Abstract

This study introduces a detailed and objective classification for midlatitude maritime fronts. The classification is based on a principal component analysis (PCA) to determine the dominant patterns of variability between fronts. Here, fronts are defined as three‐dimensional frontal volumes, which are detected in the ERA‐Interim dataset for a large number of locations in the Atlantic, Pacific and Indian oceans during both winter and summer. In addition to the well‐established distinction between warm and cold fronts, the PCA exposes several new dimensions of variability: (i) front intensity, (ii) surface fluxes and (iii) along‐front transports, linked to the intensity of the associated conveyor belts. These new dimensions of variability are regionally and seasonally robust and a lagged composite analysis demonstrates that each of the new front types evolves in a dynamically characteristic way. Further, the new front types can be related to established ones like katafronts and anafronts. The new front types are finally redefined based on simple parameter thresholds to simplify their application in future studies.

Highlights

  • Fronts are one of the essential building blocks of extratropical cyclones and midlatitude atmospheric dynamics (Shapiro and Keyser, 1990; Bjerknes, 1919)

  • Journal of the Royal Meteorological Society published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society

  • We focus on the orange circles that make up rotated principal components (RPCs) 2 in the example region, because this variability pattern can serve as a proof-of-concept for our analysis method

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Summary

Introduction

Fronts are one of the essential building blocks of extratropical cyclones and midlatitude atmospheric dynamics (Shapiro and Keyser, 1990; Bjerknes, 1919). They go along with temperature changes, precipitation and winds that shape the public perception of weather in these regions. The conceptual models of Bjerknes (1919) and Shapiro and Keyser (1990) distinguish between warm and cold fronts, occlusions and bent-back fronts Each of these front types is associated with a characteristic sequence of surface weather and plays a well-defined role in the conceptual life cycle of an extratropical cyclone. We aim for a classification that is not limited to a specific location, storm track or season and adopt a climatological perspective based on reanalysis data

Front detection and classification
Our front-detection method
Regional front volumes
Front-type classification method
Patterns of front variability from recurring PCs
Simplified redefinition the variability patterns
Relation to alternative front-type definitions
Findings
Summary and conclusions
Full Text
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