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Abstract
The Kenyan Rift Valley has experienced an abrupt and significant rise in its lake levels since 2010, followed by a more rapid rise since 2020. This paper examines the dynamic changes in precipitation patterns and their climatic drivers in the Kenyan Rift Valley region from 1981 to 2021, focusing on Lake Nakuru. Notably, in 2010, a pivotal change point in precipitation aligns with the rising water levels of Lake Nakuru. Using an atmospheric moisture tracking model, our study reveals that this transformation is associated with a southward shift in moisture sources. More moisture is now coming from the southern Indian Ocean, where substantial increases in sea surface temperatures and evaporation are observed. These findings highlight the complex interplay between climatic drivers, changing moisture sources, and lake Nakuru's water levels.
DOI
https://doi.org/10.31223/X5M70D
Subjects
Atmospheric Sciences, Civil and Environmental Engineering, Engineering, Environmental Engineering, Meteorology, Oceanography, Oceanography and Atmospheric Sciences and Meteorology
Keywords
Moisture tracking, hydrology, Kenya Rift Valley, Evaporative contribution, Water Management, Rising water levels, evaporation, hydrology, Kenya Rift Valley, evaporation, Water management, rising lakes
Dates
Published: 2025-01-21 13:46
Last Updated: 2025-01-21 21:46
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Data Availability (Reason not available):
Kenya Meteorological Department precipitation data can be requested through https://meteo.go.ke/resources/data-request. Time series of lake characteristics can be obtained through https://dahiti.dgfi.tum.de/en/13220/surface-area/. The code for WAM2layers moisture tracking model is provided at https://github.com/WAM2layers/WAM2layers. ERA5 reanalysis data on hourly basis can be downloaded from https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-single-levels?tab=overview. Sea surface temperature data can be retrieved via https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-oras5?tab=overview.
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