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Detection of atmospheric rivers with inline uncertainty quantification: TECA-BARD v1.0.1

  • Travis A. O'Brien
  • , Mark D. Risser
  • , Burlen Loring
  • , Abdelrahman A. Elbashandy
  • , Harinarayan Krishnan
  • , Jeffrey S. Johnson
  • , Christina M. Patricola
  • , John P. O'Brien
  • , Ankur Mahesh
  • , Prabhat
  • , Sarahi Arriaga Ramirez
  • , Alan M. Rhoades
  • , Alexander Charn
  • , Hector Inda Diaz
  • , William D. Collins

Research output: Contribution to journalArticlepeer-review

33 Citations (Scopus)

Abstract

It has become increasingly common for researchers to utilize methods that identify weather features in climate models. There is an increasing recognition that the uncertainty associated with choice of detection method may affect our scientific understanding. For example, results from the Atmospheric River Tracking Method Intercomparison Project (ARTMIP) indicate that there are a broad range of plausible atmospheric river (AR) detectors and that scientific results can depend on the algorithm used. There are similar examples from the literature on extratropical cyclones and tropical cyclones. It is therefore imperative to develop detection techniques that explicitly quantify the uncertainty associated with the detection of events.We seek to answer the following question: given a"plausible"AR detector, how does uncertainty in the detector quantitatively impact scientific results? We develop a large dataset of global AR counts, manually identified by a set of eight researchers with expertise in atmospheric science, which we use to constrain parameters in a novel AR detection method. We use a Bayesian framework to sample from the set of AR detector parameters that yield AR counts similar to the expert database of AR counts; this yields a set of "plausible"AR detectors from which we can assess quantitative uncertainty. This probabilistic AR detec It has become increasingly common for researchers to utilize methods that identify weather features in climate models. There is an increasing recognition that the uncertainty associated with choice of detection method may affect our scientific understanding. For example, results from the Atmospheric River Tracking Method Intercomparison Project (ARTMIP) indicate that there are a broad range of plausible atmospheric river (AR) detectors and that scientific results can depend on the algorithm used. There aresimilar examples from the literature on extratropical cyclones and tropical cyclones. It is therefore imperative to develop detection techniques that explicitly quantify the uncertainty associated with the detection of events.We seek to answer the following question: given a "plausible"AR detector, how does uncertainty in the detector quantitatively impact scientific results? We develop a large dataset of global AR counts, manually identified by a set of eight researchers with expertise inatmospheric science, which we use to constrain parameters in a novel AR detection method. We use a Bayesian framework to sample from the set of AR detector parameters that yield AR counts similar tothe expert database of AR counts; this yields a set of "plausible"AR detectors from which we can assess quantitative uncertainty. This probabilistic AR detector has been implemented in the Toolkit for Extreme Climate Analysis (TECA), which allows for efficient processing of petabyte-scale datasets. We apply the TECA Bayesian AR Detector, TECA-BARD v1.0.1, to the MERRA-2 reanalysis and showthat the sign of the correlation between global AR count and El Ni o-Southern Oscillation depends on the set of parameters used.

Original languageEnglish
Pages (from-to)6131-6148
Number of pages18
JournalGeoscientific Model Development
Volume13
Issue number12
DOIs
Publication statusPublished - 3 Dec 2020

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action

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