Since the end of the last ice age around 11.000 years ago, the isostatic sea level is rising due to warming climate and melting of the glaciers. Stone-Age hunter-gatherer groups, […]
The rapid decline of polar sea ice under accelerating global warming is increasingly recognized as a key factor influencing albedo feedback and large-scale ocean circulation. In particular, recent sea ice […]
In this presentation, I will discuss some of the work I have been doing to reconstruct the history of the last glacial cycle (120-6 kyr BP). First, I will introduce […]
This talk presents a new statistical framework for evaluating climate models that captures three key features of climate time series: multivariate dependence, temporal correlation, and the response to external forcings. […]
When a large task is divided into several smaller subtasks, and these subtasks are allocated to different people or groups, then the system is called a division of labour. Division […]
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 […]