Heidelberg Temperature & Trend Analysis
Analyzing 154 years of climate data (1871–2025) and long-term warming trends.
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... per decade (1926-2025)
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... vs. 1871-1900 baseline
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Climatological Analysis
This dashboard provides a clear, quantitative look at the temperature development in Heidelberg. Over the last 150+ years, the region has experienced an undeniable shift in its temperature baseline.
Historically, Heidelberg's position in the Upper Rhine Plain and the Neckar valley has given it a relatively warm and sheltered climate compared to other regions in Germany. However, anthropogenic warming has dramatically amplified this. While the warming trend since 1871 is +0.15°C per decade, this rate has accelerated to +0.20°C per decade over the last 100 years.
This warming is reflected in a shift of seasonal averages: modern winters (2021–2025) are now warmer than historical winters, and modern summers are breaking records. The number of annual "Hot Days" (maximum temperature ≥ 30°C) has surged from a decadal average of under 5 days in the early 20th century to over 20 days in recent years, while "Frost Days" (minimum temperature < 0°C) continue to decline.
Methodology Notes
Data Origin: German Weather Service (Deutscher Wetterdienst, DWD) Climate Data Center.
Heidelberg Station (02080): Coordinates 49.4206° N, 8.6676° E, elev. 110m. Closed in 2012. Used as the historical baseline (1871-2012).
Mannheim Station (05906): Coordinates 49.5063° N, 8.5584° E, elev. 98m. Active. Used as a proxy for recent years (2013-2025).
Calibration: Analysis of overlapping years (1947–2011) showed Mannheim is consistently 0.53°C cooler on average than Heidelberg due to station placement and topography. To create a seamless composite, Mannheim daily and monthly data for 2013–2025 has been adjusted by +0.53°C.