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 …

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

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

Greenhouse gas emissions are warming the ocean with profound consequences at all
levels of organization, from organismal rates to ecosystem processes. The proximate driver …

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 …

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 …

With predictions that mass coral bleaching will occur annually within this century,
conservation efforts must focus their limited resources based on an accurate understanding …

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 …

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