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Portrait photo of Nadja Omanovic in front of a modern glass building.

Humboldt Fellow Nadja Omanovic Conducts Research on Arctic Clouds

Nadja Omanovic, a postdoctoral researcher in the Lise Meitner Research Group “Multiscale Cloud Physics,” is studying the impact of Arctic clouds on…

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Which Mechanisms Control the Temperature Trend in the Tropical Pacific?

According to climate projections, the eastern tropical Pacific will warm up in the long term, but the opposite is currently being observed. A new…

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Clara Bayley Conducts Postdoctoral Research as Part of the Susanne Hasselmann Fellowship

Clara Bayley, recent graduate of the IMPRS-ESM program, is conducting postdoctoral research on the microphysics of tropical clouds using a numerical…

Johannes Gerhardt, Johanna Baehr, Lara Wallberg and Sven Bethune in formal attire.

Lara Wallberg Receives Böttcher Award

Lara Wallberg was honored with the Johann Max Böttcher Award for her innovative research on the variability of hot summers in Europe. The Max Planck…

Katharina Fegebank next to Jochem Marotzke, who is holding a certificate and wearing the Order of Merit.

Jochem Marotzke Honored with the Federal Cross of Merit

Jochem Marotzke, director at the Max Planck Institute for Meteorology, has been awarded the Cross of the Order of Merit of the Federal Republic of…

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New Study Provides Empirical Evidence of Human Influence on Regional Climate Change

Climate change is affecting the entire planet—and yet different regions are warming at different rates. Where is human-induced warming already clearly…

Our Research

PhD positions in Climate Research - Annual Call 2027 open 1 July to 15 September

The International Max Planck Research School on Earth System Modelling (IMPRS-ESM) is a structured, interdisciplinary and international program for graduate students who want to earn a PhD degree. The aim of our doctoral program is to advance our understanding of processes and dynamics in the Earth system as well as predictive capabilities.

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ICON Team Receives International Recognition for Groundbreaking Achievements in High-Performance Computing

A team led by the Max Planck Institute for Meteorology and the German Climate Computing Center has received the prestigious Gordon Bell Prize for Climate Modelling for their groundbreaking work at the intersection of climate science and high-performance computing. Their achievement—a landmark simulation of the full Earth system with the ICON model at 1.25-kilometer resolution—overcame a challenge long considered impossible to master.

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About our institute

We are an internationally renowned institute for climate research. Our mission is to understand Earth's changing climate.

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Nobel Prize in Physics 2021 for Prof. Klaus Hasselmann

The statistical model with which global warming can be attributed to increasing concentrations of CO2 in the atmosphere was developed by Klaus Hasselmann, former director of the Max Planck Institute for Meteorology. He received the Nobel Prize in Physics for his work.

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Our institute as an attractive employer

Our research requires us to seek out the most talented, creative and passionate individuals. This compels us to draw from the greatest possible pool of talent.

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Seminars

Joint Seminar: Aerosol–Ice–Cloud Interactions: A Justified Afterthought

Efforts to constrain estimates of the effective radiative forcing (ERF) from aerosol–cloud interactions (ERFaci) have primarily focused on aerosol effects on liquid clouds. In contrast, the impact of aerosol effects on ice clouds is much less understood. Using a perturbed parameter ensemble (PPE) of CAM6 simulations, we investigate the response of ice clouds to anthropogenic aerosols and its sensitivity to key aerosol and microphysics parameters. We quantify the radiative impacts of changes in ice crystal size, ice water path, and ice cloud fraction using a new cloud radiative kernel framework. A pathway is proposed that relates aerosol-induced subtropical low cloud changes to tropical ice cloud changes via changes in boundary layer moisture. The PPE results demonstrate that dynamical changes can drive the SW aerosol forcing on ice clouds in certain regions, adding another dimension of complexity to aerosol–cloud interactions. Hence the simplistic picture of weak aerosol impacts on ice clouds is revealed to obscure substantial variability in aerosol–ice–cloud interactions, with potential implications for efforts to constrain ERFaci. 


Date

03.11.2026

Time

15:15

- 16:40

Event Place

Bundesstr. 53, room 022/023

Seminar Room 022/023 Ground Floor Bundesstrasse 53 20146 Hamburg, Hamburg

Speakers

Brandon Duran

Chair

Clara Bayley

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