EuLerian Identification of Ascending air Streams (ELIAS 2.0) in Numerical Weather Prediction and Climate Models. Part II: Model application to different data sets

Abstract. Warm conveyor belts (WCBs) affect the atmospheric dynamics in midlatitudes and are highly relevant for total and extreme precipitation in many parts of the extratropics. Thus, these air streams and their effect on midlatitude weather should be well represented in numerical weather prediction (NWP) and climate models. This study applies newly developed convolutional neural network (CNN) models which allow the identification of footprints of WCB inflow, ascent, and outflow from a limited number of predictor fields at comparably low spatio-temporal resolution. The goal of the study is to demonstrate the versatile applicability of the CNN models to different data sets and that their application yields qualitatively and quantitatively similar results as their trajectory-based counterpart which is most frequently used to objectively identify WCBs but requires data at higher spatio-temporal resolution which is often not available and is computationally more expensive. First, an application to reanalyses reveals that the well-known relationship between WCB ascent and extratropical cyclones as well as between WCB outflow and blocking anticyclones is also found for WCB footprints identified with the CNN models. Second, the application to Japanese 55-year reanalyses shows how the CNN models may be used to identify erroneous predictor fields that deteriorate the models' reliability. Third, a verification of WCBs in operational European Centre for Medium-Range Weather Forecasts (ECMWF) ensemble forecasts for three Northern Hemisphere winters reveals systematic biases over the North Atlantic with both the trajectory-based approach and the CNN models. The ensemble forecasts' skill tends to be lower when being evaluated with the trajectory approach due to the fine-scale structure of WCB footprints in comparison to the rather smooth CNN-based WCB footprints. A final example demonstrates the applicability of the CNN models to a convection permitting simulation with the ICOsahedral Nonhydrostatic (ICON) NWP model. Our study illustrates that deep learning methods can be used efficiently to support process-oriented understanding of forecast error and model biases, and opens numerous directions for future research.

[1]  S. Rasp,et al.  Convective and Slantwise Trajectory Ascent in Convection-Permitting Simulations of Midlatitude Cyclones , 2016 .

[2]  C. Schwierz,et al.  A Multifaceted Climatology of Atmospheric Blocking and Its Recent Linear Trend , 2007 .

[3]  Heini Wernli,et al.  Warm Conveyor Belts in the ERA-Interim Dataset (1979–2010): Part I: Climatology and Potential Vorticity Evolution , 2014 .

[4]  Robert S. Plant,et al.  The dichotomous structure of the warm conveyor belt , 2014 .

[5]  B. Hoskins,et al.  On the use and significance of isentropic potential vorticity maps , 2007 .

[6]  K. Browning Conceptual Models of Precipitation Systems , 1986 .

[7]  H. Wernli,et al.  Convective activity in an extratropical cyclone and its warm conveyor belt – a case‐study combining observations and a convection‐permitting model simulation , 2019, Quarterly Journal of the Royal Meteorological Society.

[8]  T. W. Harrold Mechanisms influencing the distribution of precipitation within baroclinic disturbances , 1973 .

[9]  C. Grams,et al.  Toward a systematic evaluation of warm conveyor belts in numerical weather prediction and climate models. Part II: Verification of operational reforecasts , 2021, Journal of the Atmospheric Sciences.

[10]  Alan J. Thorpe,et al.  The Evolution and Dynamical Role of Reduced Upper-Tropospheric Potential Vorticity in Intensive Observing Period One of FASTEX , 2000 .

[11]  Toby N. Carlson,et al.  Airflow Through Midlatitude Cyclones and the Comma Cloud Pattern , 1980 .

[12]  C. Grams,et al.  Toward a Systematic Evaluation of Warm Conveyor Belts in Numerical Weather Prediction and Climate Models. Part I: Predictor Selection and Logistic Regression Model , 2021, Journal of the Atmospheric Sciences.

[13]  Thomas Brox,et al.  U-Net: Convolutional Networks for Biomedical Image Segmentation , 2015, MICCAI.

[14]  Ulrich Corsmeier,et al.  The key role of diabatic processes in modifying the upper‐tropospheric wave guide: a North Atlantic case‐study , 2011 .

[15]  C. Grams,et al.  EuLerian Identification of ascending Air Streams (ELIAS 2.0) in Numerical Weather Prediction and Climate Models. Part I: Development of deep learning model , 2021 .

[16]  S. Pfahl,et al.  The role of latent heating in atmospheric blocking dynamics: a global climatology , 2019, Climate Dynamics.

[17]  M. Shapiro,et al.  The Life Cycle of an Extratropical Marine Cyclone. Part I: Frontal-Cyclone Evolution and Thermodynamic Air-Sea Interaction , 1993 .

[18]  Heini Wernli,et al.  A 15-Year Climatology of Warm Conveyor Belts , 2004 .

[19]  H. Joos Warm Conveyor Belts and Their Role for Cloud Radiative Forcing in the Extratropical Storm Tracks , 2019, Journal of Climate.

[20]  K. D. Beheng,et al.  A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 1: Model description , 2006 .

[21]  Heini Wernli,et al.  The Role of Warm Conveyor Belts for the Intensification of Extratropical Cyclones in Northern Hemisphere Winter , 2016 .

[22]  Heini Wernli,et al.  A Lagrangian‐based analysis of extratropical cyclones. I: The method and some applications , 1997 .

[23]  M. Stoelinga A Potential Vorticity-Based Study of the Role of Diabatic Heating and Friction in a Numerically Simulated Baroclinic Cyclone , 1996 .

[24]  Martin Wirth,et al.  The North Atlantic Waveguide and Downstream Impact Experiment , 2018, Bulletin of the American Meteorological Society.

[25]  C. Schwierz,et al.  Surface Cyclones in the ERA-40 Dataset (1958–2001). Part I: Novel Identification Method and Global Climatology , 2006 .

[26]  H. Wernli,et al.  Growth and Decay of an Extra-Tropical Cyclone’s PV-Tower , 2000 .

[27]  G. Zängl,et al.  The ICON (ICOsahedral Non‐hydrostatic) modelling framework of DWD and MPI‐M: Description of the non‐hydrostatic dynamical core , 2015 .

[28]  John Methven,et al.  Potential vorticity in warm conveyor belt outflow , 2015 .

[29]  Harald Sodemann,et al.  Planning aircraft measurements within a warm conveyor belt , 2014 .

[30]  Veronika Eyring,et al.  Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization , 2015 .

[31]  Heini Wernli,et al.  The LAGRANTO Lagrangian analysis tool – version 2.0 , 2015 .

[32]  Yayoi Harada,et al.  The JRA-55 Reanalysis: Representation of Atmospheric Circulation and Climate Variability , 2016 .

[33]  O. Martius,et al.  Northern Hemisphere Rossby Wave Initiation Events on the Extratropical Jet—A Climatological Analysis , 2018 .

[34]  C. Kobayashi,et al.  The JRA-55 Reanalysis: General Specifications and Basic Characteristics , 2015 .

[35]  H. Wernli,et al.  Potential vorticity structure of embedded convection in a warm conveyor belt and its relevance for the large-scale dynamics , 2019 .

[36]  Michel Rixen,et al.  The Subseasonal to Seasonal (S2S) Prediction Project Database , 2017 .

[37]  Florian Pappenberger,et al.  The TIGGE Project and Its Achievements , 2016 .

[38]  M. Tiedtke A Comprehensive Mass Flux Scheme for Cumulus Parameterization in Large-Scale Models , 1989 .

[39]  Michael Sprenger,et al.  Global Climatologies of Eulerian and Lagrangian Flow Features based on ERA-Interim , 2017 .

[40]  Heini Wernli,et al.  Warm Conveyor Belts in the ERA-Interim Dataset (1979–2010). Part II: Moisture Origin and Relevance for Precipitation , 2014 .