Clifford I. Voss has been selected as the 2015 Birdsall-Dreiss Distinguished Lecturer by the Geological Society of America (GSA) Hydrogeology Division. Cliff is a senior scientist with the National Research Program of the U.S. Geological Survey (USGS), currently working in Menlo Park, California. Cliff, an internationally recognized expert in groundwater modeling, has over 35 years of project management, implementation, field work and research experience in groundwater systems, including: computer model development and effective model use for scientific evaluation of hydrogeologic systems; groundwater resources development, management and protection; coastal and island groundwater resources subject to seawater intrusion; and use of the subsurface for energy production/storage and toxic waste isolation. Cliff advises extensively on groundwater system evaluation and management and he lectures worldwide on these and related subjects. His scientific interests in hydrogeology include addressing hydrogeologic heterogeneity, physics of solute and energy transport, behavior of fluids with varying density, phase change in geothermal and frozen systems, inverse modeling and network design, and evaluating extensive aquifer systems in light of sparse data.
The practical methodology and models that Cliff and his colleagues developed are now widely used for managing both the quantity and quality of water supply. In particular, the SUTRA computer code, developed and maintained by Cliff and USGS colleagues, has been a standard tool for groundwater resource assessment ever since USGS made it publicly available in 1984. SUTRA has made possible hundreds of practical and research investigations globally since its release.
Examples of Cliff's work include: nuclear waste repository safety (Germany, Japan, Sweden), transboundary water resource management (Nubian Aquifer of Egypt, Libya, Sudan, Chad), sustainability of water supply (arsenic-free groundwater supply from the Bengal Aquifer of India, Bangladesh), groundwater management in coastal areas subject to saltwater intrusion (USA), evaluation of water resources emergency (2004 tsunami in Thailand), and assessment of climate-change impacts on permafrost-mediated hydrology in cold regions (Alaska, USA), in part using simulation methodology for groundwater flow with freeze/thaw developed by Cliff and colleagues.
Cliff is the Executive Editor of Hydrogeology Journal, the official journal of the International Association of Hydrogeologists (IAH), which has become a premier venue for worldwide progress in theoretical and practical hydrogeology and groundwater-resource management under his twenty years of leadership. Hydrogeology Journal is co-sponsored by GSA's Hydrogeology Division.
For more information on Cliff's work and a list of his publications, please visit https://profile.usgs.gov/cvoss.
The Birdsall-Dreiss Distinguished Lecturer tour is sponsored by the GSA Hydrogeology Division. GSA will pay travel expenses, and the host institution will provide local accommodation and meals and, if needed, some local travel expenses. Cliff needs to organize several lectures in each region to make effective use of the travel funds, so lecture requests received by 15 December 2014 will be given priority when Cliff organizes his tour schedule.
Upon request, Cliff will present one of the three lectures listed below. All three lectures are appropriate for a general audience with some science background or interest. To request a visit to your institution please use our lecture request form. You can also contact Cliff by e-mail at email@example.com with any questions.
During the 50 years since its development, groundwater flow modeling has become the tool of choice that, when used wisely, provides deep insight into the functioning of aquifer systems that can become a foundation of effective water-resources management. This presentation reviews typical difficulties in characterizing aquifer systems (due to heterogeneity and data scarcity) and argues that simply-structured models are the most-effective means of dealing with inevitable uncertainties. Two examples of simply-structured model analyses of very large aquifer systems with sparse data will be presented. (1) In West Bengal, India, and Bangladesh, dissolved arsenic concentrations exceeding world standards exists in the drinking water of about 50 million people, making this the world's largest groundwater contamination problem. Previous scientific and technological efforts aimed at solving the problem had been largely directed towards understanding the chemistry of arsenic occurrence and release, but this groundwater modeling study is unique in providing a possible region-wide solution to the problem. (2) The Nubian aquifer is the world's largest non-renewable groundwater resource. It is a transboundary aquifer belonging to Chad, Egypt, Libya, and Sudan. International questions regarding resource fate, equitable use of the resource by each country (most current usage is by Egypt and Libya), and adverse impacts of cross-border pumping drawdown on shallow wells and oases were the reason for development of this model as part of a four-country Global Environmental Facility (GEF) project led by the International Atomic Energy Agency (IAEA). Simply-structured model development provided robust answers to these questions, and provided a relatively simple tool that could be adopted and used by water managers in each country.
Difficulties in understanding and managing hydrogeologic systems with variable-density groundwater flow are often due to the common notion that groundwater flow is driven in the direction of decreasing water-table elevation or hydraulic head; i.e. 'downhill'. However, even small variations in groundwater density can drive flow in directions that have no relation to decreasing elevation or head. Groundwater density varies due to spatial or temporal differences in temperature and concentration of dissolved solids. These differences in density can lead to interesting and sometimes unexpected flow patterns. In coastal aquifers, seawater intrusion (and contamination of groundwater supplies) occurs because denser salty sub-sea groundwater pushes laterally inland below less-dense fresh groundwater flowing seaward. Saltwater also occurs above fresher groundwater (in sabkhas, salt ponds, areas of coastal sea incursion) and here, denser saltwater 'falls' downward through the fresher less-dense groundwater, also salinizing the aquifer. Vertical density-driven flow giving rise to natural convection similarly occurs where warmer groundwater exists below cooler water, such as in geothermal, volcanic and ocean-ridge regions. This presentation reviews variable-density groundwater flow phenomena and their importance in practical settings. It is shown that the flow pattern in cases of lateral density differences is rather uniform in comparison with the flow pattern generated by vertical density differences, which exhibits fascinating variety and evolution. Examples of lateral and vertical density-driven flows in coastal aquifers show how modeling variable-density groundwater flow can be used to understand and effectively manage coastal resources.
As much as one third of the earth's land surface undergoes yearly freezing and one quarter of the earth's land surface is underlain by perennially-frozen ground -- permafrost. There is limited knowledge about the hydrogeology of these dominant cold regions of earth because most human population lives in temperate-climate areas. This knowledge base, cryohydrogeology, is the study of the dynamic interaction of groundwater with freezing and thawing processes. Subsurface ice is a barrier to flow, thus, the pattern of frozen ground is a major control on surface and subsurface water flows. Consequently, ice distribution controls cold-regions hydrology, which in turn affects cold-regions geochemistry and ecology. Motivated by international concern regarding global warming impacts on ground ice distribution and resulting changes to ecosystems, and by the opportunity to study the intriguing hydrological processes mediated by water-ice phase change, recent work by the U.S. Geological Survey and partner institutions have focused on a permafrost region of interior Alaska. This presentation describes some results of that work, including: observed cold-region hydrologic phenomena, efforts to understand the ground ice and water flow mechanisms that control them, and, assessment of likely hydrologic changes resulting from climate evolution. The study produced extraordinary maps of permafrost distribution and thickness (from airborne geophysical surveys), never before obtained for such large regions. The study found that complex inter-related ice-hydrology mechanisms cause surface-water bodies to shrink and expand, and permafrost continuity affects groundwater discharge to rivers (impacting river chemistry). A new model that simulates groundwater flow with heat transport and groundwater freezing and thawing, being finalized as part of the effort, has already allowed evaluations of paleoclimate-change permafrost evolution and of future climate-change scenario impacts on today's permafrost. It is found that groundwater flow and permafrost formation and thaw are strongly-coupled processes; where groundwater flows in cold regions, it accelerates permafrost thaw during climate warming.