Coastal vegetated habitats such as seagrasses, salt marshes, and mangroves are among the most effective natural systems for capturing and storing carbon in the ocean, collectively known as blue carbon […]
Nitrogen is a crucial nutrient for biological productivity in the upper ocean, and its cycling is sensitive to global climate. The stable nitrogen isotopic ratio (i.e., 15N/14N ratio, or δ15N) […]
We invite you to join us on Thursday, September 25, 2025 at 16:00 KST with speaker Dr. Stacy Carolin from the University of Oxford, UK. This online speleothem lecture series at the IBS Center for Climate Physics, Busan, South Korea welcomes […]
Climate stabilization scenarios limiting global warming to 1.5-2℃ targets generally require augmentation of natural atmospheric CO2 removal with additional carbon dioxide removal (CDR) around 2-3 PgC year-1 solutions sustained over […]
Since the Industrial Revolution, the global average annual temperature has risen by 1.09ºC by 2020. According to the 6th Intergovernmental Panel on Climate Change report, the ongoing global warming is […]
In 1961, Klaus Wyrtki published a landmark study [1], in which he laid out the foundation of our modern understanding of the thermohaline circulation. The only problem was that the […]
Extensive modeling evidence indicates the relationship between projected temperature changes and the expected increase in heat-related mortality and morbidity. While the link between temperature and climate-sensitive health outcomes may appear […]
The influence of El Niño-Southern Oscillation (ENSO) on Australian rainfall varies with its Eastern Pacific (EP) and Central Pacific (CP) types. Here we revisit the EP/CP ENSO’s impact on Australian […]
Past climate aberrations provide unique insight into climate-carbon cycle feedbacks in the Earth System on time scales extending far beyond the instrumental record. In this presentation, I will focus on […]
Abstract: Past glacial periods were characterized by pronounced millennial-scale climate variability, mainly associated with Dansgaard-Oeschger (DO) and Heinrich events, while climate during warm interglacial periods is much more stable. While […]