Closed hannahker closed 3 years ago
Need to validate that these are the most appropriate and up-to-date versions of the CHIRPS and ARC2 dry spells events:
public/exploration/mwi/arc2/mwi_arc2_dry_spells.csv
public/processed/mwi/dry_spells/dry_spells_during_rainy_season_list_2000_2021_mean_back.csv
Both datasets should be:
@Tinkaa could you confirm that I've found the right files?
Yes great job idenitying those in the mess! Trying to open mwi_arc2_dry_spells.csv
gave me a corrupted file error, so I just recomputed it using the notebook and hope it is correct now. You might want to recompute with 2021 data though. also this arc2 file now contains dry spells outside the rainy season as well.
Few thoughts:
And precipitation:
ARC2: public/exploration/mwi/arc2/mwi_arc2_precip_long.csv
CHIRPS: public/processed/mwi/dry_spells/data_long_mean_values_2000_2021.csv
If using ARC2 over CHIRPS for the Malawi observational trigger, we need to make an effort to explain discrepancies between the historical dry spells that are identified by these two data sources. The most obvious difference is that these datasets have differing resolutions (0.05 and 0.1 degrees, respectively), but it's not clear what kind of impact this has.
In addition to a basic literature review, we should explore and compare the daily precipitation values for both datasets during cases where a dry spell is identified by one source but not the other. So for example, if CHIRPS identifies a dry spell between Dec 1-Dec 20 but ARC2 doesn't, what is going on with the precipitation values from ARC2 during this time? This could probably be accomplished by basic visualisation of the daily precipitation time series from both sources during a time period of interest (akin to what we've already done when comparing GloFAS discharge between stations - here).
Any systematic differences revealed as result of this analysis may have to be accounted for in our use of ARC2 for the trigger.