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Two special seminars

Time

02. October 2025, 22:00-22:00

Location

BCCR lecture rom 4020, Jahnebakken 5

Dear all,

 

We are fortunate to have Gokhan Danabasoglu (NCAR) and Jon Robson (NCAS/U. Reading) visiting next week, and they will be giving back-to-back seminars on Friday 2nd October, BCCR seminar room 4020.

 

10:00 - 10:50, High-Resolution Simulations with the Community Earth System Model (CESM), Gokhan Danabasoglu

 

As impacts of climate change are being felt by the society through sea level rise, increased intensity and occurrences of heat waves, droughts, extreme rainfall events, and tropical cyclones (TCs), decision makers and stakeholders need reliable weather and climate information at increasingly finer spatial and temporal scales. There are also numerous science questions regarding representation of and changes in importance of various processes with increased model resolution. It is generally anticipated that with less reliance on uncertain parameterizations and their parameter choices, high-resolution (HR) models will represent various processes and coupled interactions of the Earth system with increased fidelity. To address these needs and challenges, we have made significant advances in HR global Earth system modeling and predictions. Specifically, we have performed an unprecedented set of simulations at a TC-permitting (0.25°) and ocean-eddy-rich (0.1°) horizontal resolution using the Community Earth System Model (CESM-HR). The presentation will introduce these simulations and provide a few highlights from our extensive analysis. While not a panacea to address all model biases, the HR simulations certainly offer promising improvements with reduced biases in comparison with their low-resolution counterparts and advance our understanding of processes. 

 

11:00 - 11:50 Understanding model uncertainty in North Atlantic multi-decadal variability and change,  Jon Robson

 

Changes in the North Atlantic Ocean play an important role in shaping regional weather and climate. Yet climate models differ widely in how they represent both the response to external forcing and internal variability on multi-decadal timescales. These differences contribute to substantial uncertainty in how we might expect the North Atlantic to evolve in the coming decades. In this talk, I will highlight key uncertainties in our understanding of variability and change in the region. Focusing on two central issues—the Atlantic Meridional Overturning Circulation (AMOC) and multi-decadal variability in the tropical North Atlantic—I will discuss some ongoing efforts to untangle the underlying processes and make progress toward reducing uncertainty.

 

 

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Abstract Glacial inception is commonly interpreted as a response to declining summer insolation, which reduces ablation and allows perennial snow to accumulate. How the controls on ice-sheet growth evolve after this initial phase, however, is less well understood. Here, we analyze a transient simulation of the last glacial inception from 127 to 65 ka using the AWI Earth System Model (AWI-ESM) coupled to the Parallel Ice Sheet Model (PISM) for the Northern Hemisphere domain. Our results show two stages of Laurentide Ice Sheet (LIS) growth. During the early phase (127–115 ka), glaciation is mainly associated with reduced summer melt and follows the southward migration of the summer 0 °C isotherm. After approximately 115 ka, this relationship changes and the ice sheet margin continues to advance into regions with negative surface mass balance. A decomposition of changes in local ice thickness indicates that dynamic mass redistribution from the interior to the margin supports this advance. Changes in LIS surface elevation are associated with changes in regional moisture transport and an increasing fraction of precipitation falling as snow over parts of the ice sheet help maintain a positive surface mass balance in the interior. Our simulation indicates a transition from early, climate-limited glaciation to dynamically supported growth, in which local climate conditions no longer determine ice-sheet advance. Although the timing and magnitude of this transition depend on the experimental setup, our results show how an evolving ice sheet can shift the relative roles of melt, accumulation, and ice dynamics during glacial inception. Speaker information Lars Ackermann is a postdoctoral researcher in the Paleoclimate Dynamics section at the Alfred Wegener Institute (AWI). He received his PhD from the University of Bremen in 2023 and has been part of the PalMod project (Paleo Modelling) since 2020. His research focuses on long-term climate–ice sheet interactions, particularly the role of the Greenland Ice Sheet and icebergs in past and future climate change. Using coupled climate–ice sheet modelling, he investigates ice sheet evolution and its impacts on ocean circulation and the wider climate system over centennial to millennial timescales. Join Zoom Meeting https://uib.zoom.us/j/68304284910?pwd=2IgsDMWHuJlQw3XFHSTo3OoGBsRrhz.1 Meeting ID: 683 0428 4910 Password: 7pwZK4mG
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