Climate Forecast System (CFS) Preliminary review of 2015 CFS anomaly forecasts of precipitation and severe weather Greg Carbin, NOAA/NWS/SPC
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1 Climate Forecast System (CFS) Preliminary review of 2015 CFS anomaly forecasts of precipitation and severe weather Greg Carbin, NOAA/NWS/SPC
2 Climate Forecast System (CFS) Severe Updates Dashboard now operational on SPC website (uses SPC grib2) Used by forecasters for SPC Day 4-8 forecasts Visualizing Long-range Severe Thunderstorm Environment Guidance from CFSv2, Gregory W. Carbin, Michael K. Tippett, Samuel P. Lillo, Harold E. Brooks (BAMS Online Early Release)
3 Climate Forecast System (CFS) Severe Now operational at
4 Climate Forecast System (CFS) Severe Re-orient your perspective by placing grid count forecasts on parallel diagonals (Day 1 to Day 45 for each 00 UTC CFS run) Day 45 lead Example for initial CFS run on January 1, 2015 As additional forecasts are added along the diagonals, run-to-run consistency in grid count forecasts will appear as vertical stripes with similar color. Y axis is decreasing lead time with Y=0 being valid date X axis = dates in calendar year starting Jan. 1, 2015 Day 7 lead Day 1 Day 7 Day Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
5 Climate Forecast System (CFS) Severe Re-orient your perspective by placing grid count forecasts on parallel diagonals (Day 1 to Day 45 for each 00 UTC CFS run) Day 45 lead After 7 CFS runs, on January 7, grid count forecasts can be verified by total storm reports occurring on Jan. 7, Day 7 lead Day 1 Day 7 Day Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
6 Climate Forecast System (CFS) Severe 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
7 Climate Forecast System (CFS) Severe 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
8 Climate Forecast System (CFS) 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
9 Climate Forecast System (CFS) 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
10 Climate Forecast System (CFS) Severe 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
11 Climate Forecast System (CFS) Severe 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
12 Climate Forecast System (CFS) Severe 2016 Severe Convection and Climate Workshop, Columbia University, NYC March 10, 2016
13 Monthly CFS Precipitation Forecasts with Probability Matched Mean QPF May 2015 Forecast made April 30, 2015 From NWS AHPS analysis
14 Why probability matched mean (PMM)? Ability of a Poor Man's Ensemble to Predict the Probability and Distribution of Precipitation Elizabeth E. Ebert Monthly Weather Review Volume 129, Issue 10 (October 2001) pp The most successful strategy used probability matching (PM) to reassign the rain rates in the ensemble mean using the rain rate distribution of the component QPFs. The PM forecast benefited from the improved rain location given by the ensemble mean, with more realistic rain rates taken directly from the model QPFs.
15 May 2015 Total CONUS Precipitation PMM of 8 CFS members on April 30
16 May 2015 Total CONUS Precipitation Ens Mean of 8 CFS members on April 30
17 Methods Take latest 1- month lead CFS forecasts Use last n CFS runs For 1-month ahead, forecast precipitation is computed by summing valid CFS 6h APCP grids for all available runs on the last day of current month. For example, forecasts for May 2015 use CFS runs initialized April 30, Compute ensemble mean and PMM PMM QPF For ensemble of n- size, entire ensemble distribution is ranked. The ensemble mean values are similarly ranked. Ensemble mean ranked values are replaced with every nth value from total ensemble ranking. Use CFSR and compare areal extent of extremes Observed v. Forecast Using CFSR/CDAS, calculate 37-year climatology of monthly precipitation. Compare areal coverage of extreme wet/dry areas (based on percentile rank) with CFS PMM monthly forecasts.
18 Observed vs. CDAS/CFS, May mm!
19 May 2015 Total CONUS Precipitation Areal coverage of extreme values
20 May 2015 Total CONUS Precipitation CFS PMM forecast of extreme values
21 Despite limited areal extent of extremes in CFS forecast is this still a signal? Can CFS PMM precipitation forecasts of areal extremes accurately represent climatological variability of monthly precipitation and have prognostic value ahead of significant/highly anomalous events?
22 CFS/CDAS CONUS Monthly Precipitation Areal coverage of extreme values Monthly extent of wettest / driest areas in 37 year reanalysis
23 CFS/CDAS CONUS Monthly Precipitation Areal coverage of extreme values Monthly extent of wettest / driest areas in 37 year reanalysis
24 CFS/CDAS CONUS Monthly Precipitation Areal coverage of extreme values Monthly extent of wettest / driest areas in 37 year reanalysis
25 Monthly CONUS Precipitation Areal Coverage (%) Observed Extremes 2014 OBS
26 Monthly CONUS Precipitation Areal Coverage (%) Forecast Extremes 2014 FCST
27 Monthly CONUS Precipitation Observed vs. Forecast Extremes (%Cvg) 2014 OBS FCST OBS FCST
28 Monthly CONUS Precipitation Observed vs. Forecast Extremes (%Cvg) 2015 OBS FCST OBS FCST
29 Monthly CONUS Precipitation Observed vs. Forecast Extremes (%Cvg) 2015 OBS FCST OBS FCST
30 Monthly CONUS Precipitation Observed vs. Forecast Extremes (%Cvg) 2015 OBS FCST? OBS FCST
31 December 2015 CONUS Precipitation Observed vs. Forecast Extremes (%Cvg) Despite missing the highly anomalous heavy December precipitation across the middle of the CONUS, CFS accurately forecast extreme December precipitation over inland southeast, southern Florida, and Pacific Northwest. OBS FCST
32 March 2016 Forecast Extremes (%Cvg) from Feb. 29, 2016 CFS runs (8)
33 CFS Probability Match Mean QPF to Forecast Monthly Precipitation Extremes Using PMM to maintain extreme values within ensemble output shows promise for one month-lead forecasts of extreme precipitation (wet and dry areas in lowest/highest %-tile ranks) based on a review of forecasts. Further refinement of this method could be used to generate shorterterm (two-week) extreme precipitation forecasts. CDAS as analysis may have issues in the warm season across high terrain of the west. Additional ensemble and re-forecast methods should improve extreme precipitation predictability.
34 Thank you!
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