Browsing by Subject "Namib desert"

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    The Contributions of Soil Moisture and Groundwater to Non-Rainfall Water Formation in the Namib Desert
    (2019-08) Adhikari, Bishwodeep; Wang, Lixin; Li, Lin; Jacinthe, Pierre-André
    Non-rainfall waters such as fog and dew are considered as important source of water in drylands, and the knowledge of possible sources of its formation is very important to make future predictions. Prior studies have suggested the presence of radiation fog in drylands; however, its formation mechanism still remains unclear. There have been earlier studies on the effects of fog on soil moisture dynamics and groundwater recharge. On the contrary, no research has yet been conducted to understand the contribution of soil moisture and groundwater to fog formation. This study, therefore, for the first time intends to examine such possibility in a fog-dominated dryland ecosystem, the Namib Desert. The study was conducted at three sites representing two different land forms (sand dunes and gravel plains) in the Namib Desert. This thesis is divided into two parts: the first part examines evidences of fog formation through water vapor movement using field observations, and the second part simulates water vapor transport using HYDRUS-1D model. In the first part of the study, soil moisture, soil temperature and air temperature data were analyzed, and the relationships between these variables were taken as one of the key indicators for the linkage between soil water and fog formation. The analysis showed that increase in soil moisture generally corresponds to similar increase in air or soil temperature near the soil surface, which implied that variation in soil moisture might be the result of water vapor movement (evaporated soil moisture or groundwater) from lower depths to the soil surface. In the second part of the study, surface fluxes of water vapor were simulated using the HYDRUS-1D model to explore whether the available surface flux was sufficient to support fog formation. The actual surface flux and cumulative evaporation obtained from the model showed positive surface fluxes of water vapor. Based on the field observations and the HYDRUS-1D model results, it can be concluded that water vapor from soil layers and groundwater is transported through the vadose zone to the surface and this water vapor likely contributes to the formation of non-rainfall waters in fog-dominated drylands, like the Namib Desert.
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    Investigating Dew Trends and Drivers Using Ground-Based Metreological Observations at the Namib Desert
    (2024-08) Javanmardi, Sara; Wang, Lixin; Li, Lin; Jacinthe, Pierre-André
    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.