The global impacts of climate change are evident in every marine ecosystem. On coral reefs,
mass coral bleaching and mortality have emerged as ubiquitous responses to ocean …

Tip** elements are components of the Earth system which may respond nonlinearly to
anthropogenic climate change by transitioning toward substantially different long‐term …

Climate change impact syntheses, such as those by the Intergovernmental Panel on Climate
Change, consistently assert that limiting global warming to 1.5° C is unlikely to safeguard …

The severity of marine heatwaves (MHWs) that are increasingly impacting ocean
ecosystems, including vulnerable coral reefs, has primarily been assessed using remotely …

As global temperatures continue to rise, shallow coral reef bleaching has become more
intense and widespread. Mesophotic coral ecosystems reside in deeper (30–150 m), cooler …

Internal solitary waves (ISW) are widely distributed worldwide and significantly affect the
ocean environment and offshore activities. ISW propagation speed is important for ISW …

Anomalously high ocean temperatures have increased in frequency, intensity, and duration
over the last several decades because of greenhouse gas emissions that cause global …

Marine heatwaves are triggering coral bleaching events and devastating coral populations
globally, highlighting the need to identify processes promoting coral survival. Here, we show …

The Earth's oceans have absorbed more than 90% of the excess, climate change–induced
atmospheric heat. The resulting rise in oceanic temperatures affects all species and can …

Coral reefs were traditionally perceived as productive hot spots in oligotrophic waters. While
modern evidence indicates that many coral reef food webs are heavily subsidized by …