Talks and presentations

Physics-Constrained Adaptive Flow Matching for Climate Downscaling

June 16, 2026

Oral presentation, CESM Workshop 2026, Boulder, CO

Regional climate information at kilometer scales is essential for assessing the impacts of climate change, but generating it with global climate models is too expensive due to their high computational costs. Machine learning models offer a fast alternative, yet they often violate basic physical laws and degrade when applied to climates outside of their training distribution. We present Physics-Constrained Adaptive Flow Matching (PC-AFM), a generative downscaling model that addresses both problems. Building on the Adaptive Flow Matching (AFM) model of Fotiadis et al. (2025) as our baseline, we add soft conservation constraints that keep the downscaled output consistent with the large-scale input for precipitation and humidity, and use gradient surgery via the ConFIG algorithm to prevent these constraints from interfering with the generative objective. We train the model on Central Europe climate data, evaluate it on a 10-time downscaling task (63km to 6.3km) over six variables (near-surface temperature, precipitation, specific humidity, surface pressure, and horizontal wind components) across a comprehensive set of metrics including bias, ensemble skill scores, power spectra, and conservation error, and test the generalization on two held-out climate regions. Within the training distribution, PC-AFM reduces conservation errors and improves ensemble calibration while matching the baseline on standard skill metrics. Outside the training distribution, where unconstrained models develop large systematic errors by extrapolating learned statistics, PC-AFM halves precipitation wet bias, reduces conservation error and improves extreme-quantile accuracy, all without any information about the target climate at inference time. These results indicate that physical consistency is a practical requirement for deploying generative downscaling models in real-world applications.

Understanding European Heatwaves with Variational Autoencoders

March 11, 2026

Virtual poster presentation, CMIP Community Workshop 2026, Kyoto, Japan

Understanding the dynamics of heatwaves is critical for accurate climate risk assessment. Traditional definitions, based solely on surface temperature thresholds, often overlook the complex, multivariate nature of heatwaves. In this study, we use a spatiotemporal Variational Autoencoder (VAE), an unsupervised machine learning method, to identify compact representations of year-round multivariate heatwave patterns. We extract eleven-day multivariate (e.g., circulation, humidity, temperature, geopotential height, cloud cover, stream function, and radiation) heatwave samples from ERA5 reanalysis data over the North Atlantic, based on near-surface temperature extremes in Western Europe. The VAE model is trained on heatwave samples from 1941–1990 and evaluated using 2001–2022 samples. The VAE model effectively clusters heatwave events by season, and composite maps reveal the interplay and temporal evolution between different atmospheric variables in their contributions to heatwaves over Western Europe, such as summer blocking highs and winter omega blocks. Notably, recent summer heatwaves form a distinct cluster within the latent space, pointing to a shift in atmospheric dynamics consistent with climate change. This approach offers a powerful framework to explore the spatiotemporal evolution of multivariate extremes. As a next step, we plan to apply the VAE model to CMIP simulations to evaluate how well climate models reproduce observed heatwave patterns and their associated atmospheric dynamics. This can provide a promising diagnostic to assess model skill and improve projections of heatwaves under climate change.

Detecting Extreme Temperature Events Using Gaussian Mixture Models

April 24, 2023

Oral presentation, EGU General Assembly 2023, Vienna, Austria

Extreme events are rare atmospheric phenomena that cause significant damage to humans and natural systems, but detecting extreme events in the future in a changing climate can be challenging. Traditionally, temperature distributions were assumed to follow a normal distribution and certain thresholds were used to define extreme events. However, the mean and the variance of temperatures are expected to change in a future climate, which might limit the application of traditional methods for detecting extreme events.

Determination of Exposures of Mediterranean Touristic Resources by Using Regional Climate Modeling

April 10, 2019

Poster presentation, EGU General Assembly 2019, Vienna, Austria

Summer tourism in the Mediterranean Basin is one of the most important contributors to the countries’ GDPs, and is highly dependent on the climatic conditions. In this study, it is aimed to determine the exposures of the most visited touristic resources in the Mediterranean Basin via Tourism Climate Index [1] which is an ideal indicator of tourism exposure to the hazard of changes to the mean climate [2]. For this purpose, the outputs of the MPI-ESM-MR global climate model of the Max Planck Institute for Meteorology are downscaled to 50km by the use of Regional Climate Model (RegCM4. 4) of the Abdus Salam International Centre for Theoretical Physics (ICTP). To make future projections for the period of 2021-2050 and 2070-2099 with respect to the reference period of 1971-2000, RCP 4.5 and RCP 8.5 scenarios are used. Tourism Climate Index (TCI) for projected periods are computed by using the 30-year monthly mean temperature, relative humidity, precipitation, wind and sunshine outputs of the RegCM4. 4. Thereafter, the TCI values are plotted to see the changes throughout the months.