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RISK OUTLOOK ARCHIVE

NOVEMBER 2017

Even with similar forecasts for a La Nina, ECMWF and UKMO give quite different precipitation patterns over Europe for DJF, with ECMWF being dry over Poland and wet in southern Europe while UKMO is wet in central and northern Europe. The difference is enhanced by the UKMO NAO-based product.

But even when using the relatively dry ECMWF forecast for Poland, the EFAS and SMHI hydrology models’ discharge for the region is high due to the wet initial conditions and a long sensitivity from the initial conditions. If the discharge forecast was driven by the UKMO atmosphere the result would probably be more severe.

State at starting point, based on ERA-5

Normalised anomaly soil moisture 0-1m

Dry soil in southern France and Spain. Poland is initially very wet initially. Basins with long hydrological memory as seen in the sensitivity analysis.

Normalised anomaly soil moisture 0-1m zoom

SST anomaly

Emerging La Nina

SST anomaly zoom

Atm. seasonal forecasts (month 1-3) from Copernicus C3S

Indices based on ECMWF

  • ENSO

    ENSO

  • NAO

    NAO

  • Northern Europe Temperature

    Northern Europe Temperature

  • Northern Europe Precipitation

    Northern Europe Precipitation

  • Southern Europe Temperature

    Southern Europe Temperature

  • Southern Europe Precipitation

    Southern Europe Precipitation

Hydrological outlooks

EFAS (0-1.5 months)

High discharge in Poland due to wet initial conditions.

Hydrological outlooks (all by ECMWF) zoom

BfG for Kaub (0-1.5 months)

SMHI Seasonal