Data sources and references

KLIMAT-P is built exclusively on publicly available observational data, established atmospheric indices, and peer-reviewed methodology. Every number in the platform traces back to one of the sources below.

Observational Data

IMGW-PIB — Synoptic Station Network

Primary observational data
Instytut Meteorologii i Gospodarki Wodnej — Państwowy Instytut Badawczy
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Poland's national meteorological and hydrological institute. KLIMAT-P uses real-time synoptic station readings from the IMGW-PIB open data programme, covering temperature, wind, precipitation, humidity and pressure across the Polish station network. Readings are published approximately hourly.

IMGW-PIB — Climatological Normals (1991–2020)

Climatological baseline
Instytut Meteorologii i Gospodarki Wodnej — Państwowy Instytut Badawczy
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Published 30-year climatological baseline (1991–2020) for Polish regions, used as the reference period for all anomaly computations. This is the WMO-standard reference period adopted by meteorological services worldwide for the current generation of climate normals.

Atmospheric Indices

NOAA CPC — North Atlantic Oscillation (NAO)

Teleconnection index
National Oceanic and Atmospheric Administration, Climate Prediction Center
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Monthly NAO index, standardised. The NAO is the dominant mode of atmospheric variability over the North Atlantic and is one of the primary large-scale signals influencing precipitation and temperature patterns over Poland. Positive NAO phases are associated with warm, dry conditions in central Europe; negative phases with cold, wet patterns.

NOAA CPC — Arctic Oscillation (AO)

Teleconnection index
National Oceanic and Atmospheric Administration, Climate Prediction Center
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Monthly AO index, standardised. The Arctic Oscillation describes the dominant pattern of non-seasonal sea-level pressure variations north of 20°N latitude. It influences the strength of westerly winds and affects the position of storm tracks across Europe.

NOAA CPC — Oceanic Niño Index (ONI / ENSO)

Teleconnection index
National Oceanic and Atmospheric Administration, Climate Prediction Center
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Three-month running mean of sea surface temperature anomalies in the Niño 3.4 region (5°N–5°S, 120°–170°W), used as the standard ENSO indicator. ENSO phase influences seasonal temperature and precipitation patterns across Europe through teleconnection pathways, typically with a 1–3 month lag.

Verification Methodology

Brier Score

Forecast verification
Brier, G.W. (1950). Verification of weather forecasts expressed in terms of probability.
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The primary accuracy metric used to evaluate KLIMAT-P probability estimates. For each prediction, the Brier Score computes (predicted probability − actual outcome)². A perfect score is 0.0; a naive model that always predicts 50% scores 0.25. The score is computed automatically each week using actual IMGW station observations as ground truth.

WMO Guidelines on Probabilistic Prediction

International standard
World Meteorological Organization
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KLIMAT-P follows WMO guidelines for the construction and communication of probabilistic forecasts, including the use of the 1991–2020 standard reference period for climatological anomaly calculations and the calibration of probabilistic outputs against historical observations.

Climatological Literature

Atlas Klimatyczny Polski

Regional climatology
Lorenc, H. (Ed.) (2005). Atlas klimatyczny Polski. IMGW-PIB, Warsaw.
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The primary Polish climatological reference atlas published by IMGW-PIB. Used as a secondary source for regional temperature and precipitation characteristics across Polish voivodeships, supplementing the 1991–2020 normals for regional model configuration.

Coelho et al. (2006) — Forecast Calibration and Combination

Methodology reference
Coelho, C.A.S., Pezzulli, S., Balmaseda, M., Doblas-Reyes, F.J., Stephenson, D.B. (2006). Forecast calibration and combination: A simple Bayesian approach for ENSO. Journal of Climate, 19(10), 1504–1516.
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A key methodological reference for the Bayesian approach used in KLIMAT-P's probability updating framework. The paper describes how prior seasonal climate probabilities can be updated using observed anomalies and large-scale atmospheric indices.

Doblas-Reyes et al. (2005) — Multi-model Seasonal Forecasting

Methodology reference
Doblas-Reyes, F.J., Hagedorn, R., Palmer, T.N. (2005). The rationale behind the success of multi-model ensembles in seasonal forecasting. Tellus A, 57(3), 234–252.
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Provides the theoretical basis for using multiple independent signals (station anomalies, teleconnection indices, historical analogs) in combination rather than relying on a single predictor — a core principle of the KLIMAT-P model design.

A note on what's not listed here

This page lists the intellectual and data sources that inform the model. It does not describe implementation infrastructure. KLIMAT-P is a beta research platform, and the model is under active development.