Investigating Drought–Seismicity Linkages Across Botswana and surrounding areas: Evidence from SPEI and Earthquake Catalogues

Preliminary analysis shows that periods of severe and prolonged drought often coincide with elevated seismic activity in the Okavango Rift Zone and adjacent areas, suggesting a coupling between hydrological stress and tectonic processes. Notable findings include clustering of moderate‑magnitude earthquakes (Mw ≥ 2.5) during multi‑year drought episodes, and a tendency for seismicity rates to decline during wetter intervals.

These patterns underscore the importance of considering climate variability in regional hazard assessments. Earthquake records include event identifiers, date, time, latitude, longitude, depth, magnitude, and source catalog, while SPEI files present standardized drought indices across multiple timescales. Preprocessing steps involved magnitude homogenization, duplicate removal, and spatial filtering of seismic events, alongside standardized SPEI computation using R-based scripts.

The dataset is structured into tabular files (CSV/Excel) with accompanying metadata and scripts to ensure transparency and reproducibility. Potential applications include multi-hazard risk assessment, investigations of climate–tectonic interactions, and educational use in geophysics and climate science. Limitations include variations in seismic catalog completeness and uncertainties in SPEI values, particularly in arid regions.