Agnostic detection of large-scale weather patterns in the northern hemisphere: from blockings to teleconnections

TL;DR

This paper introduces an unsupervised method inspired by Markov State Modelling to detect and analyze dominant large-scale weather patterns and teleconnections in the Northern Hemisphere's mid-latitudes, revealing complex dynamical regimes.

Contribution

The authors adapt a spectral analysis approach to identify slow modes of atmospheric variability without predefined states, providing a dynamical foundation for weather regimes and teleconnections.

Findings

Identified dominant weather regimes in Atlantic and Pacific sectors.

Discovered a dynamical regime linked to Atlantic-Pacific blocking.

Revealed that atmospheric variability lacks clear-cut modes due to overlapping time scales.

Abstract

Detecting recurrent weather patterns and understanding the transitions between such regimes are key to advancing our knowledge on the low-frequency variability of the atmosphere and have important implications in terms of weather and climate-related risks. We adapt an analysis pipeline inspired by Markov State Modelling and detect in an unsupervised manner the dominant winter mid-latitude Northern Hemisphere weather patterns in the Atlantic and Pacific sectors. The daily 500 hPa geopotential height fields are first classified in $\sim 200$ microstates. The weather dynamics is then represented in the basis of these microstates and the slowest decaying modes are identified from the spectral properties of the transition probability matrix. These modes are defined on the basis of the nonlinear dynamical processes of the system and not as tentative metastable states as often done in Markov state analysis. In the Atlantic and Pacific sectors slow relaxation processes are mainly related to transitions between blocked regimes and zonal flow. We also find strong evidence of a dynamical regime associated with the simultaneous Atlantic-Pacific blocking. When the analysis is performed in a broader geographical region of the Atlantic sector, we discover that the slowest relaxation modes of the system are associated with transitions between dynamical regimes that resemble teleconnection patterns like the North Atlantic Oscillation and weather regimes like the Scandinavian and Greenland blocking, yet have a much stronger dynamical foundation than classical methods based e.g. on EOF analysis. Our method clarifies that, as a result of the lack of a time-scale separation in the atmospheric variability of the mid-latitudes, there is no clear-cut way to represent the atmospheric dynamics in terms of few, well-defined modes of variability.