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Reproducing ENSO CLIVAR metrics - background climatology

ENSO CLIVAR metrics by Yann Planton, background climatology for REF

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Diagnostic_Metrics

run preprocessors on variables for background climatology metrics

Diagnostic Metrics: Plot Script

Zonal bias in the time-mean precipitation structure across the equatorial Pacific (averaged between 5°S-5°N), illustrating the increased precipitation in the eastern Pacific and decreased precipitation in the western Pacific.
Zonal bias in the time-mean precipitation structure across the equatorial Pacific (averaged between 5°S-5°N), illustrating the increased precipitation in the eastern Pacific and decreased precipitation in the western Pacific.

download | references | extra data citation | provenance
Zonal bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific (averaged between 5°S-5°N).
Zonal bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific (averaged between 5°S-5°N).

download | references | extra data citation | provenance
Zonal bias in the sea surface temperature structure across the equatorial Pacific (averaged between 5°S-5°N), primarily illustrating the cold tongue bias (typically warmer near South America and cooler further west).
Zonal bias in the sea surface temperature structure across the equatorial Pacific (averaged between 5°S-5°N), primarily illustrating the cold tongue bias (typically warmer near South America and cooler further west).

download | references | extra data citation | provenance
Zonal bias in the amplitude of the mean seasonal cycle of sea surface temperature in the equatorial Pacific (averaged between 5°S-5°N).
Zonal bias in the amplitude of the mean seasonal cycle of sea surface temperature in the equatorial Pacific (averaged between 5°S-5°N).

download | references | extra data citation | provenance
Zonal bias in the structure of zonal wind stress across the equatorial Pacific (averaged between 5°S-5°N), primarily highlighting the trade winds bias (typically weaker circulation in the central Pacific and stronger in the western Pacific).
Zonal bias in the structure of zonal wind stress across the equatorial Pacific (averaged between 5°S-5°N), primarily highlighting the trade winds bias (typically weaker circulation in the central Pacific and stronger in the western Pacific).

download | references | extra data citation | provenance
Zonal bias in the amplitude of the mean seasonal cycle of zonal wind stress in the equatorial Pacific (averaged between 5°S-5°N).
Zonal bias in the amplitude of the mean seasonal cycle of zonal wind stress in the equatorial Pacific (averaged between 5°S-5°N).

download | references | extra data citation | provenance
Meridional bias in the time-mean precipitation structure across the eastern Pacific (averaged between 150-90°W), primarily illustrating the double intertropical convergence zone (ITCZ) bias.
Meridional bias in the time-mean precipitation structure across the eastern Pacific (averaged between 150-90°W), primarily illustrating the double intertropical convergence zone (ITCZ) bias.

download | references | extra data citation | provenance
Meridional bias in the amplitude of the mean seasonal precipitation cycle in the eastern Pacific (averaged between 150-90°W).
Meridional bias in the amplitude of the mean seasonal precipitation cycle in the eastern Pacific (averaged between 150-90°W).

download | references | extra data citation | provenance

Data files

  • Zonal bias in the time-mean precipitation structure across the equatorial Pacific (averaged between 5°S-5°N), illustrating the increased precipitation in the eastern Pacific and decreased precipitation in the western Pacific. | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance
  • Zonal bias in the sea surface temperature structure across the equatorial Pacific (averaged between 5°S-5°N), primarily illustrating the cold tongue bias (typically warmer near South America and cooler further west). | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of sea surface temperature in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance
  • Zonal bias in the structure of zonal wind stress across the equatorial Pacific (averaged between 5°S-5°N), primarily highlighting the trade winds bias (typically weaker circulation in the central Pacific and stronger in the western Pacific). | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of zonal wind stress in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance
  • Meridional bias in the time-mean precipitation structure across the eastern Pacific (averaged between 150-90°W), primarily illustrating the double intertropical convergence zone (ITCZ) bias. | download | references | extra data citation | provenance
  • Meridional bias in the amplitude of the mean seasonal precipitation cycle in the eastern Pacific (averaged between 150-90°W). | download | references | extra data citation | provenance
  • Zonal bias in the time-mean precipitation structure across the equatorial Pacific (averaged between 5°S-5°N), illustrating the increased precipitation in the eastern Pacific and decreased precipitation in the western Pacific. | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance
  • Meridional bias in the time-mean precipitation structure across the eastern Pacific (averaged between 150-90°W), primarily illustrating the double intertropical convergence zone (ITCZ) bias. | download | references | extra data citation | provenance
  • Meridional bias in the amplitude of the mean seasonal precipitation cycle in the eastern Pacific (averaged between 150-90°W). | download | references | extra data citation | provenance
  • Zonal bias in the sea surface temperature structure across the equatorial Pacific (averaged between 5°S-5°N), primarily illustrating the cold tongue bias (typically warmer near South America and cooler further west). | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of sea surface temperature in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance
  • Zonal bias in the structure of zonal wind stress across the equatorial Pacific (averaged between 5°S-5°N), primarily highlighting the trade winds bias (typically weaker circulation in the central Pacific and stronger in the western Pacific). | download | references | extra data citation | provenance
  • Zonal bias in the amplitude of the mean seasonal cycle of zonal wind stress in the equatorial Pacific (averaged between 5°S-5°N). | download | references | extra data citation | provenance

Diagnostic_Level2

run preprocessors on variables for background climatology diagnostic level 2

Diagnostic Level2: Plot Script

Time-mean precipitation bias in the equatorial Pacific, primarily highlighting the double intertropical convergence zone (ITCZ) bias.
Time-mean precipitation bias in the equatorial Pacific, primarily highlighting the double intertropical convergence zone (ITCZ) bias.

download | references | extra data citation | provenance
Bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific.
Bias in the amplitude of the mean seasonal cycle of precipitation in the equatorial Pacific.

download | references | extra data citation | provenance
Time-mean zonal wind stress bias in the equatorial Pacific.
Time-mean zonal wind stress bias in the equatorial Pacific.

download | references | extra data citation | provenance
Time-mean sea surface temperature bias in the equatorial Pacific.
Time-mean sea surface temperature bias in the equatorial Pacific.

download | references | extra data citation | provenance

Files

main_log.txt | main_log_debug.txt | recipe.yml | figures | data