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) […]

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 […]