Little is known about the interaction between climatically expressed hydrology and topographic evolution of dryland basins because the processes by which they are shaped occur so infrequently and typically on timescales longer than human lives. In semi-arid to arid drainage basins, the primary driver of changes at or near the Earth’s surface is convective rainstorms. These storms are short-lived and small-in-area relative to drainage basin size, yet they dominate runoff generation and groundwater recharge, and control both water supply and flood risk to marginal communities of people. They also govern the availability of water to vegetation and other ecology, as well as spatial patterns of sediment, nutrient, and contaminant transport and deposition on local to basin scales. How would dryland landscapes (vegetation, water storage, and landforms) evolve to a wetter/drier climate regime or one with increased/decreased storminess? This information gap creates great challenges for predicting expected hydrologic patterns and processes under a shifting climate within dryland drainage basins, thus limiting research advances in environments occupying 41% of the Earth’s surface and home to 1/3 of the world’s population.
We have been working to better understand the climate drivers in dryland environments and the Earth surface responses to heterogeneous runoff generation with a broader goal of characterizing the evolving water balance and landscape evolution under climate change. We have made contributions to the development of new modeling tools for simulating the spatial and temporal effects of individual rainstorms over the landscape and their influence on soil moisture, runoff, streamflow, groundwater recharge, and evapotranspiration. We have also compiled new topographic databases of the world’s drainage basins that enabled us to identify distinct and unprecedented climatic signatures within topography that segregate by regional aridity.
Projects on this research theme include:
Climatic controls on river topography. PhD Project of Shiuan-An (Andrew) Chen, Unfunded.
Drought Resilience In East African dryland Regions (DRIER). Funded by The Royal Society, K. Michaelides, M. Singer (co-PI), M. Cuthbert, D. Mitchell, R. Rosolem, 2019-2022
Publications on this research theme include:
*Quichimbo, E.A., Singer, M.B., Michaelides, K., Hobley, D., Rosolem, R., Cuthbert, M.O. (In Preparation); Development of a parsimonious model for assessing climate impacts on the water balance in drylands across spatial and temporal scales
*Kipkemoi, I., Michaelides, K., Singer, M.B., Rosolem, R. (In Preparation); Climatic expression of rainfall on soil moisture dynamics in drylands
Singer, M.B., Grieve, S.W.D., *Chen, S-A, Michaelides, K. (In Revision); Climate controls the length and shape of the world’s drainage basins
*Adloff, M., Singer, M.B., MacLeod, D.A., Michaelides, K., *Mehrnegar, N., Hansford, E., Funk, C., Mitchell, D. (In Revision); Translation of seasonal rainfall into regional water storage in the Horn of Africa Drylands
*Quichimbo, A., Singer, M.B., Cuthbert, M.O. (2020); Characterizing groundwater-surface water interactions in idealized ephemeral stream systems, Hydrological Processses, doi: 10.1002/hyp.13847
Singer, M.B., Michaelides, K., Hobley, D.E.J. (2018); STORM 1.0: A simple, flexible, and parsimonious stochastic rainfall generator for simulating climate and climate change, Geoscientific Model Development, 11:3713-3726, doi: 10.5194/gmd-11-3713-2018. pdf
Michaelides, K., *Hollings, R., Singer, M.B., Nichols, M., Nearing, M. (2018); Spatial and temporal analysis of hillslope-channel coupling and implications for the longitudinal profile in a dryland basin, Earth Surface Processes and Landforms, 43:1608–1621, doi: 10.1002/esp.4340. pdf
Jaeger, K., Sutfin, N.A., Tooth, S., Michaelides, K., Singer, M.B. (2017); Geomorphology and sediment regimes of intermittent rivers and ephemeral streams; in Datry, T., Bonada, N., Boulton, A. (eds.), Intermittent Rivers and Ephemeral Streams, pp.21-49, Academic Press, Burlington, doi: 10.1016/B978-0-12-803835-2.00002-4. pdf