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Tracing the History of Meteorological Science

A living archive of the science, instruments, institutions, and records that shaped our understanding of weather.

Preserving the History of Meteorological Science

This site explores the history of meteorology as a scientific discipline. It examines how weather knowledge developed over time—how people observed the atmosphere, built instruments, formed theories, organized data, and gradually learned to forecast what had once seemed unpredictable.

The focus is on historical context: what was known at the time, how it was measured, what assumptions were made, and where those methods succeeded or failed. No prior scientific background is required.

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Foundations

Early weather knowledge, cultural interpretations, and pre-scientific ideas.

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Institutions & Networks

The organizations and data systems behind modern meteorology.

Explore the Archive

Instruments & Observation

How temperature, pressure, wind, and precipitation became measurable.

Antique Brass Compass

Maps & Charts

Geographic views of meteorological development.

Orbiting Satellite
Forecasting & Theory

From pattern recognition to numerical weather prediction.

Powerful Tornado Scene
Extremes & Records

Heat, cold, wind, storms, and the challenges of historical records.

Featured Content

c. 1700–1742

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Standardization and the Problem of Measurement Scales

The problem of standardization and measurement scales marks a turning point in the history of science, when atmospheric observation shifted from local, instrument-bound readings to shared and comparable numerical systems. Emerging between the 17th and 19th centuries, it reveals how temperature and pressure measurements were gradually aligned through common reference points, enabling scientists to translate scattered observations into a unified language of data.

18th century

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Dew Point, Condensation, and Early Hygrometric Tables

A foundational exploration of how moisture in the air becomes measurable through condensation, linking dew formation to early attempts at quantifying atmospheric humidity. Developed across the eighteenth and nineteenth centuries, it traces the emergence of dew point as a physical threshold and the rise of hygrometry as a numerical approach to understanding weather and atmospheric change.

1686

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Edmond Halley and the Mapping of Global Winds

This work represents a key moment in early modern science, when observation from maritime exploration began to merge with theoretical explanation. Although later models would refine and correct his mechanisms, Halley’s approach helped establish the idea of a dynamic, planet-wide atmosphere shaped by systematic physical processes rather than isolated regional effects.

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