Investigating Dew Trends and Drivers Using Ground-Based Metreological Observations at the Namib Desert

Abstract

In arid environments such as the Namib Desert, sources of non-rainfall waters such as dew and fog are crucial for sustaining ecosystem functions such as vegetation dynamics and biogeochemical processes, yet they remain among the least studied features of the water cycle. There is a concern that dew may become increasingly scarce because of climate warming, a trend not yet documented in the Namib Desert. This study aims to examine how dew formation trends in this region are evolving, drawing on field observations and assessing the factors influencing these trends. Our analysis involved processing meteorological data gathered from SASSCAL (Southern African Science Service Center for Climate and Adaptive Land Management) between 2015 and 2022, supplemented by direct dew observations to estimate dew occurrence in Gobabeb, a research station in Namib Desert. We developed an empirical equation to calculate dew formation based on the meteorological data. We used field-based dew records to validate the empirical equation and applied this equation to calculate dew formation between 2015 and 2022. We found dew formation concentrated in December to May (wet season). We evaluated the trends of dew formation at both monthly and annual scales. The findings showed a decline in dew formation (13.74% in the annual dew days count), a trend that could significantly impact the ecosystems in the Namib Desert. We found that soil temperature, air temperature, and humidity are the major contributors of the observed dew trends. The inverse relationship observed between increasing temperatures and dew formation supports the notion that elevated temperatures accelerate evaporation rates and diminish the chances of dew formation. This association underscores the susceptibility of dew formation to the impacts of climate change, as rising temperatures and shifting precipitation patterns are anticipated outcomes.