With each new IFS cycle ECMWF updates, via a recalibration exercise, the decision trees used for its ecPoint post-processing (see Figure 1 below). This is particularly important when there are model physics changes that affect rainfall characteristics. In cycle 50r1 fundamental changes were made to the convection scheme. Practically, these brought benefits for users in raw model output: notably more propagation inland of rainfall associated with (SST-triggered) marine convection, and more propagation downstream of convection triggered by upslopes. So rainfall patterns in forecasts have changed. Not only that, but to achieve these structural improvements a proportion (ordinarily 40%) of the snow and rain particulates in the model column are now commuted across from the convection scheme into the large scale scheme. This implies that the meaning of "convective precipitation" in model output has changed. And in turn the convective precipitation ratio (CPR = (convective precipitation accumulation in a period) / (total precipitation accumulation in that period) ), which has been a key variable used by ecPoint, now has different characteristics. Occurrence, worldwide, of high values of CPR is much lower in 50r1 than it was 49r1, whilst intermediate values are more common.

Figure 1: Schematic of an ecPoint post-processing decision tree. Based on what classes (for a given gridbox, member and time interval), different governing variable values fall into (the branches at each level in the hierarchy) we apply a mapping function (1-D matrix) of multiplication factors to the raw model rainfall forecast, to deliver equiprobable forecast values of rainfall for the said period, as would be measured by a raingauge randomly situated within the said gridbox.
This all necessitated a re-think and a restructuring of the ecPoint decision trees, as shown on the 2 tables below. Alongside these decision tree changes, we have now started archiving the output in ECMWF's MARS archive (under the heading "weather-type-subgrid-calibration"). At the same time the ecPoint outputs have been expanded, to encompass 6h, 12h and 24h periods, when previously only 12h periods had been available. The ecPoint products retain their "EXPERIMENTAL" status.
| 12h Period: Hierarchy used (most "significant" at the top) | |
|---|---|
| 1 | Convective Precipitation Ratio (CPR) for the period |
| 2 | Total Precipitation forecast for the period (TP) |
| 3 | Weighted time-average mean of the 700mb Wind Speed for the period |
| 4 | Maximum MUCAPE during the period |
| 5 | Clear-sky Direct Solar Radiation (24h total for the location in question) |
| 6h Period: Hierarchy used (most "significant" at the top) | | 12h Period: Hierarchy used (most "significant" at the top) | 24h Period: Hierarchy used (most "significant" at the top) | ||||
|---|---|---|---|---|---|---|---|
| 1 | Convective Precipitation Ratio (CPR) for the period | 1 | Convective Precipitation Ratio (CPR) for the period | 1 | Convective Precipitation Ratio (CPR) for the period | ||
| 2 | Total Precipitation forecast for the period (TP) | 2 | Total Precipitation forecast for the period (TP) | 2 | Total Precipitation forecast for the period (TP) | ||
| 3 | Maximum MUCAPE during the period | 3 | Maximum MUCAPE during the period | 3 | Maximum MUCAPE during the period | ||
| 4 | Weighted time-average of the 2m dewpoint depression (DPD) for the period | 4 | Weighted time-average of the 2m dewpoint depression (DPD) for the period | 4 | Weighted time-average of the 2m dewpoint depression (DPD) for the period | ||
| 5 | Local solar time at the mid-point of the period (LST) | 5 | Weighted time-average of the 700mb Wind Speed for the period | 5 | Weighted time-average of the 700mb Wind Speed for the period | ||
| 6 | Weighted time-average of the 700mb Wind Speed for the period | 6 | Clear-sky Direct Solar Radiation (24h total for the location in question) | 6 | Clear-sky Direct Solar Radiation (24h total for the location in question) | ||
| 7 | Clear-sky Direct Solar Radiation (24h total for the location in question) | ||||||
MARS keywords:
Point values (Perturbed members + Control combined): type: "pfc", param: "228", levtype: "sfc", quantile: "n:100" (where n=1,2,..,99), stream: "enfo"
Bias-corrected gridbox (Perturbed members): type: "gbf", param: "228", levtype: "sfc", stream: "enfo", number: m (where m=1,2,..,50)
Gridbox weather Type (Perturbed members): type: "gwt", param: "228", levtype: "sfc", stream: "enfo", number: m (where m=1,2,..,50)
Bias-corrected gridbox (Control): type: "gbf", param: "228", levtype: "sfc", stream: "oper"
Gridbox weather Type (Control): type: "gwt", param: "228", levtype: "sfc", stream: "oper"
In each case, the method of specifying the step dictates whether the requirement is for a 6-hourly or a 12-hourly or a 24-hourly product, as shown in the following examples:
step: "18-24" (6-hourly, ending T+24); step: "90-102" (12-hourly, ending T+102); step "48-72" (24-hourly, ending T+72)
Rationale behind new decision tree structures:
Development of the new decision tree structures was based on extensive tests, examining also other variables; only a short overview is given here.
To maintain some backwards compatibility, and also recognising that CPR is still a pivotal governing variable for post-processing, we have kept CPR at the top of the hierarchy for all 3 period lengths (6,12,24h), but at the same time have elevated the importance of the "Max MUCAPE" variable, in each case, to hierarchy level 3, from level 4 used with 49r1. "Max MUCAPE" is now considered to be complimentary to CPR in defining whether the situation is convective, as well as being a metric of how much convective instability there is. It was just the latter of these that was considered relevant for 49r1.
At level 4 we have introduced the new governing variable of dewpoint depression (DPD); this follows on from investigation of poor (over)forecasting of rain reported by a member state user in 2025 (49r1), other case studies of extreme rainfall (as discussed here for the 2024 Valencia floods), and systematic tests with both 49r1 and 50r1 that highlighted a strong dependance of gridscale bias on this quantity: on average high DPDs correlate with substantial over-forecasting, whilst very small DPDs correlate with under-forecasting. Users may also notice noteworthy improvements over more mountainous areas related to inclusion of this variable.
For the 6-hourly period alone we adopt also a local solar time variable (LST), which aims to help the post-processing address systematic errors in the diurnal cycle of convection. This was previously adopted in the MISTRAL project (see here). It makes no sense to use this with 24h periods, and even with 12h periods it becomes unhelpful.
Tests indicate that gridscale biases have negligible dependance on the total amount of precipitation forecast (TP, level 2 in each hierarchy); however there is, unsurprisingly, a strong dependance of sub-grid variability on this quantity, which markedly affects the forecast point values (type = pfc), and it is for this reason that we retain this at level 2, as with 49r1.
Evidently the decision tree structure rationale is very multifaceted, and one can see how it has been very carefully formulated, and expanded, to match up with the features of new cycle 50r1. We thus expect the 50r1 ecPoint products to deliver even more added value for users, versus the raw model output, than have previous versions.
For reference the original ecPoint paper can be found here.