years at current emission rates creates acute pressure on NDC compliance cycles and compresses adaptation windows for climate-fragile sta
AMOC slowdown has crossed from modelling-only to observationally grounded trajectory assessment, with meridionally consistent decline confirmed across four independent Atlantic mooring arrays and irre
AMOC slowdown has crossed from modelling-only to observationally grounded trajectory assessment, with meridionally consistent decline confirmed across four independent Atlantic mooring arrays and irre
AMOC slowdown has entered structural lock-in phase where enhanced North Atlantic salinity variability persists even under climate mitigation because ocean circulation recovers slowly, creating irrever