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Forecast Season/Verification & Skill
Route 06 · The uncomfortable half

Verification & Skill

Every forecast on this site is scored against its own reforecast, and each route publishes its own card. This is the page that puts them in one table — and asks the three questions no single route can ask about itself.

06ROUTE

Best scorecard

9 / 10
whole-month scorings taken by C3S multi-system

Systems compared

3 pipelines
one metric, one mask, three implementations

Pooling pays

10/10 vs 6/10
C3S multi-system against NMME

Disagreements settled

50 / 60
to C3S multi-system, on its own reforecast

The matched scorecard

RPSS over land · 1 October 2026

Temperature

TargetleadSEAS551 membersC3S multi-system10 systemsNMME4 models
October 2026part elapsed+0+0.248+0.268+0.256
November 2026+1+0.056+0.094+0.096
December 2026+2+0.042+0.076+0.054
January 2027+3+0.032+0.082+0.059
February 2027+4+0.074+0.117+0.103
March 2027+5+0.064+0.102+0.083

Over the 5 whole months, C3S multi-system scores highest at 4 of 5. The rest are split between NMME (1)

Rainfall

TargetleadSEAS551 membersC3S multi-system10 systemsNMME4 models
October 2026part elapsed+0+0.148+0.154+0.114
November 2026+1+0.004+0.042+0.017
December 2026+2+0.006+0.039+0.020
January 2027+3-0.014+0.029+0.003
February 2027+4-0.007+0.025+0.006
March 2027+5-0.017+0.012-0.008

Over the 5 whole months, C3S multi-system scores highest at 5 of 5. A clean sweep.

Every figure above is the ranked probability skill score of that system’s own reforecast against ERA5, area-weighted over land: SEAS5 (route 10), C3S multi-system (route 03), NMME (route 02). Zero is climatology. Three separately written implementations produced them and they share only the region boxes and the averaging code, so agreement between them is worth something and so is disagreement. A ‡ marks a score below zero — a forecast that verified worse than issuing climatology would have. ⚠ They are not scored over the same years. SEAS5 1993–2016 (24 years); C3S multi-system 1993–2016 (24 years); NMME 1991–2016 (26 years). A comparison down a column is exact; a comparison across one is close but not matched, and the honest weight to put on a gap of a few thousandths across systems is not much. The gaps in the table above are larger than that.

Does pooling pay?

The one exact comparison here

C3S multi-system

10 / 10
scorings where pooling 10 systems beat the best single one — rainfall 5/5

NMME

6 / 10
scorings where pooling 5 models beat the best single one — rainfall 2/5

This is the only question on the page that the difference in reforecast period cannot touch, because neither answer is compared with the other’s numbers: each route scores its own consensus against its own members, in the same pass, from the same reforecast. Both are exact.

And they disagree completely. C3S multi-system pools 10 systems and gains at 10 of 10; NMME pools 5 and gains at only 6. Read together they are not a contradiction but a condition: pooling pays in proportion to how much there is to pool. 10 systems from nine centres carry enough independent error to average away; 5 models that share more of their heritage do not, and their consensus mostly just dilutes whichever one was best.

Neither route can say this on its own page, because neither can see the other’s members. It is the whole reason this route exists.

Which multi-model to believe

60 region-months, whole months only

Routes 03 and 02 both publish a tercile probability for the same six boxes and the same months, and they differ by as much as 12 points. Neither page can say which to believe. But each also publishes, for that same box, the share of it where its own reforecast beat climatology — so the disagreement can be settled with the only evidence either of them offers about itself.

Across all 60 region-months, C3S multi-system has the better reforecast in 50, NMME in 7, with 3 level. That is not close, and it points the same way as both results above it.

RegionfieldmonthP(above) — C3S vs NMMEgapbeats climatology therebetter
AfricaTemperatureFebruary 202775% vs 63%+1291% vs 88%C3S multi-system
EuropeTemperatureDecember 202644% vs 32%+1274% vs 42%C3S multi-system
AfricaTemperatureMarch 202774% vs 64%+1074% vs 79%NMME
AsiaTemperatureNovember 202647% vs 38%+966% vs 53%C3S multi-system
United StatesTemperatureFebruary 202727% vs 36%-990% vs 93%NMME
AfricaTemperatureJanuary 202770% vs 61%+872% vs 67%C3S multi-system
AfricaTemperatureNovember 202658% vs 50%+881% vs 82%NMME
AsiaTemperatureFebruary 202752% vs 44%+883% vs 56%C3S multi-system
The eight widest disagreements. Better is whichever system’s own reforecast beat climatology over more of that box — not which one turned out right, which nobody knows yet.

Where the skill is

by region, at March 2027

Temperature

RegionSEAS5C3S multi-systemNMME
United States46%89%64%
S. America78%88%78%
Oceania77%88%71%
Asia52%85%70%
Africa67%74%79%
Europe47%68%62%

Rainfall

RegionSEAS5C3S multi-systemNMME
Oceania51%78%59%
S. America36%57%39%
United States43%56%45%
Asia28%47%36%
Europe38%46%42%
Africa20%24%25%
Share of land in each box where that system’s own reforecast beat climatology, at the longest lead this run reaches. The month-by-month detail for two of these boxes is on the U.S. and Europe lanes; all six are on Global.

The same model, scored twice

A check on the machinery

Route 03 benchmarks its consensus against one named member, and for the C3S archive that member is ecmwf-51 — ECMWF SEAS5, which is exactly the model route 10 publishes on its own. The two arrive by different roads: separate CDS ingests, separate store modules, and separate RPSS implementations that share no code beyond the region boxes.

They agree to 0.0008 at worst, across all 12 scorings. That is a statement about this site’s verification machinery and not about the model: the underlying forecast is the same C3S dataset in both, so this is a consistency check, not a second opinion. It is here because the rest of the page asks you to compare numbers from three pipelines, and this is the evidence that those pipelines agree when they should.

Fieldmonthroute 10 — SEAS5route 03 — ecmwf-51difference
TemperatureOctober 2026part elapsed+0.248+0.248+0.0003
TemperatureNovember 2026+0.056+0.056+0.0005
TemperatureDecember 2026+0.042+0.042+0.0000
TemperatureJanuary 2027+0.032+0.032+0.0001
TemperatureFebruary 2027+0.074+0.074-0.0004
TemperatureMarch 2027+0.064+0.064-0.0004
RainfallOctober 2026part elapsed+0.148+0.147+0.0006
RainfallNovember 2026+0.004+0.004-0.0004
RainfallDecember 2026+0.006+0.006-0.0003
RainfallJanuary 2027-0.014-0.013-0.0008
RainfallFebruary 2027-0.007-0.007-0.0003
RainfallMarch 2027-0.017-0.018+0.0005

What this page will not compare

And where the matched version is

Three systems are in the table above. The site publishes a fourth forecast — the Analog Bench, route 09, its own — and it is deliberately not there.

It could not be. It scores rolling three-month seasons where these score months; it reports anomaly correlation against an 86-year library where these report RPSS against a 24-year reforecast; and a correlation and a skill score are not the same kind of number even before the periods differ. Putting 0.26 beside +0.056 in one row would produce a sentence that reads perfectly and means nothing.

The matched version of that comparison already exists and is worth more than a shared row would be: route 11 puts the analog engine and SEAS5 on identical footing over the same 24 years and the same targets. It found that doing so reverses the answer the two routes’ own published numbers imply. That reversal is the reason this page states the footing of every comparison it makes and refuses the ones it cannot make.

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