2015 - Member of the National Academy of Engineering For modeling of coupled ground- and surface water flow and of solute transport in groundwater.
2001 - Fellow of American Geophysical Union (AGU)
Fellow of the Geological Society of America
Leonard F. Konikow mainly focuses on Groundwater, Hydrology, Aquifer, Surface water and Water table. His studies deal with areas such as Sea level rise and Atmospheric sciences as well as Groundwater. His primary area of study in Hydrology is in the field of Groundwater recharge.
His Aquifer study combines topics in areas such as Water quality, Irrigation and Calcite. As a part of the same scientific family, Leonard F. Konikow mostly works in the field of Irrigation, focusing on Aquatic ecosystem and, on occasion, Hydrogeology. His work in Water table tackles topics such as Salinity which are related to areas like Dispersion.
His primary scientific interests are in Groundwater, Hydrology, Aquifer, Hydrogeology and Groundwater flow. He combines subjects such as Mineralogy and Water resource management with his study of Groundwater. His work in Hydrology addresses subjects such as Salinity, which are connected to disciplines such as Calibration.
His work focuses on many connections between Aquifer and other disciplines, such as Irrigation, that overlap with his field of interest in Water quality. His Groundwater flow research focuses on subjects like Soil science, which are linked to Steady state. The Groundwater recharge study combines topics in areas such as Drainage basin and Extraction.
Hydrology, Groundwater, Streamflow, Water resource management and Aquifer are his primary areas of study. Leonard F. Konikow integrates Hydrology with Spring in his research. His Groundwater study frequently draws connections between adjacent fields such as Hydrogeology.
His Hydrogeology research includes elements of Drawdown, Hydraulic head, Extraction and Environmental planning. His Aquifer research incorporates themes from Soil science and Petrology. His studies in Groundwater recharge integrate themes in fields like Discharge, Water table, STREAMS and Submarine groundwater discharge.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Ground water and climate change
Richard G. Taylor;Bridget R. Scanlon;Petra Döll;Matt Rodell.
Nature Climate Change (2013)
Computer model of two-dimensional solute transport and dispersion in ground water
Leonard F. Konikow;J.D. Bredehoeft.
Techniques of water-resources investigations (1978)
Ground-water models cannot be validated
Leonard F. Konikow;John D. Bredehoeft.
Advances in Water Resources (1992)
Groundwater depletion: A global problem
Leonard F. Konikow;Eloise Kendy.
Hydrogeology Journal (2005)
Revisiting the Earth's sea-level and energy budgets from 1961 to 2008
John A. Church;Neil J. White;Leonard F. Konikow;Catia M. Domingues.
Geophysical Research Letters (2011)
Contribution of global groundwater depletion since 1900 to sea‐level rise
Leonard F. Konikow.
Geophysical Research Letters (2011)
A three-dimensional method-of-characteristics solute-transport model (MOC3D)
Leonard F. Konikow;D.J. Goode;G.Z. Hornberger.
Water-Resources Investigations Report (1996)
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts?
Jonathan M Gregory;N. J. White;J. A. Church;M. F. P. Bierkens.
Journal of Climate (2013)
Groundwater Depletion in the United States (1900?2008)
Leonard F. Konikow.
(2014)
Modeling flow and chemical quality changes in an irrigated stream‐aquifer system
Leonard F. Konikow;John D. Bredehoeft.
Water Resources Research (1974)
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