More Than an Emission: How Rising Waste Heat Are Cooking North America

This blog post and the “Deep Dive” podcast, created by NotebookLM, are based on “Energy‐Consumption‐Induced Anthropogenic Heat Release Intensifies Heatwaves and Wildfire Threats in North America: A CESM2‐Based Projection for the Late 21st Century” by Wang et al. (2025). When we talk about climate change, the conversation almost invariably turns to greenhouse gases. Carbon dioxide,... Continue Reading →

Why Rising Seas Could Lower a Hurricane’s Peak Surge—But Drown a Wider Area

This blog post and the “Deep Dive” podcast, created by NotebookLM, are based on “Combined impacts of hurricane strengthening and global mean sea level rise on future Atlantic storm surge events” by Danso et al. (2025). It’s a scenario that seems frighteningly straightforward: as climate change causes sea levels to rise and hurricanes to strengthen,... Continue Reading →

A Critical Ocean Carbon Sink May Reverse, Forming a “CO2 Uptake Hole”

This blog post and the “Deep Dive” and "Critique " podcasts, created by NotebookLM, are based on “Emergence of an oceanic CO2 uptake hole under global warming” by Huiji Lee et al. (2025). Deep Dive Podcast “North Atlantic Carbon Sink Reverses Near-Term” powered by NotebookLM: Two hosts provide a critical analysis and constructive feedback to... Continue Reading →

Solving the Mystery of the Great Atlantic Sargassum Belt: 5 Surprising Truths

This blog post and the “Deep Dive” podcast, created by NotebookLM, are based on “Equatorial upwelling of phosphorus drives Atlantic N2 fixation and Sargassum blooms" by Jung et al. (2025). Deep Dive Podcast “Climate History Solves Sargassum Crisis”: Introduction: The Golden Tide Mystery Since 2011, a mysterious phenomenon has plagued the coastlines of the Caribbean,... Continue Reading →

Sustained ocean measurements at 34°S crucial for estimating the distance to an AMOC collapse

The Atlantic Meridional Overturning Circulation (AMOC) transports warm and salty upper ocean water to the subpolar North Atlantic where the upper ocean releases some heat to the atmosphere. Due to the surface cooling and the high salinity (i.e., salty), the upper ocean water becomes heavier and thus sinks down to the deep ocean and then... Continue Reading →

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