Combined Climate Extreme Index

Overview

The goal of this diagnostic is to compute time series of a number of extreme events: heatwave, coldwave, heavy precipitation, drought and high wind. Then, the user can combine these different components (with or without weights). The result is an index similar to the Climate Extremes Index (CEI; Karl et al., 1996), the modified CEI (mCEI; Gleason et al., 2008) or the Actuaries Climate Index (ACI; American Academy of Actuaries, 2018). The output consists of a netcdf file containing the area-weighted and multi-model multi-metric index. This recipe can be applied to data with any temporal resolution, and the running average is computed based on the user-defined window length (e.g. a window length of 5 would compute the 5-day running mean when applied to data, or 5-month running mean when applied to monthly data).

In recipe_extreme_index.yml, after defining the area and reference and projection period, the weigths for each metric selected. The options are

  • weight_t90p the weight of the number of days when the maximum temperature exceeds the 90th percentile,

  • weight_t10p the weight of the number of days when the minimum temperature falls below the 10th percentile,

  • weight_Wx the weight of the number of days when wind power (third power of wind speed) exceeds the 90th percentile,

  • weight_cdd the weight of the maximum length of a dry spell, defined as the maximum number of consecutive days when the daily precipitation is lower than 1 mm, and

  • weight_rx5day the weight of the maximum precipitation accumulated during 5 consecutive days.

Available recipes and diagnostics

Recipes are stored in recipes/

  • recipe_extreme_index.yml

Diagnostics are stored in diag_scripts/magic_bsc/

  • extreme_index.R

User settings

User setting files are stored in recipes/

  1. recipe_extreme_index.yml

    Required settings for script

    • weight_t90p: 0.2 (from 0 to 1, the total sum of the weight should be 1)

    • weight_t10p: 0.2 (from 0 to 1, the total sum of the weight should be 1)

    • weight_Wx: 0.2 (from 0 to 1, the total sum of the weight should be 1)

    • weight_rx5day: 0.2 (from 0 to 1, the total sum of the weight should be 1)

    • weight_cdd: 0.2 (from 0 to 1, the total sum of the weight should be 1)

    • running_mean: 5 (depends on the length of the future projection period selected, but recommended not greater than 11)

Variables

  • tasmax (atmos, daily, longitude, latitude, time)

  • tasmin (atmos, daily, longitude, latitude, time)

  • sfcWind (atmos, daily, longitude, latitude, time)

  • pr (atmos, daily, longitude, latitude, time)

Observations and reformat scripts

None

References

  • Alexander L.V. and Coauthors (2006). Global observed changes in daily climate extremes of temperature and precipitation. J. Geophys. Res., 111, D05109. https://doi.org/10.1029/2005JD006290

  • American Academy of Actuaries, Canadian Institute of Actuaries, Casualty Actuarial Society and Society of Actuaries. Actuaries Climate Index. http://actuariesclimateindex.org (2018-10-06).

  • Donat, M., and Coauthors (2013). Updated analyses of temperature and precipitation extreme indices since the beginning of the twentieth century: The HadEX2 dataset. J. Geophys. Res., 118, 2098–2118, https://doi.org/10.1002/jgrd.50150.

  • Fouillet, A., Rey, G., Laurent, F., Pavillon, G. Bellec, S., Guihenneuc-Jouyaux, C., Clavel J., Jougla, E. and Hémon, D. (2006) Excess mortality related to the August 2003 heat wave in France. Int. Arch. Occup. Environ. Health, 80, 16–24. https://doi.org/10.1007/s00420-006-0089-4

  • Gleason, K.L., J.H. Lawrimore, D.H. Levinson, T.R. Karl, and D.J. Karoly (2008). A Revised U.S. Climate Extremes Index. J. Climate, 21, 2124-2137 https://doi.org/10.1175/2007JCLI1883.1

  • Meehl, G. A., and Coauthors (2000). An introduction to trends inextreme weather and climate events: Observations, socio-economic impacts, terrestrial ecological impacts, and model projections. Bull. Amer. Meteor. Soc., 81, 413–416. doi: 10.1175/1520-0477(2000)081<0413:AITTIE>2.3.CO;2

  • Whitman, S., G. Good, E. R. Donoghue, N. Benbow, W. Y. Shou and S. X. Mou (1997). Mortality in Chicago attributed to the July 1995 heat wave. Amer. J. Public Health, 87, 1515–1518. https://doi.org/10.2105/AJPH.87.9.1515

  • Zhang, Y., M. Nitschke, and P. Bi (2013). Risk factors for direct heat-related hospitalization during the 2009 Adelaide heat-wave: A case crossover study. Sci. Total Environ., 442, 1–5. https://doi.org/10.1016/j.scitotenv.2012.10.042

  • Zhang, X. , Alexander, L. , Hegerl, G. C., Jones, P. , Tank, A. K., Peterson, T. C., Trewin, B. and Zwiers, F. W. (2011). Indices for monitoring changes in extremes based on daily temperature and precipitation data. WIREs Clim Change, 2: 851-870. doi:10.1002/wcc.147. https://doi.org/10.1002/wcc.147

Example plots

../_images/t90p_IPSL-CM5A-LR_rcp85_2020_2040.png

Average change in the heat component (t90p metric) of the Combined Climate Extreme Index for the 2020-2040 compared to the 1971-2000 reference period for the RCP 8.5 scenario simulated by MPI-ESM-MR.